text:
Wikipedia:Files for discussion/2020 August 17

File:Commonwealth of Pennsylvania House of Representatives Citation, James E. Casorio, Jr., Sponsor, April 29, 2008.jpg

The result of the discussion was: Deleted by (non-admin closure) Aasim 07:42, 25 August 2020 (UTC)
 * File:Commonwealth of Pennsylvania House of Representatives Citation, James E. Casorio, Jr., Sponsor, April 29, 2008.jpg ([ delete] | talk | [ history] | links | [ logs])  – uploaded by Dennyboy34 ( [ notify] | contribs | uploads | upload log).

Works of the Pennsylvania state government are copyrighted. Wikiacc (¶) 03:04, 17 August 2020 (UTC)

 * Delete per nom. Yet another misuse of PD-because. The Squirrel Conspiracy (talk) 04:47, 17 August 2020 (UTC)
 * Delete, essentially orphaned (not used in the main space) with questionable licensing. Salavat (talk) 06:19, 22 August 2020 (UTC)

File:Selfless Service- The Cavalry Career of Brigadier General Samuel M. Whitside from 1858 to 1902.pdf

The result of the discussion was: delete.  MBisanz  talk 15:34, 29 August 2020 (UTC)
 * File:Selfless Service- The Cavalry Career of Brigadier General Samuel M. Whitside from 1858 to 1902.pdf ([ delete] | talk | [ history] | links | [ logs])  – uploaded by V8m8i ( [ notify] | contribs | uploads | upload log).

Originally nominated for speedy deletion by @Wikiacc under criterion WP:CSD  F ASTILY   07:43, 17 August 2020 (UTC)

 * Delete - It's current use is on a user page where it is just plunked down with no explanation. Wikipedia is not a web host and if this is needed as a reference, then it can referenced without hosting it here. -- Whpq (talk) 13:10, 20 August 2020 (UTC)
 * Delete, essentially orphaned (not used in the main space) with no obvious value. Salavat (talk) 06:20, 22 August 2020 (UTC)
 * Delete: Unencyclopedic Aasim 06:55, 25 August 2020 (UTC)

File:IPLlogo.png

The result of the discussion was: Deleted by (non-admin closure) Aasim 07:43, 25 August 2020 (UTC)
 * File:IPLlogo.png ([ delete] | talk | [ history] | links | [ logs])  – uploaded by Shahin ( [ notify] | contribs | uploads | upload log).

Does not satisfy WP:NFCC. The image is not used as the primary means of visual identification. The use of historical, former, alternate or anniversary logos for an entity is not allowed, unless the logo itself is described in the context of sourced critical commentary about that logo. Jonteemil (talk) 13:21, 17 August 2020 (UTC)

File:Azadegan League Logo old.png

The result of the discussion was: deleted by (non-admin closure) Aasim 07:43, 25 August 2020 (UTC)
 * File:Azadegan League Logo old.png ([ delete] | talk | [ history] | links | [ logs])  – uploaded by User90fan ( [ notify] | contribs | uploads | upload log).

Does not satisfy WP:NFCC. The image is not used as the primary means of visual identification. The use of historical, former, alternate or anniversary logos for an entity is not allowed, unless the logo itself is described in the context of sourced critical commentary about that logo. Jonteemil (talk) 13:22, 17 August 2020 (UTC)

File:Tata Air Lines&

The result of the discussion was: Delete; deleted by A file with this name on Commons is now visible. AnomieBOT ⚡ 08:07, 25 August 2020 (UTC)
 * File:Tata Air Lines& ([ delete] | talk | [ history] | links | [ logs])  – uploaded by Faizhaider ( [ notify] | contribs | uploads | upload log).

see Magog the Ogre (t • c) 23:23, 17 August 2020 (UTC)
 * The above discussion is preserved as an archive of the debate. Please do not modify it. Subsequent comments should be made on the appropriate discussion page (such as the media's talk page or in a deletion review).  No further edits should be made to this section.

File:Pagal (1940).jpg

The result of the discussion was: Delete; deleted by A file with this name on Commons is now visible. AnomieBOT ⚡ 08:07, 25 August 2020 (UTC)
 * File:Pagal (1940).jpg ([ delete] | talk | [ history] | links | [ logs])  – uploaded by Kaayay ( [ notify] | contribs | uploads | upload log).

see. Magog the Ogre (t • c) 23:26, 17 August 2020 (UTC)
 * The above discussion is preserved as an archive of the debate. Please do not modify it. Subsequent comments should be made on the appropriate discussion page (such as the media's talk page or in a deletion review).  No further edits should be made to this section.

File:Chandika.jpg

The result of the discussion was: Delete; deleted by A file with this name on Commons is now visible. AnomieBOT ⚡ 08:07, 25 August 2020 (UTC)
 * File:Chandika.jpg ([ delete] | talk | [ history] | links | [ logs])  – uploaded by Rajasekhar1961 ( [ notify] | contribs | uploads | upload log).

per. Magog the Ogre (t • c) 23:26, 17 August 2020 (UTC)
 * The above discussion is preserved as an archive of the debate. Please do not modify it. Subsequent comments should be made on the appropriate discussion page (such as the media's talk page or in a deletion review).  No further edits should be made to this section.

File:Baghban (1938).jpg

The result of the discussion was: Delete; deleted by A file with this name on Commons is now visible. AnomieBOT ⚡ 08:07, 25 August 2020 (UTC)
 * File:Baghban (1938).jpg ([ delete] | talk | [ history] | links | [ logs])  – uploaded by Kaayay ( [ notify] | contribs | uploads | upload log).

per. Magog the Ogre (t • c) 23:27, 17 August 2020 (UTC)
 * The above discussion is preserved as an archive of the debate. Please do not modify it. Subsequent comments should be made on the appropriate discussion page (such as the media's talk page or in a deletion review).  No further edits should be made to this section.

File:Tata Sons&

The result of the discussion was: Delete; deleted by A file with this name on Commons is now visible. AnomieBOT ⚡ 08:07, 25 August 2020 (UTC)
 * File:Tata Sons& ([ delete] | talk | [ history] | links | [ logs])  – uploaded by Faizhaider ( [ notify] | contribs | uploads | upload log).

see. Magog the Ogre (t • c) 23:31, 17 August 2020 (UTC)
 * The above discussion is preserved as an archive of the debate. Please do not modify it. Subsequent comments should be made on the appropriate discussion page (such as the media's talk page or in a deletion review).  No further edits should be made to this section.

File:Mahe 1-63360 43M10 1920s.jpg

The result of the discussion was: Delete; deleted by A file with this name on Commons is now visible. AnomieBOT ⚡ 08:07, 25 August 2020 (UTC)
 * File:Mahe 1-63360 43M10 1920s.jpg ([ delete] | talk | [ history] | links | [ logs])  – uploaded by Verityanne ( [ notify] | contribs | uploads | upload log).

see. Magog the Ogre (t • c) 23:34, 17 August 2020 (UTC)
 * The above discussion is preserved as an archive of the debate. Please do not modify it. Subsequent comments should be made on the appropriate discussion page (such as the media's talk page or in a deletion review).  No further edits should be made to this section.


text:
French/Lessons/Introductory/Review

G: The French alphabet
In addition, French uses several accents which are worth understanding. These are: à, è, ù, (grave accents) and é (acute accent). A circumflex applies to all vowels: â, ê, î, ô, û. A tréma (French for dieresis) is also applied: ä, ë, ï, ö, ü, ÿ. Two combined letters are used: æ and œ, and a cedilla is used on the c to make it sound like an English s: ç.

Things of note about numbers

 * For 70-79, it builds upon "soixante" but past that it builds upon a combination of terms for 80-99
 * Only the first (21,31,41,51,61 and 71, but not 81 nor 91) have "et un" without a hyphen; but past this it is simply both words consecutively (vingt-six, trente-trois, etc.) with a hyphen in between.
 * For 100-199, it looks much like this list already save that "cent" is added before the rest of the number; this continues up to 1000 and onward.

V: Time
In French, “il est” is used to express the time; though it would literally translate as “he is”, it is actually, in this case, equivalent to “it is” (unpersonal "il"). Unlike in English, it is always important to use “heures” (“hours”) when referring to the time. In English, it is OK to say, “It’s nine,” but this wouldn’t make sense in French. The French time system traditionally uses a 24-hour scale. Shorthand for writing times in French follows the format "17h30", which would represent 5:30PM in English.

V: The days of the week.

 * The days of the week are not capitalized in French.
 * For phrases relating to the day of the week, see the phrasebook.

Notes:
 * What day is it today? is equivalent to Quel jour sommes-nous ?.
 * Quel jour sommes-nous ? can be answered with Nous sommes..., C'est... or On est... (last two are less formal).
 * Nous sommes... is not used with hier, aujourd’hui, or demain. C'était (past) or C'est (present/future) must be used accordingly.

Bien... is an adverb meaning well. Its adjective equivalent is bon(ne), which means good. Since je vais, meaning I go, uses an action verb, the adverb bien is used. In English, I'm good, which uses the linking verb am, is followed by an adjective rather than an adverb.

Est-ce que... doesn't mean anything (like the Spanish upside down question mark) and is used to start a question. This can be used in a similar manner to do in English. Instead of You want it?, one can say Do you want it?

chez... is a preposition meaning at the house of.... Chez moi is used to say at my place. Chez [name] is used to say at [name's] place.

on... can mean we or one.

Review

source: wikimedia

license: Creative Commons - Attribution Share-Alike - https://creativecommons.org/licenses/by-sa/4.0/

title: French/Lessons/Introductory/Review


text:
kilogramo

Etymology
.

Noun

 * 1) kilogram

Etymology
From, calqued from.

Noun

 * 1) kilogram

Etymology
From, calqued from.

Noun

 * 1) kilogram

Etymology
From, a calque of.

Noun

 * 1) kilogram

Etymology
, from, from +.

Noun

 * 1) kilogram

Usage notes

 * In everyday language, kilo is more commonly in use than kilogramo.

title: kilogramo


text:
Wikiversity:Archive/No early policies

We believe that the policy process below is fundamentally flawed. To be valid such policies must reflect the accumulated wisdom of time and not the compulsions of the moment. While many of the proposals, when viewed individually, may be overwhelmingly supported, this is not the way to deal with them. If these policies are meant to be they will come in time. We therefore request that everyone desist from participating in the votes below, and ask those who have voted already to withdraw all their votes (except the ones for this policy).

title: Wikiversity:Archive/No early policies


text:
Mondo Kagonyera

George Mondo Kagonyera, also Mondo Kagonyera, is a Ugandan veterinarian, politician, academic, and university administrator. He is the immediate past chancellor of Makerere University, the oldest and largest university in Uganda. He was appointed to that position in 2007 by President Yoweri Museveni. After serving a full four year-term, he was re-appointed for another term in 2011, and was re-installed in January 2012.

Background and education
Kagonyera was born in Kabuga Village, Rukungiri District, in the Western Region of Uganda, circa 1941, to Zakaria Kagonyera and Elizabeth Kirihura. He attended Kigezi College Butobere for his O-Level studies, before he was admitted to Royal College Nairobi for his A-Level education. He studied at the University of Nairobi, graduating with the degree of Bachelor of Veterinary Medicine in the early 1960s. Later, he went on to obtain a Master of Science in Veterinary Medicine, from the University of California Davis, followed by a Doctor of Philosophy from the same institution.

Work experience
In 1967, he worked as a District Veterinary Officer for Masaka district for about five months which job he dropped to go for further studies. In 1971, following graduation from the University of California with his Master of Science degree, Kagonyera joined Makerere University as a lecturer. He was instrumental in establishing the Faculty of Veterinary Medicine, which has since morphed into the College of Veterinary Medicine, Animal Resources & BioSecurity. He also served as the chairman of the university appointments board from 1993 until 1999. He left the university to join Ugandan politics in 1998. As a politician, he served as the member of Parliament for Rubabo constituency in Rukungiri District and as a minister for general duties in the office of the prime minister. He also served as the deputy managing director of the Ugandan National Social Security Fund from 2006 until 2008.

title: Mondo Kagonyera


text:
Sotiris Alexandropoulos

Sotiris-Polykarpos Alexandropoulos (Σωτήρης-Πολύκαρπος Αλεξανδρόπουλος; born 26 November 2001) is a Greek professional footballer who plays as a defensive midfielder for Super League club Olympiacos, on loan from Sporting CP, and the Greece national team.

Panathinaikos
Alexandropoulos plays mainly as a midfielder and joined Panathinaikos from the team's youth ranks. Having turned 19, he became a near automatic starter for Panathinaikos in the 2019–20 season.

On 15 June 2021, he signed an extension with the club until the summer of 2024. On 11 September 2021, he scores his first goal for Panathinaikos senior team, against Apollon Smyrnis on a 4–1 win, at the first game of the season

On 21 May 2022, Alexandropoulos won the Greek Cup with Panathinaikos against PAOK, his first trophy in his senior career.

Sporting CP
On 29 August 2022, Alexandropoulos signed a five-year contract with Portuguese club Sporting CP for a fee of €4.5 million, with Panathinaikos also receiving 30% of a future transfer. On 2 September, he made his debut for the club, replacing Manuel Ugarte in the 89th minute in a 2–0 away win against Estoril in the Primeira Liga.

Loan to Olympiacos
On 3 August 2023, Olympiacos announced the acquisition of Alexandropoulos. The 21-year-old midfielder signed on an initial one-year loan with a purchase option for the following summer, amounting to €4 million.

International career
On 24 March 2021, Alexandropoulos was called up to the Greek senior team by coach John van 't Schip for the forthcoming World Cup 2022 qualifiers against Spain and Georgia. On 28 March 2021, he made his debut with the national team as a substitute in a friendly match against Honduras. Alexandropoulos also represented the country at all youth levels from under-16 onwards.

Honours
Panathinaikos
 * Greek Cup: 2021–22

Olympiacos
 * UEFA Europa Conference League: 2023–24

Individual
 * Super League Greece Young Player of the Season: 2021–22

title: Sotiris Alexandropoulos


text:
Electronics/RCL time domain

Figure 1: RCL circuit

When the switch is closed, a voltage step is applied to the RCL circuit. Take the time the switch was closed to be 0s such that the voltage before the switch was closed was 0 volts and the voltage after the switch was closed is a voltage V. This is a step function given by $$V\cdot u(t)$$ where V is the magnitude of the step and $$u(t)=1$$ for $$t\geq0$$ and zero otherwise.

To analyse the circuit response using transient analysis, a differential equation which describes the system is formulated. The voltage around the loop is given by:

$$ Vu(t)=v_c(t)+\frac{di(t)}{dt}L+Ri(t) \mbox{ (1)} $$

where $$v_c(t)$$ is the voltage across the capacitor, $$\frac{di(t)}{dt}L$$ is the voltage across the inductor and $$Ri(t)$$ the voltage across the resistor.

Substituting $$i(t)=\frac{dv_c(t)}{dt}$$ into equation 1:

$$ Vu(t)=v_c(t)+\frac{d^2v_c(t)}{dt^2}LC+R\frac{dv_c(t)}{dt}C $$ $$ \frac{d^2v_c(t)}{dt^2}+\frac{R}{L}\frac{dv_c(t)}{dt}+\frac{1}{LC}v_c(t)=\frac{Vu(t)}{LC} \mbox{ (2)} $$

The voltage $$v_c(t)$$ has two components, a natural response $$v_n(t)$$ and a forced response $$v_f(t)$$ such that:

$$ v_c(t)=v_f(t)+v_n(t)\mbox{ (3)} $$

substituting equation 3 into equation 2.

$$ \bigg[\frac{d^2v_n(t)}{dt^2}+\frac{R}{L}\frac{dv_n(t)}{dt}+\frac{1}{LC}v_n(t)\bigg]+\bigg[\frac{d^2v_f(t)}{dt^2}+\frac{R}{L}\frac{dv_f(t)}{dt}+\frac{1}{LC}v_f(t)\bigg]=0+\frac{Vu(t)}{LC} $$

when $$t>0s$$ then $$u(t)=1$$:

$$ \bigg[\frac{d^2v_n(t)}{dt^2}+\frac{R}{L}\frac{dv_n(t)}{dt}+\frac{1}{LC}v_n(t)\bigg]=0 \mbox{ (4)} $$ $$ \bigg[\frac{d^2v_f(t)}{dt^2}+\frac{R}{L}\frac{dv_f(t)}{dt}+\frac{1}{LC}v_f(t)\bigg]=\frac{V}{LC} \mbox{ (5)} $$

The natural response and forced solution are solved separately.

Solve for $$v_f(t):$$

Since $$\frac{V}{LC}$$ is a polynomial of degree 0, the solution $$v_f(t)$$ must be a constant such that:

$$ v_f(t)=K $$ $$ \frac{dv_f(t)}{dt}=0 $$ $$ \frac{d^2v_f(t)}{dt}=0 $$

Substituting into equation 5:

$$ \frac{1}{LC}K=\frac{V}{LC} $$ $$ K=V $$ $$ v_f=V \mbox{ (6)} $$

Solve for $$v_n(t)$$:

Let: $$ \frac{R}{L}=2\alpha $$ $$ \frac{1}{LC}=\omega_n^2 $$ $$ v_n(t)=Ae^{st} $$

Substituting into equation 4 gives:

$$ \frac{d^2Ae^{st}}{dt^2}+2\alpha\frac{dAe^{st}}{dt}+\omega_n^2Ae^{st}=0 $$ $$ s^2Ae^{st}+2\alpha Ae^{st}+\omega_2^2Ae^{st}=0 $$ $$ s^2+2\alpha s+\omega_n^2=0 $$

$$ s=\frac{-2\alpha\pm\sqrt{4\alpha^2-4\omega_n^2}}{2}=-\alpha\pm\sqrt{\alpha^2-\omega_n^2} $$

Therefore $$v_n(t)$$ has two solutions $$Ae^{s_1t}$$ and $$Ae^{s_2t}$$

where $$s_1$$ and $$s_2$$ are given by:

$$ s_1=-\alpha+\sqrt{\alpha^2-\omega_n^2} $$ $$ s_2=-\alpha-\sqrt{\alpha^2-\omega_n^2} $$

The general solution is then given by:

$$ v_n(t)=A_1e^{s_1t}+A_2e^{s_2t} $$

Depending on the values of the Resistor, inductor or capacitor the solution has three posibilies.

1. If $$\alpha > \omega_n$$ the system is said to be overdamped

2. If $$\alpha = \omega_n$$ the system is said to be critically damped

3. If $$\alpha < \omega_n$$ the system is said to be underdamped

Example
Given the general solution

$$ \alpha=\frac{R}{2L}=1000 $$ $$ \omega_n=\frac{1}{\sqrt{LC}}\approx 4472 $$

$$ s_1=-1000-4359j $$ $$ s_2=-1000+4359j $$

$$ v_n(t)=A_1e^{(-1000-4359j)t}+A_2e^{(-1000+4359j)t} $$

Thus by Euler's formula ($$e^{j\phi}=\cos{\phi}+j\sin{\phi}$$):

$$ v_n(t)=e^{-1000}\big[A_1\big(\cos(-4359t)+j\sin(-4359t)\big)+A_2\big(\cos(4359t)+j\sin(4359t)\big)\big] $$ $$ v_n(t)=e^{-1000t}\big[(A_1+A_2)\cos(4359t)+j(-A_1+A_2)\sin(4359t)\big] $$

Let $$B_1=A_1+A_2$$ and $$B_2=j(-A_1+A_2)$$

$$ v_n(t)=e^{-1000t}\big[B_1\cos(4359t)+B_2\sin(4359t)\big] $$

Solve for $$B_1$$ and $$B_2$$:

From equation \ref{eq:vf}, $$v_f=1$$ for a unit step of magnitude 1V. Therefore substitution of $$v_f$$ and $$v_n(t)$$ into equation \ref{eq:nonhomogeneous} gives:

$$ v_c(t)=1+e^{-1000t}\big[B_1\cos(4359t)+B_2\sin(4359t)\big] $$

for $$t=0$$ the voltage across the capacitor is zero, $$v_c(t)=0$$

$$ 0=1+B_1\cos(0)+B_2\sin(0) $$ $$ B_1=-1\mbox{ (7)} $$

for $$t=0$$, the current in the inductor must be zero, $$i(0)=0$$

$$ i(t)=\frac{dv_c(t)}{dt}C $$ $$ i(0)=100\cdot10^{-9}\big[e^{-1000t}\big(-4359B_1\sin(4359t)+4359B_2\cos(4359t)\big)-1000e^{-1000t}\big(B_1\cos(4359t)+B_2\sin(4359t)\big)\big] $$ $$ 0=100\cdot10^{-9}\big[4359B_2-1000B_1 \big] $$

substituting $$B_1$$ from equation \ref{eq:B1} gives

$$ B_2\approx-0.229 $$

For $$t>0$$, $$v_c(t)$$ is given by:

$$ v_c(t)=1-e^{-1000t}\big[\cos(4359t)+0.229\sin(4359t)\big] $$

$$v_{out}$$ is given by:

$$ v_{out}=V_{in}-v_c(t) $$ $$ v_{out}=Vu(t)-v_c(t) $$

For $$t>0$$, $$v_{out}$$ is given by:

$$ v_{out}=e^{-1000t}\big[\cos(4359t)+0.229\sin(4359t)\big] $$

title: Electronics/RCL time domain


text:
Wikipedia:Articles for deletion/Qazi Mahbub Hussain

The result was delete. Jo-Jo Eumerus (talk, contributions) 19:09, 11 October 2017 (UTC)

Qazi Mahbub Hussain

 * – ( View AfD View log  Stats )

NN relation of several notable people. The article has only ever cited one source, a magazine with the article title, author, and page number missing. Searches of the usual Google types, De Gruyter, EBSCO, Gale, HighBeam, JSTOR, Project Muse, ProQuest, and Questia, by Bengali script and two transliterations of his name, found only one other reliable source that is more than an author or translator credit: a brief obituary that doesn't mention anything he accomplished.

WP:BASIC requires multiple sources so that a neutral article can be written that doesn't simply repeat one person's point of view. Wikipedia doesn't have articles on authors, or translators, just because their names are on books. Enough people have to have written about the person for a full and balanced biographical article to be constructed. If the subject were notable, then he would have been written about, in depth, independently, in multiple sources. Worldbruce (talk) 18:51, 19 September 2017 (UTC)
 * Note: This debate has been included in the list of Authors-related deletion discussions. Worldbruce (talk) 18:51, 19 September 2017 (UTC)
 * Note: This debate has been included in the list of Bangladesh-related deletion discussions. Worldbruce (talk) 18:51, 19 September 2017 (UTC)

 Relisted to generate a more thorough discussion and clearer consensus.
 * Delete as per nom statement. Altaf  ( talk )  23:16, 19 September 2017 (UTC)

Please add new comments below this notice. Thanks,  MBisanz  talk 02:30, 27 September 2017 (UTC)  Relisted to generate a more thorough discussion and clearer consensus.

Please add new comments below this notice. Thanks, Optakeover (U)(T)(C) 04:52, 4 October 2017 (UTC)
 * Delete even after 1 decade of death, the struggle of notability is apparent. D4iNa4 (talk) 02:02, 7 October 2017 (UTC)


text:
Talk:David Rosen (rabbi)

Birth and nationality
He is son of Kopul Rosen, and he is a Britain naturalized Israelian. See. --Spinoziano (talk) 17:52, 17 January 2013 (UTC)

title: Talk:David Rosen (rabbi)


text:
List of New England hurricanes

A New England hurricane is a tropical cyclone originating in the Atlantic Ocean that affects the states of Connecticut, Rhode Island, Massachusetts, Vermont, New Hampshire, or Maine in the United States. Due to geography and climatology, the vast majority of tropical cyclone strikes to the New England region occur in Connecticut, Rhode Island, and eastern Massachusetts.

Since record keeping began for Atlantic tropical cyclones in 1851, there have been approximately 30 tropical cyclones to directly strike New England. Due to the location of New England, most tropical cyclones that threaten the region tend to recurve out to sea, mainly due to upper-level steering patterns, such as the jet stream. Tropical cyclones also tend to weaken upon approach due to the cooler waters above 40 latitude (near southeastern New England). Thus, tropical cyclone formation near New England and over the Gulf of Maine is very unfavorable. However, tropical cyclones moving up the East Coast can rapidly approach the Connecticut and Rhode Island coast before the encounter the cooler waters of southeast New England, and strike far southern New England as a category 3 hurricane. Both Connecticut and Rhode Island have been struck several times by a major hurricane since 1850.

Most commonly, New England will see the remnants or weakening stage of most tropical cyclones that make landfall either along the United States east coast or Gulf coast. This can sometimes lead to excessive rainfall, and in rare cases destructive flooding. Hurricane Diane in 1955 produced over 19 inches of rain in Massachusetts and contributed to the 1955 Connecticut floods, one of the worst flooding events in Connecticut's history. More recently, in 2011, a weakening Hurricane Irene produced historic flooding in Vermont, causing over $175 million in damage.

The return period for hurricane and major landfalls along the coast of New England is highest in Connecticut and Rhode Island, and declines rapidly north toward Maine. Generally, the return period for hurricane force winds is 12-16 years along the coast of Connecticut and Rhode Island (which is for example higher than the coast of Georgia much farther south), to more than 50 years along the Maine coast.

Due to the fact that sea surface temperatures from eastern Massachusetts northward are generally too cool to support a major tropical cyclone, the region very rarely sees a major hurricane landfall (Category 3 or higher). Since 1851, only 3 major hurricanes have ever made landfall on the New England coastline, and all of these were in Connecticut and Rhode Island. The return period for storms of such strength along the southern New England coastline is considered to be 50-70 years, and upwards of 300 years in coastal Maine. As of 2022, the most recent major hurricane to make landfall in the region was Hurricane Carol in 1954.

On September 21, 1938, a Category 3 hurricane made landfall over New Haven, Connecticut with sustained winds of 115 mph (gusts of 150 mph) and a pressure of 941 millibars. Many coastal towns and cities on the Connecticut and Rhode Island coast suffered extreme damage. The coastal community of Napatree Point, Rhode Island was hit with a 20 - foot storm surge and the day after the cyclone was totally gone (34 killed). The cyclone produced very high wind gusts inland at higher elevations, delivering a 186 mph wind gust to the Blue Hill Observatory in Massachusetts, a 163 mph gust atop Mount Washington. A storm surge of 10-18 feet from Long Island Sound to Narragansett Bay, it is often considered to be the most intense hurricane to ever strike New England in modern times. One estimate from Rhode Island stated the water level "reflects a storm occurring roughly once every 400 years. A study of sand deposits also gives more evidence that this was the strongest hurricane to hit Rhode Island in over 300 years, since 1635."

Pre–17th century
Multiple intense hurricanes (Category 3+) are noted to have possibly struck New England in pre-Columbian times: between 1100 and 1150, 1300–1400 (1295–1407), and 1400–1450 (1404–1446), respectively.

17th century

 * Great Colonial Hurricane of 1635 track.png]]August 25, 1635 – The Great Colonial Hurricane struck Narragansett Bay, killing at least 46 people. This hurricane is often considered to be the most intense hurricane to hit New England since its European colonization. The only other storm of a similar magnitude was the 1938 hurricane.
 * August 23, 1683 – A tropical cyclone hit Connecticut and caused tremendous flooding.
 * October 29, 1693 – Another tropical cyclone struck New England and caused flooding so great that new permanent inlets were created.

18th century

 * October 18, 1703 – A tropical system caused great wind and flood damage; many ships were lost.
 * February 23, 1723 – An off-season storm struck Cape Cod causing a great deal of damage, but no reported deaths.
 * October 8, 1747 – Seven ships were destroyed, and "many" perished.
 * September 8, 1769 – A hurricane that earlier caused great damage in Annapolis, Maryland; blew ashore boats at Boston and adjacent areas, Providence, and Newport. Some houses were blown down and destroyed.
 * September 1775 – The Newfoundland hurricane apparently brought strong winds and/or waves to New England, though it is not known to have actually made landfall. This report may also be confused with the Independence Hurricane of September 2–3, 1775, which passed into New England from New York as a tropical depression or weak tropical storm.
 * August 13, 1778 – A weakening hurricane that struck the Carolinas, and impacted the coasts of Massachusetts and Rhode Island but did not make landfall. This storm prevented a major battle between England and France off the coast of Rhode Island.
 * November 1, 1778 – A possible late-season hurricane struck Cape Cod, Massachusetts, killing between 50 and 70 people. Twenty-three of these deaths are believed to be attributed to HMS Somerset III, a British ship which ran aground on Cape Cod during this storm.
 * October 8–9, 1782 – A hurricane struck the Carolinas and moved up the coast, causing damage in Providence, Rhode Island. It is currently not known if this hurricane made landfall in New England.
 * October 18–19, 1782 – A second hurricane moved up the coast and was considered more severe than the previous storm in portions of New England, especially Boston. This was a rare snow hurricane for New England and the storm was likely transforming into an extratropical cyclone as it approached the New England states.
 * September 24–25, 1785 – A hurricane which made landfall near Ocracoke, North Carolina, impacted southern New England. Based on known observations, this hurricane remained offshore of New England but passed close enough to inflict heavy rain and strong winds to New York City and Boston.
 * August 19, 1788 – A weakening hurricane moved up through eastern New York.

19th century

 * September 12, 1804 – The Antigua–Charleston hurricane, a major storm for the Caribbean, Georgia, and South Carolina, impacted portions of New England as a weakening tropical storm and then a tropical depression before dissipating off the coast of Nova Scotia.
 * October 9, 1804 – As the Snow hurricane crossed New England, cool air became entrained in the circulation, and it became extratropical. The storm brought heavy snow across the Northeast, in some areas up to 2 –, and killed a total of 16 people; one on land and fifteen at sea. This was the second observation of snow from a landfalling hurricane, but not the last. This hurricane which peaked at Category 3 intensity was a major one, especially for eastern Massachusetts.
 * October 3, 1805 – A hurricane that struck Mantanzas, Cuba reportedly reached the District of Maine (part of Massachusetts until 1820) as a tropical cyclone. Little information is available on this storm, however, a tropical cyclone exclusively striking Maine is not unique. This is what occurred during the passage of both Hurricane Gerda in 1969 and Tropical Storm Heidi in 1971.
 * September 1815 – What was once a major hurricane in the Carolinas brought tropical-storm-force winds to portions of New England. The likely track of this cyclone takes it very near but offshore of Nantucket.

 * September 23–24, 1815 – The 1815 New England hurricane struck New England as a major hurricane and delivered an 11 ft storm surge that funneled up Narragansett Bay. The hurricane destroyed some 500 houses and 35 ships and flooded Providence, Rhode Island. It also caused at least 38 deaths throughout New England.
 * August 12, 1817 – A hurricane that was first reported near Tobago made landfall on the Florida panhandle and moved slowly up the coast. As either a weak tropical storm or tropical depression, the system brought rain to New York and portions of New England on the 12th before moving into Quebec.
 * September 4, 1821 – The Norfolk and Long Island hurricane was a very powerful tropical cyclone that made landfall within the modern day limits of New York City. It sliced through New England and was likely extratropical as it moved along the Maine coastline.
 * June 4–5, 1825 – An early-season hurricane formed in late May near Santo Domingo and later struck Cuba, Florida, and South Carolina before moving up the Mid-Atlantic coast and into New England. Hurricane conditions were reported as far north as New York City, and the cyclone's status as a tropical cyclone in New England is debatable given the early date.
 * August 27, 1827 – The St. Kitts Hurricane impacted the eastern seaboard from Wilmington, North Carolina, to Portsmouth, New Hampshire. It is possible that this cyclone made landfall along the United States, but there are also conflicting reports that say it remained offshore of Cape Hatteras, Delaware, and Nantucket. August 1827 was a very active month with at least four hurricanes impacting the North Atlantic.
 * August 1830 – Two hurricanes passed close to southeastern Massachusetts within a week of each other. First came the Atlantic Coast Hurricane on August 19 followed by a second hurricane around the 25th. Damage from these two systems was duly noted on Nantucket. It appears that the later system approached the region from the southeast before turning out to sea southeast of Cape Cod.
 * October 11, 1830 – A third hurricane impacted New England in 1830 but like the two in August, this cyclone did not make landfall in New England. Barnstable, Massachusetts, reported the storm.
 * July 19, 1835 – The remnants of a hurricane that struck Florida twice moved into northern New England from New York.
 * August 30, 1839 – A hurricane moved up the east coast but did not make landfall. Fringe effects were felt on Long Island and southeastern New England.
 * October 3, 1841 – The October Gale became an extratropical storm, and passed off the coast of New England. The system dropped snow and sleet in Connecticut, bringing up to 18 in of snow in some areas. The storm wrecked the Georges Bank fishing fleet which drowned 81 fishermen and knocked down trees, tore roofs off houses and forced boats to go up on shore. The storm also destroyed a saltworks factory along Cape Cod, sending the economy to a slump. In 1842, a monument was erected to remember the sailors and fishermen lost at sea.
 * October 14, 1846 – The Great Havana Hurricane was still a strong tropical cyclone when it passed into New England from New York. In Hartford, Connecticut, hurricane-force winds destroyed a trestle bridge. Numerous apple orchards in Massachusetts were reported ruined. No deaths due to the hurricane's passage over New England were reported.
 * October 6, 1849 – A tropical cyclone made landfall in Massachusetts, causing 143 deaths. This was the first known tropical cyclone known to have made landfall in New England since June 1825.
 * 1850 – Three tropical cyclones impacted New England this season. The remnants of a July hurricane in the Carolinas passed into New England. An August hurricane caused damage in its wake through New England but was probably a tropical storm. Finally, a September hurricane passed off the coast causing some damage.
 * October 19, 1851 – A tropical storm formed north of the Bahamas on October 16. It continued northward and reached a peak intensity of 70 mi/h. But it weakened to a 60 mi/h-storm before making landfall in Rhode Island on the 19th. Later that day it dissipated on the border between Rhode Island and Massachusetts.
 * September 16, 1858 – A Category 1 hurricane made landfall on the Connecticut-Rhode Island border and brought heavy rain to New England before exiting Maine as a tropical storm. It then continued northeast until it dissipated just over the other side of the Gulf of St. Lawrence on the 17th.
 * September 28, 1861 – The Equinoctial Storm hit Connecticut as a 60 mi/h tropical storm. It then continued east-northeast and dissipated in extreme eastern Maine later that day.
 * November 3, 1861 – The Expedition hurricane struck eastern Connecticut as a 60 mi/h tropical storm. It then continued northeast until dissipating over southern Maine later that day.
 * September 19, 1863 – A tropical storm makes landfall in New York and brings strong winds to western New England.
 * October 30, 1866 – A tropical storm made landfall in New Jersey, Long Island, and New York City and began to parallel the New York-New England border until it briefly enters Vermont and dissipates.
 * September 8, 1869 – A Category 3 hurricane made landfall in Rhode Island, before moving north and dissipating in Maine. There was one confirmed death in Massachusetts. Offshore Maine, a schooner capsized, killing all but one of the twelve crew. The storm also caused at least $50,000 (1869 USD) in damage in Maine alone.
 * October 4, 1869 – The Saxby Gale crossed Cape Cod and Martha's Vineyard as a Category 2 hurricane, before striking Maine as a Category 1 hurricane. In Maine, heavy rainfall caused widespread flooding, and high winds destroyed at least 90 houses. A very high storm tide also occurred in the Bay of Fundy, and the storm killed at least 37 people offshore of Nova Scotia.
 * October 9–13, 1878 – A Category 1 hurricane passes offshore, resulting in heavy rains and strong winds, causing 27 deaths.
 * October 10, 1894 – A Category 1 hurricane struck Connecticut.
 * September 10, 1896 – A Category 1 hurricane struck Massachusetts.
 * September 24, 1897 – A tropical storm hit Connecticut with maximum sustained winds of 50 mi/h. It continued up through all the New England states except for Vermont.
 * October 6, 1898 – A hurricane came from the west and hit Maine as a tropical depression, then continued east into Atlantic Canada.
 * November 1, 1899 – A hurricane struck New England as a 50 mi/h extratropical storm.

20th century

 * August 1904 – An extratropical storm with hurricane-force winds left behind damage in southeastern Massachusetts, especially Martha's Vineyard. Trees were downed in Providence, Rhode Island, and New Bedford, Massachusetts. Center moved NE just within the coastline from Carolinas, with its eastern sector intact over ocean. The storm then tracked across Long Island and eastern Rhode Island. Much marine destruction with heavy losses in Buzzards Bay, Vineyard Sound and Massachusetts Bay.
 * July 21, 1916 – A Category 1 hurricane moved north from open Atlantic, crossing the Buzzards Bay/Cape Cod area of Massachusetts. Hourly wind reports indicated sustained 50 mi/h but actual winds were higher than hourly observations. Gusts of 85 mi/h recorded in southeast Massachusetts and Cape Cod.
 * August 1917 – A tropical storm sank four ships while passing offshore of Nantucket, Massachusetts, killing 41 sailors. The storm later made landfall in New Brunswick before becoming post-tropical.
 * August 1924 – A Category 1 hurricane with a large center moved over and just east of Cape Cod. It was a severe hurricane in New Bedford and Martha's Vineyard, Massachusetts. New Bedford Newspaper (Mercury) published photo journal of the hurricanes severity. The system is often overlooked, however much material is present to include it as destructive storm. On Cape Cod, Martha's Vineyard and Nantucket, it is often considered worse than the 1938 hurricane. Widespread wind losses to structures were reported. Very heavy tree damage in New Bedford north to Plymouth Massachusetts. The storm was later destructive in Nova Scotia.
 * November 3–4, 1927 – The remnants of a tropical storm spawned torrential rains as it passed over the Green Mountains in Vermont. The record flooding caused $40 million in damage and killed 84 people in Vermont and 1 in Rhode Island. The storm ended as snow in the mountains. Note that this flood was unrelated to the 1927 Mississippi Flood.
 * September 9, 1934 – A strong tropical storm crossed Long Island and lost strength from slow movement as it moved through Connecticut much in a similar manner as Hurricane Belle of August 1976. Trees downed in Providence, Rhode Island, and New Haven, Conn.
 * September 1936 – A Category 1 hurricane moved east-northeast over Block Island and Nantucket Sounds after moving up East Coast of U.S. north of North Carolina and Virginia. The storm was destructive in Providence, Rhode Island, and eastern Massachusetts. Boston had 80 mi/h winds at 8 a.m. on the 18th as the storm moved east along the south coast of Cape Cod and the Islands. There was much media coverage, but this storm was later eclipsed by the extreme hurricane two years later. Heavy wind-damage was realized across all of eastern Massachusetts.

 * September 21, 1938 – 1938 New England hurricane – This storm made landfall on Long Island and Connecticut as a Category 3 hurricane. Wind gusts reached Category 5 strength in eastern Connecticut, Rhode Island and southern Massachusetts west of Buzzards Bay and Cape Cod. The anemometer at the Blue Hill Observatory registered a peak wind gust of 186 mi/h before the instrument broke. The hurricane lost strength as it tracked into interior areas of New England, but it is believed to have been at Category 2 intensity as it crossed into Vermont and at minimal Category 1 intensity as it tracked into Quebec. The storm killed over 600 people and is considered to be the worst hurricane to strike New England in modern times.
 * September 15, 1944 – The Great Atlantic Hurricane made landfall near the Connecticut/Rhode Island border as a Category 1 hurricane, causing severe wind damage in southeastern Massachusetts and across the Cape and Islands. Damage on Cape Cod and Martha's Vineyard was considered worse than that in 1938, with severe wind damage in New Bedford, Massachusetts. Much structural damage and much of the forest that had somehow escaped being decimated in 1938 fell victim to this storm. A total of 28 people died in New England due to the hurricane.
 * September 1950 – Hurricane Dog was a major offshore hurricane that moved very close to Nantucket. Hurricane conditions occurred across southeast Massachusetts. Winds gusted near hurricane force on Nantucket and along the New England coast.
 * September 7, 1953 – Hurricane Carol made landfall near Saint John, New Brunswick, Canada, with considerable wind losses throughout the region. This hurricane was eclipsed by the extreme damage of another Carol the very next year.

 * August 31, 1954 – Hurricane Carol made landfall as a Category 3 hurricane, with gusts of Category 4 strength in southeast Rhode Island and south-coastal Massachusetts in the Buzzards Bay area, west of Cape Cod. Wind gusts of 135 mi/h at Block Island, Rhode Island, and 125 mi/h in Milton, Massachusetts, were recorded. At least 68 people were killed across New England. Extreme damage was reported in south coastal Rhode Island and south coastal Massachusetts. Damage in the Buzzards Bay region rivaled that of the 1938 hurricane.
 * September 11, 1954 – Hurricane Edna made landfall on Cape Cod and Martha's Vineyard as a strong Category 2 hurricane, just two weeks after Carol, with very severe losses occurring. Hourly wind readings of 90 mi/h were recorded at New Bedford Airport in New Bedford, Massachusetts; 100 mi/h in Taunton, Massachusetts, 112 mi/h in Milton, Massachusetts, and 125 mi/h in Chilmark, Martha's Vineyard.
 * July 11, 1959 – Hurricane Cindy scrapes New England.
 * September 12–13, 1960 – Hurricane Donna makes landfall on Long Island, New York as a minimal Category 2 hurricane, and in Connecticut as a strong Category 1 hurricane. Peak wind gusts of 140 mi/h at the Blue Hill Observatory in Massachusetts and 135 mi/h on Block Island, Rhode Island. Hourly peak wind gusts at New Bedford Airport in Massachusetts recorded 110 mi/h winds from the south-southwest in a sheltered area. Heavy tree, utility, and structural damage was observed in southeastern Massachusetts, coastal New Hampshire and Maine. Donna was the sixth hurricane to hit southern New England in thirty years. Hourly wind speed readings at City Hall in downtown New Bedford, Massachusetts recorded 80 mi/h winds.
 * September 26, 1961 – Hurricane Esther moved within 35 miles of the south coast of Rhode Island and Massachusetts as a Category 1 hurricane, before subsequently making a sharp right turn and then making a loop, returning as a tropical storm five days later. Esther remained offshore, but produced hurricane-force wind-gusts from Block Island, Rhode Island, eastward across Cape Cod, Massachusetts, Nantucket, and Martha's Vineyard. There was less damage than in Hurricane Donna one year prior. Wind gusts of 75 mi/h to 90 mi/h occurred onshore.
 * October 7–8, 1962 – Hurricane Daisy remained offshore, but produced hurricane conditions in coastal northeastern Maine and on Mt. Desert Island.
 * October 29, 1963 – Hurricane Ginny remained offshore, but produced hurricane conditions in Nantucket, Massachusetts, and along coastal northeastern Maine.
 * September 8–11, 1969 – Hurricane Gerda brushed Cape Cod and made landfall at Eastport, Maine. No people were killed, though the storm was one of the strongest to hit Maine.
 * August 28, 1971 – Tropical Storm Doria moved into Connecticut after crossing Long Island. Hurricane-force winds were measured at sea level in Bridgeport, Connecticut. Wind gusts up to 80 mi/h in southeastern Massachusetts and Blue Hill Observatory.
 * September 3, 1972 – Tropical Storm Carrie passed offshore of Cape Cod as a tropical storm, producing hurricane-force wind gusts of 90 mi/h in Plymouth, Massachusetts, and 100 mi/h in Hyannis, Massachusetts.
 * August 10, 1976 – Hurricane Belle's rather slow movement enabled weakening to set in as the storm approached Long Island, New York, and then moved into Connecticut and Massachusetts, before transversing the Vermont/New Hampshire border. Wind gusts up to 90 mi/h were observed in southern Connecticut, 60 mi/h in Providence, Rhode Island, and 75 mi/h in Newport, Rhode Island.Gloria 1985-09-27 1550Z.jpg
 * September 27, 1985 – Hurricane Gloria crosses Long Island and Connecticut as a Category 1 hurricane, making it the first hurricane of significant strength to hit southern New England since 1960. Widespread wind damage was reported in Connecticut, Rhode Island, and Massachusetts, and later across coastal New Hampshire and Maine. The tree damage in Connecticut was the worst since the 1938 hurricane, and wind losses in Rhode Island and eastern Massachusetts were considerable to trees, utilities, and roofs. New Bedford, Massachusetts, reported wind gusts over 90 mi/h, and in Rehoboth, Massachusetts, police barracks observed 120 mi/h winds and also later reported a tornado in the vicinity. Winds at the T. F. Green Airport in Warwick, Rhode Island, gusted to 85 mi/h, and winds of 100 mi/h were recorded on east side of Providence, near Brown University. In addition, winds in New London, Connecticut, were clocked at 110 mi/h to 112 mi/h. Widespread forest damage occurred in Maine. Gloria also produced hurricane-force wind-gusts into New Brunswick, Canada.

 * August 19, 1991 – Hurricane Bob made landfall on Block Island, Rhode Island, and Newport, Rhode Island, as a Category 2 hurricane. Winds gusted to Category 3 strength in southeastern Massachusetts. Bob was one of the smallest in area and yet most intense hurricanes to hit southern New England since 1938. Storm surge in the Buzzards Bay area of Massachusetts was comparable to that of Hurricane Carol; Bob was considered to be the worst storm on Martha's Vineyard since the 1944 hurricane. This hurricane was among the top twenty-five costliest U.S. hurricanes of twentieth century. The 1938 and 1944 hurricanes, as well as Carol in 1954, Donna in 1960, and Bob in 1991, are all on the list. A tidal surge of 10 ft above normal was recorded in upper reaches of Buzzards Bay. A wind gust of 135 mi/h was recorded at Block Island before the anemometer blew away. A 125 mi/hh wind-gust was recorded in Newport, Rhode Island, and a 5-minute sustained wind speed of 111 mi/h with gusts to 144 mi/h was observed at Westport Harbour on the south coastal border of southern Massachusetts and Rhode Island. Additional wind recordings include a 120 mi/h gust at the Massachusetts Maritime Academy on Buzzards Bay and a 120 mi/h gust in Truro, Massachusetts. A one-minute sustained wind speed of 110 mi/h was recorded on Chappaquiddick Island, Massachusetts. Several private anemometers in Falmouth, Massachusetts, on Cape Cod reported unofficial gusts of 150 mi/h. A New Bedford fishing boat off Cuttyhunk Island, Massachusetts, reported a peak gust of 162 mi/h.
 * October 30 – November 1, 1991 – The Perfect Storm remained offshore, but produced wind gusts to 77 mi/h over Cape Cod, and as far west as Jamestown, Rhode Island. Coastal damage was very high in exposed eastern Massachusetts due to high waves and tidal surge. Minor wind damage came just two months after Hurricane Bob, which produced major damage over southeast Massachusetts.
 * August 28, 1992 – The remnants of Hurricane Andrew combined with a frontal boundary, and moved from the Mid-Atlantic states into New England. The system dropped light rain and produced light wind across the region.
 * September 26, 1992 – The remnants of Tropical Storm Danielle moved just west of New England, but caused rainy conditions throughout the region.
 * July 13, 1996 – Tropical Storm Bertha moved into southern New England as a strong tropical storm with 70 mi/h sustained winds, and in some exposed areas, winds gusted to minimal hurricane force in southern Rhode Island and south coastal Massachusetts, west of Buzzards Bay. Overall, Bertha produced minor damage, but notable damage in coastal Rhode Island.
 * September 2, 1996 – Hurricane Edouard passed offshore as a Category 1 hurricane, producing strong wind-gusts from Buzzards Bay eastward across Cape Cod and the islands of Nantucket and Martha's Vineyard. On Cape Cod, Edouard was a worse storm than Gloria in 1985, but not so destructive as Bob in 1991, which has become a benchmark hurricane on Cape Cod. Considerable losses occurred across Massachusetts, particularly in Oak Bluffs and Martha's Vineyard.
 * October 8, 1996 – The remnants of Tropical Storm Josephine brushed Cape Cod, dropping widespread light rain and wind gusts of 45 mi/h to 60 mi/h in New Bedford, Massachusetts.
 * July 26, 1997 – Tropical Storm Danny stalled just to the south of Nantucket, causing only minor damage, despite strong winds that were experienced in southeastern Massachusetts. The minor damage included minimal flooding, power outages, and downed tree limbs.
 * September 17–18, 1999 – After paralleling much of the U.S. East Coast, Tropical Storm Floyd moved into Connecticut and tracked northward through Maine. Floyd caused large power-outages and major flood damage across the region, with over 5 in of rain falling over most of the area. Danbury, Connecticut, received up to 15 in of rain from the storm, resulting in extensive flooding in the city and surrounding areas. Mudslides were reported in the Berkshire Mountains of western Massachusetts. Several major highways and a countless number of local roads in Connecticut and Massachusetts were closed for several days due to flooding and downed trees and power lines. Hurricane-force wind gusts were observed in southern Rhode Island; North Kingston unofficially reported wind gusts to 90 mi/h. Wind gusts to 76 mi/h were recorded at the New Bedford Hurricane Dike in New Bedford, Massachusetts, and 73 mi/h in Hyannis, Massachusetts.

21st century

 * June 17, 2001 – Tropical Storm Allison brushed southern New England as a subtropical storm. In Connecticut, rainfall peaked at 7.2 in in Pomfret, closing several roads, causing minor damage to numerous houses. In Rhode Island, the rainfall washed out several roads.
 * September 11, 2002 – The interaction between Hurricane Gustav and the non-tropical system caused strong winds that affected areas of coastal New England, mainly in eastern New York and Massachusetts. The winds downed trees and power lines, and several homes and cars were damaged by falling trees; about 19,000 homes lost power in Massachusetts.
 * September 2002 – The remnants of Tropical Storm Hanna contributed to around 1 in (25 mm) of rainfall in Vermont.
 * September 28, 2002 – The extratropical remnants of Hurricane Isidore produced widespread light rainfall across the region. No damage or flooding was reported.
 * September 2003 – Hurricane Fabian produced moderate surfing conditions along the East Coast of the United States.
 * September 4, 2003 – The remnants of Tropical Storm Grace dropped light to moderate rainfall throughout the region, though no significant damages were reported.
 * September 17, 2003 – The dissipating remnants of Tropical Storm Henri produced light rainfall. Hermine 2004-08-30 1535Z.jpg
 * September 19, 2003 – Hurricane Isabel passed far to the west, though rainfall reached 1 inch (25 mm) in portions of western Connecticut and Massachusetts, and in portions of New Hampshire and Maine. Falling trees from moderate winds downed power lines across the region, causing sporadic power outages. Two people died as a result of the hurricane, both due to the rough surf. Damage in Vermont totals about $100,000 (2003 USD, $117,000 in 2008 USD).
 * October 2003 – The interaction between Hurricane Kate and a high-pressure area to its north produced 3 to 4 foot (1 m) waves along the coast.
 * August 14, 2004 – The extratropical remnants of Tropical Storm Bonnie produced heavy rainfall, with localized totals of up to 10 in. The rainfall flooded or washed out roads across the eastern Maine. In Aroostook County, Maine, the rainfall caused a mudslide, narrowing a county road to one lane.
 * August 15, 2004 – Tropical Storm Charley dissipated near southern Massachusetts, though the remnant moisture produced up to 5 in of rainfall, particularly in Maine. In Rhode Island, one man drowned in a rip current generated by the system.
 * August 31, 2004 – Moisture from Hurricane Gaston dropped up to 3.69 in of rainfall.
 * August 31, 2004 – Tropical Storm Hermine comes ashore near New Bedford, Massachusetts, as a minimal tropical storm. Damage was minimal, and effects were limited to gusty winds and light rainfall.
 * September 10, 2004 – The remnants of Hurricane Frances produced light, yet widespread rainfall; the system eventually crossed northern Maine.
 * September 19, 2004 – A plume of moisture broke off from the remnants of Hurricane Ivan and progressed northward, producing heavy rainfall across portions of the Mid-Atlantic and New England. The rain caused extensive roadway flooding in Connecticut, and resulted in minor river flooding in other areas.
 * September 29, 2004 – Moisture from the remnants of Hurricane Jeanne storm produced light to heavy rainfall, with totals of over 7 in on Nantucket.

 * June 15, 2005 – After being absorbed into a frontal wave, the remnants of Tropical Storm Arlene drop light rainfall in Northern New England.

 * July 8, 2005 – The extratropical remnants of Hurricane Cindy produced moderate rainfall in northern Vermont, generally within the range of 1 to 3 in.
 * August 31, 2005 – The remnants of Hurricane Katrina dropped up to 4.17 in of rain and cause gusty winds that blew down trees and tree limbs, primarily across Vermont, New Hampshire, and Massachusetts.
 * September 17, 2005 – Hurricane Ophelia brushed Massachusetts with gusty winds and heavy rainfall.

 * October 7–12, 2005 – The remnants of Tropical Storm Tammy and Subtropical Depression Twenty-Two (2005) contributed to the Northeast U.S. flooding of October 2005, which killed 10 people and contributed to the wettest month on record in locations throughout the Northeastern United States.
 * June 15, 2006 – The extratropical remnants of Tropical Storm Alberto dropped rainfall throughout the region, peaking at 1.98 in at Windsor Locks, Connecticut.
 * July 21, 2006 – Tropical Storm Beryl makes landfall on Nantucket, generating waves 10 ft in height as the storm approached the island. Light rainfall and gusty winds were also reported there, and in portions of Massachusetts.
 * September 3, 2006 – The extratropical remnants of Hurricane Ernesto dropped light rainfall; 1.72 in of precipitation was reported at Marlboro, Vermont.
 * June 4, 2007 – The extratropical remnants of Tropical Storm Barry entered the region, producing moderate rainfall that peaked at 3.2 in at Taunton, Massachusetts.

 * November 3, 2007 – As a powerful extratropical storm, Hurricane Noel hit coastal Massachusetts, Rhode Island and Maine with hurricane-force wind-gusts of up to 89 mph, with sustained winds topping out at 59 mph. Power outages were widespread; about 80,000 customers in Massachusetts, mostly on Cape Cod, and 9,000 in Maine lost electric power. Heavy rainfall, high seas, and coastal flooding also occurred.
 * September 6, 2008 – Tropical Storm Hanna made landfall at Myrtle Beach, South Carolina, and proceeded northeastward through the Mid Atlantic states and New England, dropping moderate to heavy rainfall and spawning gusty winds across southern New England.
 * September 15, 2008 – The remnants of Hurricane Ike reached northern New England, though no effects were reported.
 * September 28, 2008 – Hurricane Kyle passed to the east as it heads towards Canada, affecting Maine with heavy rainfall and gusty winds that caused scattered power outages. Up to 7.15 in of precipitation falls in Hancock County, Maine.
 * August 21, 2009 – Hurricane Bill passed just offshore of New England causing very heavy surf, and a period of rain and gusty winds over Southeastern Massachusetts.

 * August 29, 2009 – Tropical Storm Danny passes over Nantucket as an extratropical storm, causing up to 2 in of rain in Massachusetts and Rhode Island, and bringing wind gusts up to 60 mi/h off the coast of Nantucket and Maine.

 * November 12, 2009 – Hurricane Ida, after hitting the northeast gulf coast as a tropical storm, redeveloped off the Carolina coast as a strong nor'easter, bringing severe damage as far north as New Jersey, where severe flooding, beach erosion, and strong winds were reported. As the center of the storm moved out to sea, a batch of moisture broke off it, and moved north, bringing moderate rain to New England. The storm caused millions of dollars in damage.

 * September 4, 2010 – Hurricane Earl passed about 90 miles offshore, but still brought heavy rain, large waves, and tropical storm force gusts to Cape Cod. The heaviest rain affected areas such as Nantucket, Martha's Vineyard, and areas over Maine, while the strongest wind was a recorded gust of 58 mi/h near Hyannis, Massachusetts. Sustained winds were of 29 to 35 miles per hour, just at and below tropical storm force.

 * August 28, 2011 – Hurricane Irene weakened to a tropical storm just before its landfall in New York, striking with winds of 70 mi/h. Irene produced high winds, heavy rains, and flash flooding especially in western New England. The storm left at least 16 people dead throughout New England, including ten deaths in Connecticut. The eastern quadrant of Irene remained intact, as that section had never transversed land and moved north-northeast across southern Bristol and Plymouth counties in Massachusetts. Winds at times reached hurricane force from Westport east to Woods Hole on the south coast.

 * October 29–30, 2012 – Hurricane Sandy affected Southern New England with its outer bands producing heavy storm surge, winds, and rainfall before the storm's landfall in New Jersey. Sandy devastated the Jersey Shore, New York City, parts of Long Island and the Connecticut and Rhode Island coastlines. Flooding and power outages (roughly nine million customers total) lasted several days, while thousands of trees, telephone poles and traffic light stanchions were snapped. A total of approximately $71.4 billion in property damage was left in Sandy's wake after it made landfall and its center went over Pennsylvania and New York. Sandy killed 5 people in New England (4 in Connecticut and 1 in New Hampshire). To the west, Sandy dumped 2 – of snow in the Appalachian Mountain region and flatlands.
 * Jose 2017-09-19 1540Z.jpger 2–5, 2015 – Hurricane Joaquin, at one point forecast to make a landfall in New England, eventually passed offshore and produced high surf along Cape Cod and Nantucket.
 * September 19–22, 2017 – Hurricane Jose stalled to the south of New England, meandering offshore for several days. This resulted in major rainfall and high winds throughout the region, particularly on Cape Cod, Martha's Vineyard, and Nantucket. Rainfall peaked at 6.4 in on Nantucket, and maximum sustained winds reached 53 mi/h miles per hour in Cuttyhunk, with gusts up to 62 mi/h recorded on Martha's Vineyard and Nantucket.

 * October 29–30, 2017 – The combination of Tropical Storm Philippe and an extratropical system resulted in approximately 1.2 million power outages in New England. The system produced storm-force sustained winds, reaching 57 mi/h in Warwick, Rhode Island, and hurricane-force wind gusts, peaking at 93 mi/h in Popponesset, Massachusetts. In addition, the system dropped several inches of rain, peaking at 5.5 in in Canton, Connecticut.

 * September 18, 2018 – The remnants of Hurricane Florence passed through the region, resulting in gusty winds and heavy rainfall. A maximum of 7.0 in of rainfall was recorded in Baldwinville, Massachusetts.
 * October 12, 2018 – The remnants of Hurricane Michael passed through southeastern Massachusetts, dropping 5 to 6 inches (130 to 150 mm) of rainfall on Cape Cod.[[File:Snow produced from the remnants of Hurricane Zeta across Eastern Massachusetts..jpg|thumb|Snow produced from the remnants of Hurricane Zeta blanketing Eastern Massachusetts on October 30, 2020.]]

 * Early September 2019 – Hurricane Dorian brushed Nantucket, Cape Cod and Martha's Vineyard in eastern Massachusetts; it produced tropical storm force winds and light-to-moderate rain. The storm later brushed southeast Maine as it hit Nova Scotia.

 * October 11–13, 2019 – Tropical Storm Melissa brought rainfall, coastal flooding, and strong swells to southeastern New England.
 * July 9, 2020 – Tropical Storm Fay made landfall on New Jersey and triggered multiple meteorological warnings for much of New England.

 * August 4, 2020 – Tropical Storm Isaias made landfall near North Carolina but maintained tropical storm strength well into New England, causing extensive power outages and tree damage, particularly in Connecticut. The storm became extratropical over Vermont.

 * October 30, 2020 – Post-tropical Storm Zeta brought over half a foot of snow accumulation in parts of New England, resulting in power outages, downed trees, and numerous crashes, some serious. Several injuries from crashes were also reported.

 * August 22, 2021 – Tropical Storm Henri made landfall near Westerly, Rhode Island, bringing strong winds and heavy rainfall to southern New England, which caused widespread flooding and severe weather. It was the first tropical cyclone to strike Rhode Island since Hurricane Bob in 1991.

 * September 1, 2021 - Post-Tropical Cyclone Ida brought deadly flash flooding across Northeastern U.S., including to New England.

Landfalls
A landfall in New England occurs only if the center of the storm comes ashore in Maine, New Hampshire, Massachusetts, Rhode Island, or Connecticut as they all share a coastline. Tropical cyclones that made landfall outside of New England, but subsequently passed through the region, are excluded from this category. For example, the 1893 New York hurricane, Tropical Storm Doria of 1971, and Hurricane Irene of 2011 all made landfall in New York City, but failed to cross Long Island Sound and enter Connecticut along its coastline. In addition, other systems such as the 1876 San Felipe hurricane, 1888 Louisiana hurricane, 1893 Sea Islands hurricane, and Hurricane Able of 1952 all passed through New York, to the north of New York City, before entering New England.

A landfall is also distinct from a direct hit, in which the eyewall, or core of the highest winds, comes onshore, without the center of the storm moving ashore.

New England hurricanes have made landfall on many occasions. Normally, due to cold SSTs and high wind shear, hurricanes do not last long, so the ones that do make landfall are normally weak, with major hurricanes (Category 3 or higher) being rare.

The following tables are a list of all tropical cyclones that have made landfall in New England since records began in 1851:

19th century
The 19th century saw a few notable storms. In 1869 an intense Category 3 hurricane struck Southeastern New England. Other hurricanes that made landfall include the Equinoctial Storm, Expedition hurricane, and the Saxby Gale. Since hurricanes were not named and fewer records were kept at the time, the information on some of the storms remains incomplete.

20th century
The 20th century saw eight hurricanes making landfall in New England; out of these the more notable include the 1938 New England hurricane (also called the Long Island Express), which made landfall as a major hurricane; Hurricane Carol did the same sixteen years later. The last hurricane to make landfall in New England was Hurricane Bob in 1991 as a Category 2 hurricane with maximum sustained winds of 100 mph.

21st century
So far in the 21st century, five tropical cyclones have made landfall in New England: Tropical Storm Hermine in 2004, which made landfall in southeastern Massachusetts; Tropical Storm Beryl in 2006, which made landfall in Nantucket; Tropical Storm Hanna in 2008, which made landfall in Connecticut; and Tropical Storms Elsa and Henri in 2021, which both made landfall in Rhode Island.

Deadliest storms
Some tropical cyclones that have impacted New England have resulted in fatalities in the region. The most notorious and deadly of these storms is the 1938 New England hurricane which killed between 682 and 800 people. This list includes all tropical cyclones that have resulted in at least 10 deaths in New England. Some storms may be excluded or their death toll may be inaccurate due to a lack of available data at the time.

title: List of New England hurricanes


text:
Victoria Park (constituency)

Victoria Park, formerly called Causeway Bay North, is one of the 13 constituencies of the Wan Chai District Council of Hong Kong. The seat elects one member of the council every four years. It was first created in Hong Kong district board elections, 1994. The constituency boundary is loosely based on the residential area east of the Victoria Park with estimated population of 13,412. Prior to the District Council election in 2015, it was a constituency of the Eastern District Council.

title: Victoria Park (constituency)


text:
Πύλος

Etymology
Compare 🇨🇬

Proper noun

 * 1) Pylos, Messenia, Greece

Proper noun

 * 1) Pylus, a figure in Greek mythology

title: Πύλος


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1965 Memphis State Tigers football team

The 1965 Memphis State Tigers football team represented Memphis State College (now known as the University of Memphis) as an independent during the 1965 NCAA University Division football season. In its eighth season under head coach Billy J. Murphy, the team compiled a 5–5 record and outscored opponents by a total of 215 to 153. Don McClard, Billy Fletcher, and Harry Day were the team captains. The team played its home games at Memphis Memorial Stadium in Memphis, Tennessee.

The team's statistical leaders included Billy Fletcher with 1,239 passing yards and 556 rushing yards and Bob Sherlag with 673 receiving yards and 54 points scored.

title: 1965 Memphis State Tigers football team


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Caroline Adderson

Caroline Adderson (born September 9, 1963) is a Canadian novelist and short story writer. She has published four novels, two short story collections and two books for young readers.

Biography
Adderson was born on September 9, 1963, in Edmonton, Alberta to James Neil and Bernice Adderson.

She received a Bachelor of Education degree from the University of British Columbia in 1986. Following graduation, she attended a writing program at the Banff Centre for Arts and Creativity.

Aside from writing, she has taught at the Banff Centre for Arts and Creativity and Simon Fraser University.

Adderson presently lives in Vancouver with her husband, Bruce Sweeney.

Awards and honours
In 2006, Adderson received the Marian Engel Award, "given annually to an outstanding Canadian female writer in mid-career in recognition of her body of work."

In 2010, Quill & Quire and The Globe and Mail named The Sky is Falling one of the best books of the year.

As editor

 * Vancouver Vanishes: Narratives of Demolition and Revival (2016)
 * Best Canadian Stories 2019 (2019)

Short story collections

 * Bad Imaginings (1993, ISBN 0-88984-172-1)
 * Pleased to Meet You: Stories (2006, ISBN 0-88762-220-8)
 * Sunny Days Inside (2021)

Novels

 * A History of Forgetting (1999)
 * Sitting Practice (2003, ISBN 0-88762-129-5)
 * The Sky is Falling (2010, Thomas Allen Publishers)
 * Ellen in Pieces (2014, ISBN 1-443-42678-4)
 * A Russian Sister (2020)

Novella

 * Mr. Justice (2005, ISBN 0-9735881-3-6)

Children's fiction

 * Very Serious Children (2007)
 * Middle of Nowhere (2012)
 * Norman, Speak!, illustrated by Qin Leng (2014)
 * A Simple Case of Angels (2014)
 * Eat, Leo! Eat!, illustrated by Josée Bisaillon (2015)
 * I Love You, One to Ten, illustrated by Christina Leist (2015)
 * The Mostly True Story of Pudding Tat, Adventuring Cat, illustrated by Stacy Innerst (2019)
 * It Happened on Sweet Street, illustrated by Stéphane Jorisch (2020)
 * Babble!: And How Punctuation Saved It, illustrated by Roman Muradov (2022)

Bruno series

 * I, Bruno, illustrated by Helen Flook (2007)
 * Bruno for Real, illustrated by Helen Flook (2008)

Izzy series
The Izzy books are illustrated by Kelly Collier.

 * Izzy in the Doghouse
 * Izzy's Tail of Trouble (2022)
 * Izzy's Dog Days of Summer (2023)

Jasper John Dooley series

 * 1) Star of the Week, illustrated by Ben Clanton (2012)
 * 2) Left Behind, illustrated by Ben Clanton (2013)
 * 3) Not in Love, illustrated by Ben Clanton (2014)
 * 4) You're in Trouble, illustrated by Ben Clanton (2015)
 * 5) Lost and Found, illustrated by Mike Shiell (2015)
 * 6) Public Library Enemy #1, illustrated by Mike Shiell (2016)

Pierre & Paul series
The Pierre & Paul books are illustrated by Alice Carter.

 * Avalanche! (2020)
 * Dragon! (2021)

title: Caroline Adderson


text:
User:Avula bharati

MISS INDIA UAE : GEETANJALI KELATH
Ms Geetanjali Kelath being very young has achieved more than a student of her age could ,the 19 years old MBA student who was rewarded as the  Miss Coimbatore in India has also won the title of Miss INDIA UAE  in  UAE.She  is a very good athelete and a very good singer. She made her parents and family relatives and her friends  very proud.

title: User:Avula bharati


text:
1941 North Texas State Teachers Eagles football team

The 1941 North Texas State Teachers Eagles football team represented the North Texas State Teachers College (later renamed the University of North Texas) as a member of the Lone Star Conference (LSC) during the 1941 college football season. In its 13th and final season under head coach Jack Sisco, the team compiled a 7–1 record (4–0 against LSC opponents) and won the LSC championship. The team's loss was against SMU.

North Texas was ranked at No. 160 (out of 681 teams) in the final rankings under the Litkenhous Difference by Score System.

The team played its home games at Eagle Field in Denton, Texas.


text:
Talk:Feroz Khan (actor)/Archive 1

Untitled
I think it is wrong to say Feroz's father was an Afghan hailing from Ghazni province in Afghanistan. The term Tanoli is a Hazara version of the Afghanistani Taniwal/Tanavoli tribe. Tanolis usually cite this connection and refer to Ghazni as their original homed before travelling to their present abode in Hazara with the army of Mahmood Ghaznavi. It is this historical memory that is alive and well among majority of Hazara Tanolis. Also it was only in 1901 that Hazara, along with other areas of Eastern Afghanistan, was incorporated into British IndIAwith Amb given princely state status. People of the new North West Frontier continues to call themselves as being from Afghanistan for most of the first half of 20th century - Nowjawan e Afghan was a popular newspaper based in Hazara district before partition of 'India' So the claim by Feroz Khan and his family is about historical origin of the family rather than contemporary period. The couple with their legendary enmity towards Pakistan may explain their reluctance to face the truth of their origin in the Pakistani province of Pakhtunkhwa. 5 November 2011, 17:00, User: Moarrikh —Preceding undated comment added 17:04, 5 November 2011 (UTC).

Tanolis are not native Indians nor is the area of Pakistan that is west of River Indus/Darya e Sindh/Abaseen part of South Asian subcontinent. Baluchistan is historically part of Persia and thus middle eastern whereas North Western Frontier Province was until the end of 19th century Eastern Afghanistan province of the kingdom of Afghanistan thus central Asian. Therefore for pashtuns/pathans to call themselves Afghan or descended from Afghans is correct and proper. This fact is reflected in the name of the state called Pakistan: P is for Punjab; A for Afghnia; K for Kashmir; i for the diacritical mark 'zer' or e/i;S for Sindh; and S for Stan - together the acronym PAKISTAN means land of the pure. If you guys can't stomach that then seek therapy but the above is historical reality. There was no forcible conversion but a missionary work by sufis, conquored Hindus converting for status and prestige and intermarriage - see Anglo Indian origins.User: Moarrikh 22:03, 25 November 2011.

 * The reliable news reports state that Feroz Khan's father was an ethnic Pashtun (known in India as "Pathan") and his mother was Iranian.--Nasir Ghobar (talk) 02:16, 24 August 2012 (UTC)

 * That's correct. But some editors keep reinserting "Tanoli". --Enric Naval (talk) 18:53, 24 September 2014 (UTC)

title: Talk:Feroz Khan (actor)/Archive 1


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Porfirio Fisac

Porfirio Fisac de Diego (born January 24, 1965) is a Spanish basketball coach for Casademont Zaragoza of the Liga ACB. He was the head coach of the Senegalese national team, participant at the AfroBasket 2017.

Coaching career
Born in Fuenterrebollo, Segovia, Castile and León, the first sporting success of Fisac arrived in 2002, by promoting CB Tarragona to the LEB league. He would repeat promotion two years later with Ciudad de Algeciras.

In 2004, Fisac signed with Gipuzkoa BC, again in the LEB 2 league (third tier). In his first season, despite finishing as regular season winners, he could not achieve a new promotion due to being eliminated in the quarterfinals by CB Canarias. However, the club bought the LEB place of his former club Ciudad de Algeciras.

In the club's debut season in LEB, despite finishing the regular season in the sixth position, Gipuzkoa BC completed a perfect playoff with seven wins and no defeats and promoted to the Liga ACB. In the next season, he could not avoid the last position and ended his stage at Gipuzkoa. Fisac compared the relegation of the club with the death of his father.

After one season without coaching, Fisac took the helm of freshly relegated from Liga ACB CB Valladolid and achieved the promotion in his first season, and qualified the team to the Copa del Rey in 2011. He ended the contract in that year and signed with Baloncesto Fuenlabrada, where he was sacked.

Two years later, he came back to Valladolid, for coaching the club in their last season before relegation and in 2015, after starting the season with Palencia Baloncesto, he left the team as leader of the LEB Oro with a 9–1 record for agreeing terms with Gipuzkoa Basket. Fisac could not avoid finally their relegation, but he achieved a third promotion to Liga ACB in the next season.

In March 2016, Fisac was hired as manager of the Senegal national team. After coaching the team in the Olympic Qualifying Tournament of Manila, he extended his contract for the AfroBasket 2017, where he led the hosts to the bronze medal.

On 30 May 2018, despite avoiding successfully the relegation from Liga ACB, Fisac resigned to continue at the helm of GBC. He alleged he feels he "completed the cycle".

Two weeks later, Fisac signed a two-year contract with Tecnyconta Zaragoza.

On July 8, 2020, he has signed with Gran Canaria of the Liga ACB.

title: Porfirio Fisac


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Cookbook:Gingerbread

| Dessert

This recipe produces a soft gingerbread cake, not gingerbread cookies. Gingerbread is a type of spice cake. Parkin, a variation traditionally eaten in England around Bonfire Night, is partially oat-based.

Ingredients

 * 110 g (4 oz) butter
 * 110 g (4 oz) brown sugar
 * 220 g (8 oz) golden syrup
 * 220 g (8 oz) all-purpose flour
 * 5 ml (1 level teaspoon) baking powder
 * 5 ml (1 level teaspoon) mixed spice
 * 10 ml (2 level teaspoon) ground ginger
 * 2 eggs
 * 120 ml (4 fluid oz) milk

Procedure

 * 1) Put the butter, sugar, and syrup in a saucepan. Heat gently until the butter melts.
 * 2) Place the dry ingredients in a bowl. Pour the melted butter mixture into the bowl, and beat thoroughly.
 * 3) Warm the milk in a saucepan (so it will dissolve the syrup).
 * 4) Add the milk to the bowl, and beat thoroughly.
 * 5) Beat the eggs, and then stir them in to the mixture.
 * 6) Pour the mixture into an 8-inch (20 cm) greased square cake tin.
 * 7) Bake at 170°C (325°F) for 1 hour.
 * 8) Cool in the tin for 15 minutes, then remove.
 * 9) Leave at least 1 day before cutting into squares. Serve.

Notes, tips, and variations

 * To make parkin, replace half of the flour by weight with 110 g (4 oz) coarse oat flour.

title: Cookbook:Gingerbread


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Basic cardiac anatomy

Basic Cardiac Anatomy Level 1: Blood Flow into and out of the Heart
From an anatomical point of view, the human heart is composed of four compartments or chambers. An easy way to remember the compartments of the heart is to imagine the heart composed of two apartments like a duplex. There are two halves to the heart separated by a septum (wall). Each compartment is composed of an atrium (the entrance) and a ventricle (living room). When visitors (blood) arrives at either of the two apartments, it enters the atrium through the doors (valves), then moves through to the living room (ventricle) once again through doors (valves).

Blood arrives at the heart through the veins and leaves via the arteries. For example, when the blood returns to the heart after traveling around the entire body, it enters through either the superior or the inferior vena cava. When the blood returns to the left atrium after being oxygenated in the lungs, it does so through the pulmonary veins.

The larger of the two chambers is the left side. This results from the greater distance the blood needs to travel once expulsed: after leaving the left ventricle, blood throughout the entire body is pushed. On the other hand, blood expulsed from the right ventricle only enters the pulmonary circuit -- the lung circuit -- to be reoxygenated. As such, the myocardium of the left side of the heart is vastly more developed than that of the right side.

Roughly speaking, blood circulates in two ways around the body: through pulmonary and systemic circulation. The total circulation follows a figure-eight pattern with the heart in the center, between the two loops. The lungs are supplied by the uppermost loop (pulmonary) and the rest of the body is supplied through the lower loop (systemic). The blood leaves the heart through the left atrium, into the aorta (through the aortic valve) and travels to the upper and lower portions of the body. Blood returns to the right atrium via the inferior and superior vena cava. From the right atrium, the blood empties into the right heart ventricle through the opening of the tricuspid valve; the blood leaves the right ventricle through the pulmonary semilunar valve and travels through the pulmonary arteries to the left and right lungs where it is reoxygenated. After oxygenation, the blood returns to the left atrium through the pulmonary veins and it passes through the bicuspid (or mitral) valve to the left ventricle. This process is repeated about 60 times per minute, once for each beat of the heart.

Basic Cardiac Anatomy Level 2: Circulation

 * 1 Left pulmonary vein
 * 2 Right pulmonary vein
 * 3 Left atrium
 * 4 Mitral valve
 * 5 Left ventricle
 * 6 Aortic valve (also: Aortic semilunar valve)
 * 7 Aorta Ascendens
 * 8 Aortic bow
 * 9 Aorta Descendens
 * 10 Vena Cava Inferior (also: ICV)
 * 11 Vena Cava Superior (also: SCV)
 * 12 Right atrium
 * 13 Tricuspid valve
 * 14 Right ventricle
 * 15 Pulmonalis valve (also: Pulmonary semilunar valve)
 * 16 Truncus pulmonalis
 * 17 Right pulmonary artery
 * 18 Left pulmonary artery
 * 19 Interventricular septum
 * 20 Interatrial septum

Note: The major side branches of the aorta (around the aortic bow) have not been shown. Many important vessels (arteries supplying the head, neck, and upper limbs) originate in the aortic bow.

We have learned that the heart consists of two atria (singular atrium) and two ventricula (in English, ventricles or the singular, ventricle.)and that blood circulates around the body in two distinct ways. We will now follow the route blood takes when it travels through the heart, beginning with the blood from the lungs.

 * 1. Blood is oxygenated in the lungs. Waste materials (Carbon dioxide, CO2) are released and Oxygen, O2 is absorbed by the RBCs (Red Blood Cells).
 * 2. The oxygenated blood now travels through the pulmonary veins (venae pulmonales) to the left atrium.
 * 3. During the diastolic phase (Diastole: relaxation of the heart), the blood enters the left ventricle through the mitral valve.
 * 4. During the systolic phase, (Systole: Contraction of the heart), the heart muscle contracts and the blood is pushed into the aorta ascendens (ascending aorta) through the aortic valve.
 * 5. From the aortic bow and the aorta descendens (descending aorta), the blood is spread to smaller arteries that supply every part of the body with fresh oxygenated blood.
 * 6. Blood passes through capillaries (hair vessels) where gas exchange between the tissues and the RBCs takes place. The RBCs release oxygen into the tissues and absorb carbon dioxide which will be released again in the lungs.
 * 7. The blood leaves the capillaries and flows back into veins.
 * 8. The veins combine in the vena cava superior (upper body, above the heart) or vena cava inferior (lower body, under the heart).
 * 9. The vena cava superior and inferior both end in the right atrium.
 * 10. During diastole, the blood enters the right ventricle through the tricuspid valve.
 * 11. During systole, the blood is pushed into the main pulmonary artery (truncus pulmonalis) through the pulmonalis valve.
 * 12. Via the lung arteries, the blood reaches the lung capillaries where gas exchange between air and RBCs takes place.
 * 13. Back to step 1.

Basic Cardiac Anatomy level 3: Blood Supply of the heart

 * MB = Main Branch
 * LRAD = Left Ramus Anterior Descendens
 * Cx = Circumflex artery
 * RCA = Right Coronary Artery
 * RDP = Ramus Descendens Posterior

Note: Only the most basic arteries comprising the coronary arterial system are shown here. There are many small branches to each of these arteries; this is only a basic description of the coronary system.

The heart is always working and therefore, needs a continuous uninterrupted supply of fresh oxygenated blood. A system of vessels surrounding the heart, known as the coronary arteries (or simply the coronaries) supplies the heart with all the blood it needs. The coronary arteries originate from the aorta ascendens just above the aortic valve. There are two coronaries, one of which splits into two separate coronaries just after its origin; in fact, we could also say that we have three coronaries.
 * On the right side, the right coronary artery, runs through the line known as sulcus coronarius (which lies approximately above the border between the right atrium and ventricle) all the way until the back of the heart where it ends in the long interventricular line. Its latter half is known as the Ramus Descendens Posterior. A few centimeters after its origin in the aorta ascendens, the right coronary has a small side branch known as the sinus node artery, this supplies the sinus node with blood, and after that, another small branch supplies the front side of the right ventricle with blood.
 * The left side of the heart, is more muscular since it needs to push the blood with greater force into the aorta ascendens than the right ventricle needs to push blood into the truncus pulmonalis. This is because the left side of the heart needs to supply every part of the body with blood, from the brain to the fingers and toes.

Basic Cardiac Anatomy level 4: Electrical Activity of the Heart
The pumping action of the heart is initiated by electrical stimulation of the right atrium, by a small pocket of tissue called the Sino-Atrial (SA) node. From here, electrical current follows a conduction pathway through to the ventricles. From the SA node, current travels through both atrium, stimulating their contraction, before coming to the Atrio-Ventricular (AV ) node at the junction of the atria and ventricles. Here, conduction is slowed to allow proper contraction of the atrium (and thus adequate filling of the ventricles with blood). From the AV node, curent flows to the bundle of His (located just below the AV node). It then flows down the Left and Right Bundle Branches, on either side of the intraventricular septum, and to the Purkinje fibres in the ventricles, which cause ventricular contraction.

title: Basic cardiac anatomy


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Electronics/Superconductors

In a superconductor, resistance drops to zero and current flows as a short without attenuating.

Until recently most superconductors operated at very low temperatures close to absolute zero. Recently there have been higher temperature superconductors.

Superconductors all for floating magnets.

Superconductors have a great promise for reducing electricity bills.

title: Electronics/Superconductors


text:
Talk:Phyllis George

Businesswoman?
Unfortunately, the article does nothing to indicate with what kind of business she is involved. Could someone clarify that? Badbilltucker 16:28, 11 August 2006 (UTC)

Why Sherman-Denison category?
Did George ever live in either of these two cities? Or is someone perhaps confusing Denison with her hometown of Denton, Texas? Emoll 22:09, 5 January 2007 (UTC)

Agreed and removed, I can find sources for Denton, TX, TCU and University of North Texas; none of which are in North Texas. —Preceding unsigned comment added by Tomsv 98 (talk • contribs) 21:58, 23 October 2007 (UTC)

Material removed
I have removed material from that does not comply with our policy on the biographies of living persons. Biographical material must always be referenced from reliable sources, especially negative material. Negative material that does not comply with that must be immediately removed. Note that the removal does not imply that the information is either true or false.

Please do not reinsert this material unless you can provide reliable citations, and can ensure it is written in a neutral tone. Please review the relevant policies before editing in this regard. Editors should note that failure to follow this policy may result in the removal of editing privileges.--Scott MacDonald (talk) 21:43, 11 October 2008 (UTC)

Can't we say "Miss George" instead of "George"?
"George was Miss America 1971." Such a phrase sounds too modern to me, as if Phyllis George was a transgender person, but in the 20th century, beauty queens were still women. "George" is her family name, of course, but at the same time it is a male first name. So my suggestion would be: can't we change the article's writing style to replace every "George" with "Miss George" for gender clarification? <IP_ADDRESS> (talk) 04:49, 12 September 2017 (UTC)
 * Welcome to Wikipedia! I understand your thinking, however biographies must conform to the style guide (see WP:SURNAME which states that subsequent uses must be the surname/family name without "Miss" etc preceding it. Hope this helps, feel free to ask if you have any questions! --- PageantUpdater (talk) 19:18, 12 September 2017 (UTC)

Birth Name?
Birth name listed as Phyllis George Brown? Isn't Brown her married name? Was she born with her married name already affixed? Longinus876 (talk) 06:27, 27 October 2017 (UTC)

External links modified
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Edit request
Can the day of her death please be changed to May 14? Thank you. MikaelaArsenault (talk) 00:38, 17 May 2020 (UTC)

 * ✅.  Wylie pedia  @ 00:57, 17 May 2020 (UTC)

title: Talk:Phyllis George


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Gesù, Ferrara

The Church of the Gesù of Ferrara is a Roman Catholic church, erected by the Jesuit order, located on piazzetta Torquato Tasso in Via Borgoleoni #56 in Ferrara, Region of Emilia-Romagna, Italy

History
The architect Alberto Schiatti designed the church in 1570 for the Jesuits. The facade is sober. The interior decoration was mostly lost as a result of a fire and the suppression of the order in 1773. The church became property of the Somaschi Order priests until the return of the Jesuits in 1814. The adjacent convent is now a tribunal. Of the works now in the church is a 15th-century terracotta sculptural group: Mourning Over Christ by Guido Mazzoni; this was brought here from the razed church of Santa Maria della Rosa. In the apse stands the Mausoleum of Barbara of Austria, Alfonso II d'Este's second wife, realised at the end of the 1500s by Francesco Casella.

title: Gesù, Ferrara


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Tundrikha

Tundrikha (Тундриха) is a rural locality (a selo) and the administrative center of Tundrikhinsky Selsoviet, Zalesovsky District, Altai Krai, Russia. The population was 441 as of 2013. There are 6 streets.

Geography
Tundrikha is located 15 km west of Zalesovo (the district's administrative centre) by road. Zaplyvino is the nearest rural locality.

title: Tundrikha


text:
Portal:Biblical studies

Department of Biblical Studies

Welcome to the The Wikiversity Department of Biblical Studies, part of the School of Theology. According to Wikipedia, "Biblical studies is the academic study of the Judeo-Christian Bible and related texts"; hence this department focuses on the study of the Bible, and of exegetic and hermeneutic techniques.

Biblical Languages

 * New Testament Greek
 * Prerequisite: Introductory Ancient Greek Language
 * Old Testament Hebrew

Biblical Translation

 * Portal:Bible translation

Biblical Survey

 * Biblical Survey (literal-normal)

Department Projects
At present, the primary focus of the department is content development. There are a number of pages that need to be created and/or fleshed out, and we need editors (like you :-) who are willing to contribute time and energy to the cause.

A department sub-page has been created to list some of the projects that need to be done. If you don't already have a project in mind, you can go to that page, pick a project that sounds interesting, and begin working on it. Then if you intend to stick around, you can place your username in the "Active Participants" section below. If you want to help, but don't know how to edit Wikiversity, see wiki 101 for an introduction to editing.

Active participants
The histories of Wikiversity pages indicate who the active participants are. If you are an active participant in this Department, you may list your name here. This could help the Department grow and the participants better communicate.

Active Participants:
 * OpenSourceJunkie
 * Saz909
 * Deus Vult
 * CQ
 * Elroach 00:39, 7 March 2011 (UTC)
 * DErnestWachter<EMAIL_ADDRESS><EMAIL_ADDRESS> * Mikeduke324

Prayer Requests
A page was created to contain/display prayer requests of those within the department (and without :) Feel free to add your own, or pray for others'.

title: Portal:Biblical studies


text:
Snehlata Deshmukh

Snehlata Shamrao Deshmukh (born c.1938) also spelt as Snehalata was the Vice Chancellor of the University of Mumbai from 1995–2000. She was dean of the Sion hospital. She is an eminent paediatric surgeon in India. She was a pioneer and one of the founders of the neo-natal department of KEM Hospital.

Dr Snehlata Deshmukh is also a co-opted member of Governing Council at the prestigious Tata Memorial Centre, a grant in aid institution under the Administrative control of Department of Atomic Energy, Government of India.

title: Snehlata Deshmukh


text:
High School Mathematics Extensions

 High School Pure Maths  Extensions

Introduction
This online textbook is intended for, but not limited to, high school students that do not have a rigorous understanding and knowledge of university-level mathematics. Therefore, the text's language reflects the expected mathematical maturity of the intended audience.

This book introduces several interesting topics not covered in the standard high school curriculum of most countries.

The materials presented can be challenging, but at the same time, we strive to make this book readable to all who are a few years from applying to higher education.

 From the authors

It is our firm belief that math textbooks should not just be a collection of mathematical facts carefully laid out for rote memorization and cram sessions. A math textbook, especially for the youth, should be full of questions, not just exercises. These questions require some thought to answer and spark curiosity. After all, the questions keep the students engaged, not the answers.

 * "In mathematics the art of proposing a question must be held of higher value than solving it."
 * - Georg Cantor

We sincerely hope to interest, stimulate, and challenge all those who may read this book.

Authors & Contributors
A number of persons not listed below have also made important contributions to this book. Contributors are encouraged to edit and include themselves in this list.

高等学校数学

title: High School Mathematics Extensions


text:
User:Roy Wachira

Roy Wachira
A Serial Entrepreneur from Nairobi,Kenya. He is a Graduate of University of Cape Town - B.Sc Property Studies and also a Graduate of The Red and Yellow School of Logic and Magic in Marketing Advertising and Communication. He has a background in Aviation and was Kenya's Youngest pilot when studying at the Kenya School of Flying while barely 14 yrs.

In South Africa he managed to work at the top Marketing Companies there the likes of Instant Grass, and The Jupiter Drawing Room while working on global brands such as Coca Cola, Distell, Vlisco, Willowbrook and Windhoek. After Studying and Working for over 6 years in Cape Town he relocated back to Nairobi, where he started his Company.

title: User:Roy Wachira


text:
Leuthen

Leuthen may refer to:

 * Lutynia, Środa Śląska County (German: Leuthen), a town in Poland
 * Battle of Leuthen, a 1757 battle during the Seven Years' War
 * Wolf pack Leuthen, a group of German U-boats that operated during the Battle of the Atlantic in World War II

title: Leuthen


text:
Kalpesh Patel

Kalpesh Patel may refer to:
 * Kalpesh Patel (Kenyan cricketer)
 * Kalpesh Patel (Indian cricketer)

title: Kalpesh Patel


text:
Angelópolis (Puebla)

Angelópolis is a residential and commercial area in Puebla City, in the state of Puebla, Mexico.

Today it is one of the most modern areas in Mexico and the most important of Puebla. There are 3 universities there: Instituto Tecnológico y de Estudios Superiores de Monterrey, Universidad Iberoamericana, and Universidad Anáhuac; likewise there are some private schools like: Instituto Andes, Colegio del Bosque, etc. Splits and opulent residential developments contrast with some neighbors and villages in the area, like Concepción La Cruz, Santa Rosa and Ciudad Judicial. In the area is the known "Centro Comercial Angelópolis" (Angelópolis Mall); in addition, the area is noted for being one of the most luxurious in the country as a magnet for both local and foreign investors, for its skyscrapers, luxurious residential developments, cultural spaces, parks, malls, hospitals, service centers, tourist attractions, etc.

History
The Megaproject "Angelópolis" was planned in 1995 by the state government to trigger the development of the region. In this plan were included the extension of 11 sur Avenue, construction of Atlixcáyotl Avenue, the rescue of the Historic Center and the deconstruction of the Convention Center, besides the use and fractionation of the land bank "Atlixcáyotl."

Since the installing of Angelópolis Mall (1994), until its final inauguration (2002), the name of the area took its name, so now the area is popularly called "Angelópolis" or "Zone (of) Angelópolis." Consequent to this, the price per square meter in the area began to increase; this trend is expected to increase further.

Description
Angelópolis area has an approximate area of 15 km2. It is notorious for the high purchasing power of most of its residents and the amount of skyscrapers, where the tallest building in Puebla is the Torre Adamant II, located on the side of the Atlixcáyotl Avenue. There are also several hospitals; private as the Puebla Hospital, the Ángeles Hospital and Torres Médicas, and public, as Cholula General Hospital and Hospital para el Niño Poblano.

The most attractive places are: The landmark of the area and which is called likewise, is a shopping mall located in the north of the area. Angelópolis is an exclusive resort, which boasts some of the best-known luxury brands. Its construction and inauguration was almost at the same time as Santa Fe in Mexico City.
 * Centro Comercial Angelópolis
 * La Estrella de Puebla
 * University Cultural Resort
 * The Art Park
 * Metropolitan Auditorium
 * The Lineal Park
 * Poblana Childhood Park
 * Baroque Museum (In progress)

title: Angelópolis (Puebla)


text:
User:Gemmaklawson/TWA/Earth

The Earth is home to millions of species of plants and animals, including humans.

Earth is the only planet in the solar system known to support life.

title: User:Gemmaklawson/TWA/Earth


text:
Talk:Quintana, Texas

External links modified
Hello fellow Wikipedians,

I have just modified 2 one external links on Quintana, Texas. Please take a moment to review my edit. If you have any questions, or need the bot to ignore the links, or the page altogether, please visit this simple FaQ for additional information. I made the following changes:
 * Added archive http://www.webcitation.org/6YSasqtfX to http://www.census.gov/prod/www/decennial.html

Cheers.— InternetArchiveBot  (Report bug) 15:33, 21 July 2016 (UTC)

title: Talk:Quintana, Texas


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Koroda

Koroda (Корода; Къорода) is a rural locality (a selo) and the administrative centre of Korodinsky Selsoviet, Gunibsky District, Republic of Dagestan, Russia. The population was 939 as of 2010. There are 2 streets.

Geography
Koroda is located 35 km northwest of Gunib (the district's administrative centre) by road, on the Kunada River. Karadakh and Uzdalroso are the nearest rural localities.

title: Koroda


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Joe Garten

Joseph W. Garten (born August 13, 1968) is an American former professional football guard in the Canadian Football League (CFL) and World League of American Football (WLAF). He played college football for the Colorado Buffaloes, where he was a two-time consensus All-American. He played professionally for the Las Vegas Posse and San Antonio Texans of the CFL, and the Barcelona Dragons and Frankfurt Galaxy of the WLAF.

Professional career
Garten was selected by the Green Bay Packers in the sixth round (164th pick overall) of the 1991 NFL draft.

title: Joe Garten