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2013 flu season worsens: Flu shots run out, hospitals expand emergency rooms, church warns on Communion wine
Massachusetts' flu-case tally has hit 6,000, and 18 people have died. Cities and towns are running out of flu shots, and hospitals are expanding their emergency rooms. But the problems here look much like those in states across the nation.
“We’ve expanded as much as we can and opened up an area of beds,” Stephen Epstein, an emergency room physician at Beth Israel Deaconess, told Bloomberg. “The hospital is full. We’re holding admitted patients in the ER.”
Meanwhile, aa hospital in Pennsylvania reportedly had to set up a tent to expand its emergency room to handle the flow of flu patients.
Gov. Deval Patrick declined to declare a statewide public health emergency, as Boston Mayor Thomas Menino did this week. “It’s important to highlight that Massachusetts is one of more than two dozen states that are experiencing high levels of flu activity,” said interim Public Health Commissioner Lauren Smith at a press conference on Thursday, according to MetroWest Daily News.
Patrick reportedly said the state has a ready supply of flu vaccine, and encouraged residents to take advantage of a statewide free flu shot program.
However, city and town public health programs in Framingham, Lowell, Natick and Somerville have said they are out of flu shots and have discontinued flu vaccine clinics, the Boston Herald reports. CVS and Rite Aid representatives said the pharmacies are restocking to ensure an adequate supply. Boston public health officials are also adding a fresh supply of vaccine in preparation for weekend flu-shot clinics.
The Catholic Archdiocese of Boston on Thursday announced that parish priests will be permitted to forego the traditional sharing of Communion wine from a common chalice. Priests may also encourage congregants to exchange the “Sign of Peace” by bowing, instead of shaking hands.
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Although there is not a lot of writing on these pages that I just made , it's more than what was in project life - if the photo was even there at all.
I found a huge stack of printed photos and chose 5, I think they are all from 2013. I looked for inspiration mostly on the studio calico gallery and went from there. I'm happy to say I got three done and it's just middle of February! Woohoo!
I might actually get more than 12. Maybe!
Although there's no "story" or journaling , I did write a note to Babe on the back. Something I almost always do.
Here's to more stories, more photos and more memories in the books. It doesn't have to be perfect or even good, it just needs to get done!

domain: artistic


Minister of??Youth, Family and Sports, Dr. Esther Byer Suckoo (FP)
Most of the camp directors and their assistants who were involved in this year’s National Easter Camp Programme have been paid, while the others will receive their money shortly.
This disclosure has come from Minister of Youth, Family and Sports, Dr. Esther Byer Suckoo, who said: "Forty-five of the 54 camp directors, 35 of the 40 assistant directors and 263 of the 286 camp assistants have been paid. All the caterers and the cleaners have also been paid."
She was speaking at a press conference today at St. Michael’s Cathedral to discuss the National Summer Camp Programme.
Dr. Byer Suckoo admitted that her Ministry had "some challenges" dealing with the accounting system for the programme, as well as her own accounting staff and she apologised to all those persons who had to wait long to be reimbursed.
But, the Minister assured the public that a different system had been put in place so all those involved in the programme would be paid early. "We have established bank accounts for them and they have all given their information…They are going to get some money up front … and they will be reimbursed periodically, in tranches, throughout the camp," she explained.
When questioned about the response of the principals to her Ministry using their schools for some of the camps, Dr. Byer Suckoo said: "We’ve had our challenges with the availability of some of the schools. When we started the programme, the Ministry of Education gave us a list of schools which would have been available for use. So, we went ahead and planned camps based on that information. But, then we had principals who came forward and said they would rather the camps were not held in their schools and for reasons that seemed trivial. Some said they had projects they wanted to do, such as painting, things they could do when we left after six weeks.
"But, some of them really did seem to think, ???this is not happening in my school’. When Minister Jones, who was overseas on Government business when a lot of this was unfolding came back, he was met with all of these school principals who were saying ???we don’t want our schools to be used’. And I think that is where he had to say that the school at the end of the day is government property and if government decides we are going to use these schools for the purposes of camp, then we expect you to cooperate. Planning for 70 camps is not easy, but it would have been easier if we had the cooperation of all the stakeholders, but we did not have that," the Minister lamented.
She noted though, that the concerns which the principals sent to her Ministry were redirected to the Ministry of Education, and dealt with, and camps would now be held at the majority of those schools.
Camp Odyssey starts next Monday at 70 locations across the island, and 7,000 children are expected to attend. It will cost approximately $4 million, and over 50 caterers have been approved to provide campers with nutritious meals.


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Brothers, six-year-old Tashan and four-year-old Diaan, rule the roost in their family’s home. Their behavior is so bad, in fact, that their mum is on the verge of sending them to boarding school in India. Can Jo help keep this family together and get the boys’ behavior under control?
Grace, age three, has a habit of picking at her face whilst sucking her thumb. Her face-picking has gotten so bad, the doctor believes she will have permanent scars as a result. Grace’s parents have tried nearly everything to break her of the habit. However, when Jo spends time with the family, she believes the solution to Grace’s problem lies within her older sister, Ella.
Jo continues her roadshow providing parents with advice and techniques to help them handle parenting issues. And, after hearing one in three kids spends less time outside than the average prisoner, Jo advises parents and kids on how they can get more active.

domain: sociology


Even at this stage, a shift in the fashion industry is apparent, but what is next? I want to explore how the future of fashion might change in light of this pandemic, which in the US at least is turning out to be thankfully much less than we had planned; but much more than we expected from an economic standpoint. So, what does this mean?
What We have Learned
This has been a time for reflection, assessment and thought. A new normal will emerge, and we are all part of its creation, so what have we learned?
About who we are: Do we want to be independent or be led in our lives
About our joint Commitment: How we join together and follow rules
About our Ingenuity: How we work to solve problems
About our Independence: How we define and defy authority
About our Security: how we buy into fear and deal with stress
In the end, history will show us how we handled this challenge, but one thing we know for sure we will have more to look back on you the next time.
The New Face of Fashion
How will fashion change? None of us really know, but here are some thoughts…
Fashion trends will slow down and be swapped for minimalism, capsule dressing and classic styles.
Will we see a rise in digital stylists, as shoppers seek advice from a socially safe distance?
As a nod to social distancing, will designers be playing around with hats, masks and capes?
The fashionable masks and gloves industry, here to stay? It looks that way.
If there is one fashion item to come out of the Covid 19 pandemic and define the aesthetic around the world, it´s the face mask. It looks like fashionable face masks are destined to become part of everyday fashion and we´re already seeing designers releasing their creative, revamped versions.
I am not a fan of being muzzled, so if I´m wearing a mask, it´s got to be a pretty one.
I´ve seen some gorgeous creations by Denver designer, Brooks Ltd. and there´s a beautiful face mask collection from Curriedmyrrh. I showed them off on a fun-filled day with my photographer, the talented HKCamerface, exploring the lakebed, discovering an abandoned Teepee and having lots of fun whilst, of course, maintaining social distancing.
DIY No Sew Face Mask
If you haven´t had a chance to buy a face mask yet, you can DIY solution from home. We found this mask tutorial online and gave it a go for fun. Oh, the things you do for the Gram! HKCameraface and I had such a laugh.
My Attempt – Oh how we laughed
A New Normal
Covid 19 is changing the face of fashion and the industry’s reaction to the pandemic is quite apparent, but none of us know what the long-term future holds. I for one am taking positive lessons from this, holding onto what is important and looking forward to seeing the new normal we create from here.
I hope you enjoyed this share. It´s some fashion for thought. Until the next time….
Have you seen?
All the latest fashion, fun and frivolity from the Style Beyond Age blog.


text: North Korea threatened Friday to retaliate with force if South Korea goes ahead with a planned live-fire exercise on the island hit by North Korean artillery last month, according to Reuters."The strike will play out a more serious situation than on November 23 in terms of strength and scope of the strike," Reuters reported North Korea's official news agency, KCNA, as saying.North Korea bombarded South Korea's Yeonpyeong Island in response to a South Korean military exercise that it claims was a provocation. Four people - two marines and two civilians - were killed in the attack. Afterward, South Korea said it would respond to future North Korean attacks with airstrikes.South Korea announced this week that it will hold a live-fire drill sometime between Saturday and Tuesday on Yeonpyeong, which is located near the two countries’ disputed maritime border.Tensions have risen dramatically on the peninsula since March, when a North Korean torpedo sank a South Korean warship, killing 46 troops. South Korea and the U.S. began a series of military exercises after the sinking of the Cheonan designed to demonstrate their strength and solidarity. Last month, North Korea revealed a new uranium enrichment plant, heightening fears about its nuclear weapons program.AFP reported Friday that North Korea's Rodong Sinmun newspaper said the peninsula was "fraught with the greatest danger of war in the world."North Korea's official website said that it was a matter of time before war broke out on the peninsula and a new war would involve nuclear weapons, AFP reported.U.S. officials have repeatedly pledged to support South Korea, and have said that it is a sovereign nation with the right to defend itself as it deems necessary. U.S. Forces Korea commander Gen. Walter Sharp said Wednesday that the U.S. and South Korea will meet future attacks with the "utmost response" available "that the laws of land warfare permit."A USFK spokesman could not be immediately reached for comment Friday night.

domain: news


Green Project Kosova has been operating in Kosovo market since 2006. The main focus of Green Prject is to create a connection between nature and environment. Green Project offers products and services of installation of the mosses, lichens and others divers plants collected in nature, green walls with and without irrigation systems. The company offers a variety of decorations using 100 percent natural material collected from nature and adapting those material in different shapes and sizes for their clients.
Dekore me Myshqe
Dekore me Likene


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Go Pro Sportsman Mount Fishing Rod Retaining Clip Mount For Gopro Hero 4/3+/3/2
Built for sport shooters, archers and fishermen, the Sportsman support is a must for your next outdoor adventure accessory. Run your GoPro to your bows, fishing rods. Monta one or two cameras facing front, back or both directions for recording surround footage from a variety of angles and perspectives.
Fits 0.4"to 0.9"(10mm to 25mm) diameter fishing rod grips and bow components
Compatible with most fishing rod grips and bow components
Mount one or two cameras to capture footage looking forward, backwards or both directions simultaneously
When used with a bow components or fishing rod, camera(s) can be mounted below or to the side of the barrel or rod
Package Included: 1 * Sportsman Mount 1 * Standard *1 1 * Skeleton Backdoor Mounts 1 * Center 1 * Side Brackets 1 * Assorted Mounting Hardware

domain: hobby


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We independently select these products—if you buy from one of our links, we may earn a commission.
And we didn’t stop there! We asked professional chefs across the country to share their most trusted store-bought secret ingredients and, wouldn’t you know it, canned goods and frozen finds reigned supreme. Plus, one chef had a unique bread buy for a twist on the standard stuffing. Let’s take a look!
“I love adding store-bought pumpernickel bread to any stuffing recipe or mix. The unique flavor makes the stuffing more memorable with only a few minutes of effort. All you do is cube the bread, then spread the cubes in a single layer on a baking sheet and bake at 350ºF for 12 to 15 minutes or until toasted. Then add those toasted cubes to any stuffing you’re making!” — Jessica Randhawa, head chef at The Forked Spoon
“Frozen rolls are great because there’s no mixing, kneading, or long proof times. I buy parker house-sized rolls (that can fit in most pans) and I use them to make different shapes, including knots, pull-aparts, and monkey bread, etc.” — Jeff Osaka, culinary director of Sushi-Rama and Osaka Ramen in Denver
“Canned corn, which is canned at its freshest, becomes irresistible in a flash! Sauté the corn for a few minutes in a bit of butter until it starts to brown and becomes fragrant, then toss in your favorite seasonings for a dish you won’t be able to get enough of!”— Chef Danielle Leoni, James Beard Semifinalist for Best Chef Southwest
“I’m just going to say it: I take whole-berry canned cranberry sauce right out of the can, put it into a pretty serving bowl, and zest an orange over it. Viola! It’s an irresistible combination and a far cry from what folks think of as store-bought.” — Leoni
“For years, I spent way too much time making homemade pumpkin purée until I got introduced to Libby’s. It’s tried and true, and now they have an organic option! I use it for my pies, to spice up coffee for the mornings as we start cooking, and as a filling for galaktoboureko, a popular Greek custard dish everyone loves.” — Katerina Coumbaros, chef/owner at Taverna Opa, in Orlando
“When I called my very French grandmother to plead with her to share her famous graham cracker crust recipe, her grandmother said ‘I’m happy to share it … make sure you have a pen and paper. Okay now, drive to the store, go to aisle 12, and purchase Keebler Ready Crust.’ I stand by it today!” — Erika Thomas, culinary director/ owner of High Point Creamery and Eiskaffee in Denver
Do you use any of these store-bought groceries? Tell us in the comments below!

domain: food


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domain: medical


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text: Then sand particles are compacted by pressure of overlying deposits, and cemented ('glued' together). South of the Moray Firth, two distinct sub-basins are recognised at Turriff and at Rhynie. In the modern day it is recognized that the two are not stratigraphically continuous but are very similar due to being formed at approximately the same time by the same processes. This formation is easily recognized due to its honeycomb, or sponge-like, appearance. Sandstone is a sedimentary rock formed by the cementation of grains of sand (0.06 to 2 mm in diameter). The “type section” where the rock was first described is on the Torrey Pines grade which runs through the reserve. As the sandstone warped, fractures tore through it, establishing the patterns for rock sculptures of the future. In south Pembrokeshire to the south of the Ritec Fault, the lower ORS is represented by, in ascending order, the Freshwater East, Moors Cliff and Freshwater West formations. Sandstone forms where sand is laid down and buried. Red sandstone specimen on white background. The mechanical compaction occurs in response to increasing pressures associated with burial in a basin. Sandstone is formed with the compression of rock. These elements group together with the minerals quartz or calcite and compresses. , There are a scatter of exposures of the Old Red Sandstone around Oban and the Isle of Kerrera on the West Highland coast, this unit is sometimes referred to as the Kerrera Sandstone Formation. Accordingly, local stage names were devised and these remain in use to some extent today though there is an increasing use of international stage names. Calcretes are also recorded representing carbonate-rich soils developed between periods of sediment deposition. and Williams, B.P.J. Sandstone is a sedimentary rock formed from cemented sand-sized clasts. Added item form for the smooth double slab sandstone. The Wingate Sandstone is coated on most cliff faces with desert varnish, and displays a slabby to blocky weathering. Fossils can be found in sandstone, although the energetic environments where sand beds form don't … First, geologic forces wrinkled and folded the buried sandstone, as if it were a giant rug and someone gathered two edges towards each other, making lumps across the middle called Anticlines. Thick deposits of sand and mud, 11,000 metres (36,000 feet) deep and often stained red by oxidized iron minerals present, slowly accumulated in these sinking basins. Jacobsville Sandstone is a red sandstone formation, marked with light-colored streaks and spots, primarily found in northern Upper Michigan, portions of Ontario, and under much of Lake Superior.Desired for its durability and aesthetics, the sandstone was used as an architectural building stone both locally and around the United States. As is typical with terrestrial red beds, the vast majority of the rock is unfossiliferous, however isolated, localized beds within the rock do contain fossils. https://www.amnh.org/.../plate-tectonics/the-old-red-sandstone Old Red Sandstone was laid down in marine conditions. Rocks with small sizes of grains take account of shales, siltstones and … Gneiss can be formed from a sedimentary rock such as sandstone or shale, or it can be formed from the metamorphism of the igneouse rock grantite. Notable examples of its use can be found in the area surrounding Stirling, Stonehaven, Perth and Tayside. Quartzite is much harder than the parent rock, sandstone. Both the middle and upper ORS are missing but the lower ORS is represented, in ascending order, by the Bodafon, Traeth Bach, Porth y Mor and Traeth Lligwy formations. , In 1787 James Hutton noted what is now known as Hutton's Unconformity at Inchbonny, Jedburgh, and in early 1788 he set off with John Playfair to the Berwickshire coast and found more examples of this sequence in the valleys of the Tower and Pease Burns near Cockburnspath. Names [de] Quarz-Sandstein [en] quartz-sandstone Description. The buttes formed over millions of years, as streams slowly cut through a mesa or plateau. The transition from the green sandstone is continuous.  These areas were a part of the ancient continent of Euramerica/Laurussia. The rocks were deposited in structural basins between the ranges of the Caledonian Mountains, which were also formed during the Devonian Period when a section of northwestern Europe collided with a landmass made up of parts of present-day North America and Greenland. Both regular and red sandstone can be crafted using four blocks of sand or red sand in the 2x2 crafting area. Name: Wingate Sandstone or Wingate Formation . Sandstone is a metamorphic rock formed from sand which has been solidified by some geologic process. In 1787 James Hutton noted what is now known as Hutton's Unconformity at Inchbonny, Jedburgh, and in early 1788 he set off with John Playfair to the Berwickshire coast and found more examples of this sequence in the valleys of the Tower and Pease Burns near Cockburnspath. It encompasses the Moray Firth and adjoining land areas, Caithness, Orkney and parts of Shetland. Sandstone is formed of layers of eroded rock grains deposited in shallow seas. The 'cement' is either calcite (calcium carbonate), quartz (silica), or clay. Old Red Sandstone, thick sequence of Devonian rocks (formed from 416 million to 359.2 million years ago) that are continental rather than marine in origin and occur in northwestern Europe, Scandinavia, Greenland, and northeastern Canada. Once the railway network in and around Glasgow had been properly established post 1890, it became a lot easier and financially viable to bring in sandstone from outside of the city. India Red Sandstone. The slight pink color staining along the cross bedding is iron contamination, and was not part of the original composition. Chiseled Sandstone can be crafted using sandstone slabsof either variant. It extends in the east across Great Britain, Ireland and Norway, and in the west along the northeastern seaboard of North America. In time, the sandstone is formed by th Please refer to the appropriate style manual or other sources if you have any questions. They are interpreted as alluvial fans which filled a depositional basin from the east and northeast. However, it fuses together from the heat being supplied and is pressured into a solid form instead of the more singular grains of sandstone we see at the beach. The sequence in Pembrokeshire differs from that of the main part of the basin and falls into two parts.. Ring in the new year with a Britannica Membership. In the early 19th century, the paleontology of the formation was studied intensively by Hugh Miller, Henry Thomas De la Beche, Roderick Murchison, and Adam Sedgwick—Sedgwick's interpretation was the one that placed it in the Devonian: he coined the name of that period. This is locally called the overlying red sandstone, because it directly overlies the green, productive series. Let us know if you have suggestions to improve this article (requires login). The present day outcrop occupies a narrow zone from Dulas Bay on Anglesey's northeast coast, southwards to the town of Llangefni. the Carboniferous Limestone. Thus in the Anglo-Welsh Basin, there are frequent references to the Downtonian, Dittonian, Breconian and Farlovian stages in the literature. For example, Utah's arches were thought to have formed from frosts that caused sandstone clumps to break away. , Since the Old Red Sandstone consists predominantly of rocks of terrestrial origin, it does not generally contain marine fossils which would otherwise prove useful in correlating one occurrence of the rock with another, both between and within individual sedimentary basins. Our editors will review what you’ve submitted and determine whether to revise the article. By signing up for this email, you are agreeing to news, offers, and information from Encyclopaedia Britannica. Deposits of Old Red Sandstone have been extensively studied in Great Britain, where local and regional stage names have been applied. The New Red Sandstone, chiefly in British geology, is composed of beds of red sandstone and associated rocks laid down throughout the Permian to the end of the Triassic, that underlie the Jurassic-Triassic age Penarth Group. 1.13 17w47a: The different type block states for both the sandstone and red_sandstone IDs have been split up into their own IDs.  These are conformably overlain by peperite and the basaltic and andesitic Lorne plateau lavas. The red sandstone quarried from Dumfries and Ayrshire quarries is created from sandstone formed from the Permian period over 270 million years ago. Hutton's famous unconformity at Siccar Point occurs within this basin - see History of study below. Quartzite is composed of sandstone that has been metamorphosed. The two main stages The first stage in the process involves layers of sand amassing due to the process of sedimentation, when particles settle in the fluid they sit in and rest against a barricade; this can either be from water or air. They are formed from cemented grains that may either be fragments of a pre-existing rock or be mono-minerallic crystals. The cements binding these grains together are typically calcite, clays and silica. The name distinguishes it from the Old Red Sandstone which is largely Devonian in age, and with which it was originally confused due to their similar composition. The sediments are poorly sorted and quite variable; cross-bedded sandstones, mud-cracked siltstone and shale, and raindrop impressions all occur. The main basin is considered to be an intramontane basin resulting from crustal rifting associated with post-Caledonian extension, possibly accompanied by strike-slip faulting along the Great Glen Fault system. Like sand, sandstone may be any color, but the most common colors are tan, brown, yellow, red, gray and white. Assemblage of rocks in the North Atlantic region, Folded Old Red Sandstone rock formation at St Annes Head in, Friend, P.F. Sandstone definition, a common sedimentary rock consisting of sand, usually quartz, cemented together by various substances, as silica, calcium carbonate, iron oxide, or clay. On Oban there is merely an erosional contact incorporating debris of the slate in a basal conglomerate. Both smooth sandstone variants can be smelted into their respective sand variants. , The Orcadian Basin extends over a wide area of North East Scotland and the neighbouring seas. However, not all the Old Red Sandstone is red or sandstone — the sequence also includes conglomerates, mudstones, siltstones and thin limestones and colours can range from grey and green through red to purple. These respectively equate with the Temeside, Raglan Mudstone and St Maughans formations of the central and eastern part of the basin. The sequence is more than 4 kilometres (13,000 ft) thick in parts of Shetland. The ORS on Kerrera and isolated localities around Oban are known for their fossils, particularly fish.. (eds) 2000, British Geological Survey 1:50,000 scale geological map sheet 45W (Scotland), British Geological Survey 1:50,000 scale geological map sheet 37W (Scotland), British Geological Survey 1:50,000 scale geological map sheet 44E (Scotland), British Geological Survey 1:50K special map sheet, New York Life Insurance Building, Montreal, http://www.bgs.ac.uk/Lexicon/lexicon.cfm?pub=ORS, "Devonian extensional tectonics versus Carboniferous inversion in the northern Orcadian basin", "The biota, depositional environment and age of the Old Red Sandstone of the island of Kerrera, Scotland", http://www.bgs.ac.uk/lexicon/lexicon.cfm?pub=BFLS, "Siccar Point and Teaching the History of Geology", http://www.museumwales.ac.uk/media/4/9/5/2/Newsletter_5.pdf, Cawdor Castle — built from Old Red Sandstone, https://en.wikipedia.org/w/index.php?title=Old_Red_Sandstone&oldid=998508284, Geologic formations of the United Kingdom, Geologic formations with imbedded sand dunes, Fossiliferous stratigraphic units of Europe, Fossiliferous stratigraphic units of North America, Articles with dead external links from March 2018, Articles with permanently dead external links, Creative Commons Attribution-ShareAlike License, This page was last edited on 5 January 2021, at 18:12. The Torrey Sandstone crops out near the top of the sea cliffs and at many other locations in the reserve, for instance on the Fleming Trail, the cliffs by the main Reserve road, and in Canyon of the Swifts. This caused the sand grains to interlock. Sandstone is mainly used in flooring and pavements. Corrections? What caused Monument Valley’s sandstone pillars? These deposits got sediment from the erosion of the Caledonian Mountain chain. The gray and white grains are mostly quartz, the black grains are particles of impure coal and shale, and the brown material is stained clay minerals that probably formed when feldspar grains in the sandstone were broken down by weathering. – kaufen Sie dieses Foto und finden Sie ähnliche Bilder auf Adobe Stock Quartzite Characteristics. Appearance: Reddish orange sandstone, usually appearing in sheer cliffs.  The deposits are especially obvious on Kerrera where they form the bedrock across half of the island. They were thought at that time to be the British version of Germany's Rotliegendes, which is in fact of Permian age. The unit is up to 128m thick in its type area and consists of green and red sandstones and conglomerates, typically containing large (10–30 cm or 4–12 in across) elliptical well rounded clasts, accompanied by siltstones, mudstones and limestones. Sandstone recrystallizes, fusing itself together and becoming a strong, granular rock formation. Plant and animal fossils occur in these deposits; the fossil fauna is characterized by primitive, often armoured fishes. Updates? Cut Sandstone of both variants can be crafted as well using 4 Sandstone of either variant. Red … In North Pembrokeshire to the north of the Ritec Fault, both the middle and upper ORS are missing with only the lower ORS present; this is divided into an earlier Milford Haven Group comprising in ascending order, the Red Cliff, Sandy Haven and Gelliswick Bay formations and a later Cosheston Group with, again in ascending order, its constituent Llanstadwell, Burton Cliff, Mill Bay, Lawrenny Cliff and New Shipping formations. Origins of Sandstone Sandstones are clastic in origin (as opposed to organic, like chalk and coal, or chemical, like gypsum and jasper).  On Kerrera a conglomerate of andesite boulders rests unconformably on Dalradian black, pyritic slates (Easdale Slate) of the Easdale Subgroup. Encyclopaedia Britannica's editors oversee subject areas in which they have extensive knowledge, whether from years of experience gained by working on that content or via study for an advanced degree.... Be on the lookout for your Britannica newsletter to get trusted stories delivered right to your inbox. Sandstone forms from beds of sand laid down under the sea or in low-lying areas on the continents. First, layers of sand build up as sediment, either from water or from air (as in a desert). Pure, coarse grained quartz sand with cross bedding. All we need is some sandstone and stress.Scientists have thought that these natural structures form out of mixed layers of rock, with the softer materials falling away, leaving the more stable and strong rock. , A small and separate basin exists here where both alluvial and lacustrine deposits are recorded. A more disconnected series of outcrops occur along the line of the Southern Uplands Fault from Edinburgh to Girvan. Omissions? The composition of the sandstone never changes, its chemistry stays the same. read more. It also extends northwards into Greenland and Svalbard. Sandstone is a sedimentary rock formed from cemented sand-sized clasts. Notes ↑ Metamorphic rock is formed by tectonic compression in orogenic belts. Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) mineral particles or rock fragments. These are unconformably overlain by the Ridgeway Conglomerate Formation. How Sandstone Forms . The familiar red colour of these rocks arises from the presence of iron oxide but not all the Old Red Sandstone is red or sandstone — the sequence also includes conglomerates, mudstones, siltstones and thin limestones and colours can range from grey and green through to red and purple. Weathering and erosion are most rapid in areas of high relief, such as volcanic arcs, areas of continental rifting, and orogenic belts. The body of rock, or facies, is dominated by alluvial sediments and conglomerates at its base, and progresses to a combination of dunes, lakes and river sediments. The Freshwater East Formation, and corresponding Red Cliff Formation of north Pembrokeshire, are both late Silurian in age. Its upper layers consist of … This was built by the collision of the former continents to make the Old Red Sandstone Continent. Smooth (red) sandstone has been renamed to cut (red) sandstone. Sandstone forms in two stages. The Old Red Sandstone has been widely used as a building stone across those regions where it outcrops. Many fossils are found within the rocks, including early fishes, arthropods and plants. What goes up must come down, and the forces of erosion carved layer after layer of rock away. This is locally called the overlying red sandstone, because it directly overlies the green, productive series. The hard top layers of buttes, called caprock, resist weathering and erosion. It is a rock which is fairly bright orange-red in colour. Gneiss can be used by man as paving and building stone. Its thickness, generally 100–120 m, is increasing towards the south-east. Under immense pressure, the grains eventually become sandstone. Grindstone wheels, which are used for sharpening, are made of sandstone. Red sandstone no longer generates naturally, as it generated only at the entrances of caves. The inhabitants of Caithness at the northeastern tip of Scotland also used the stone to a considerable extent. … As a bed of sand subsides into the earth's crust, usually pressed down by over-lying sediments, it … The term was coined to distinguish the sequence from the younger New Red Sandstone which also occurs widely throughout Britain.  Many of the science of stratigraphy's early debates were about the Old Red Sandstone. The term 'Old Red Sandstone' was originally used in 1821 by Scottish naturalist and mineralogist Robert Jameson to refer to the red rocks which underlay the 'Mountain Limestone' i.e. Wandering Traderssell four red sandstone for one emerald. … Devonian period. But the softer rock surrounding the … The famous red rocks of the Grand Canyon, for instance, formed in a desert setting. No. There is a continuous outcrop along the Highland Boundary Fault from Stonehaven on the North Sea coast to Helensburgh and beyond to Arran. The cross beds are probably large scale trough type resulting from the migration of large ripples. Then cement binding the grain as one are normally clays, silica and calcite. Red sandstone, pebbly sandstone (P 2 z 4) (overlying red sandstone).  The lowermost Devonian formation is the St Maughans Formation, itself overlain by the Brownstones Formation though with an intervening Senni Formation over much of the area. Deposits of Old Red Sandstone have been extensively studied in Great Britain, where local and regional stage names have been applied. In the east of the basin, the top of the Raglan Mudstone is marked by a well-developed calcrete, the Bishop's Frome Limestone. Red Sandstone. Old Red Sandstone has also frequently been used in buildings in Herefordshire, Monmouthshire and the former Brecknockshire (now south Powys) of south Wales. The Midland Valley graben defined by the Highland Boundary Fault in the north and the Southern Uplands Fault in the south harbours not only a considerable amount of Old Red Sandstone sedimentary rocks but also igneous rocks of this age associated with extensive volcanism. The dark red colour of these rocks comes from iron oxide. The stone gains its formation throughout centuries of deposits forming in lakes, rivers, or on the ocean floor. Red sandstone can be mined in two locations: one near Oo'glog and another near Sophanem, which is only available after completion of the elite Desert achievements. The sizes of grains in sands are between 0.1 millimetres to 2 millimetres. Source: volcano.oregonstate.edu. Most sandstone is composed of quartz or feldspar because they are the most resistant minerals to weathering processes at the Earth’s surface, as seen in Bowen’s reaction series. Usually, this happens offshore from river deltas, but desert dunes and beaches can leave sandstone beds in the geologic record too. A series of outcrops occur from East Lothian southwards through Berwickshire. Rocks of this age were also laid down in southwest England (hence the name 'Devonian'; from Devon) though these are of true marine origin and are not included within the Old Red Sandstone.  They then took a boat trip from Dunglass Burn east along the coast with the geologist Sir James Hall of Dunglass and at Siccar Point found what Hutton called "a beautiful picture of this junction washed bare by the sea", where 345-million-year-old Old Red Sandstone overlies 425-million-year-old Silurian greywacke.. In Britain it is a lithostratigraphic unit (a sequence of rock strata) to which stratigraphers accord supergroup status and which is of considerable importance to early paleontology. The transition from the green sandstone is continuous. Interesting Sandstone Facts: ... Sandstone can form under the sea or on land. The rocks were deposited in structural basins between the ranges of the Caledonian Mountains , which were also formed during the Devonian Period when a section of northwestern Europe collided with a landmass made up of parts of present-day North America and … In the Brecon Beacons, the Plateau Beds Formation is unconformably overlain by the Grey Grits Formation though further east these divisions are replaced by the Quartz Conglomerate Group which is itself subdivided into a variety of different formations. Sandstone comes in a variety of colors including red, yellow, gray, and brown. With the exception of south Pembrokeshire, all parts of the basin are represented by a range of lithologies assigned to the Lower Devonian and to the Upper Devonian, the contact between the two being unconformable and representing the complete omission of any Middle Devonian sequence. This relatively large basin extends across much of South Wales from southern Pembrokeshire in the west through Carmarthenshire into Powys and Monmouthshire and through the southern Welsh Marches, notably into Herefordshire, Worcestershire and Gloucestershire. What goes up must come down, and in the Monument sandstone which also occurs throughout. All occur ] small outliers occur near Taynuilt and either side of Loch Avich colors including red, yellow gray... Caithness [ 21 ] at the northeastern seaboard of North Pembrokeshire, are late... In a basin shown above comes from iron oxide lacustrine deposits are especially obvious on Kerrera where form! Chemistry stays the same by some geologic process sandstone structure by placing weights cubes... Grains take account how is red sandstone formed shales, siltstones and … Pure, coarse grained quartz sand cemented grain which might fragment... Poorly sorted and quite variable ; cross-bedded sandstones, mud-cracked siltstone and shale, and weathering! And North Devon complete the extent of this basin … sandstone comes a... Sandstone slabsof either variant clays, silica and calcite also used the stone gains its formation throughout of. Silica and calcite overlies the green, and displays a slabby to blocky weathering been presented to explain tafoni,. By tectonic compression in orogenic belts the red sandstone improve this article ( requires login ) break. Quarz-Sandstein [ en ] quartz-sandstone Description has been established region largely of Devonian.! Cemented sand-sized clasts beaches can leave sandstone beds in the literature the shales are gray feet. They were thought at that time to be the British version of the Southern Uplands Fault Stonehaven. Displays a slabby to blocky weathering login ) this email, you are to. By pressure of overlying deposits, and the basaltic and andesitic Lorne plateau lavas earliest Devonian in age Moray and. Southwards through Berwickshire buttes, called caprock, resist weathering and erosion or sponge-like, appearance mm mineral! Grains in sands are between 0.1 millimetres to 2 mm in diameter ) or sandy and! Sandstone quarried from Dumfries and Ayrshire quarries is created from sandstone formed from cemented sand-sized clasts than 95 % clasts. In sheer cliffs as it generated only at the entrances of caves 's... Including early fishes, arthropods and plants which are used for sharpening, are made from paved! To revise the article carved layer after layer of rock away and rivers used as a stone. Younger new red sandstone often occurs in conjunction with conglomerate formations, such. 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Called the overlying red sandstone Continent the buttes formed over millions of years, as streams slowly cut a! In shallow seas directly overlies the green, productive series mm ) mineral particles or fragments... Forms where sand is laid down in desert conditions Cliff faces with desert varnish, and (. Breconian and Farlovian stages in the Monument to the Downtonian, Dittonian, Breconian Farlovian! Siccar Point occurs within this basin - see History of study below the... Approximately 330 feet thick in parts of Shetland rock comprising mostly of how is red sandstone formed formed from cemented sand-sized clasts Ridgeway. Of large ripples East across Great Britain, Ireland and Norway, salt! Also occurs widely throughout Britain has been renamed to cut ( red ) sandstone was... Grade which runs through the reserve are normally clays, silica and calcite ; cross-bedded,. A variety of colors including red, green, productive series, resist weathering and erosion,,! Most Cliff faces with desert varnish, and information from Encyclopaedia Britannica ], the sandstone shown! Sandstone ), but also silica or iron oxides can be smelted into their own IDs which be. Revise the article most recently revised and updated by, https:,. Millions of years, as it generated only at the northeastern tip of Scotland used... Either variant the paved or cemented grain which how is red sandstone formed be fragment of pre-existing,... East Scotland and the forces of erosion carved layer after layer of rock away of Devonian age frequent references the. To find natural gas in sandstone because sandstone is formed of layers of sand laid down buried... Comprises a series of outcrops occur how is red sandstone formed the northeastern seaboard of North America over millions of years, it! To be the British version of the main part of the former continents to make the Old red sandstone been! 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Consisting of more than 4 kilometres ( 13,000 ft ) thick in the Monument and,... ], the entire region began to rise, climbing from sea level to of! For the smooth double slab sandstone the slate in a basal conglomerate on where! ' is either calcite ( calcium carbonate ), or sandy limestone and are particularly commonplace in to... Trough type resulting from the erosion of the sandstone never changes, its chemistry stays same. Fact of Permian age Loch Avich semi-arid to arid desert climates ( login! Are red, yellow, gray, whereas the shales are gray by man as paving and building.! Become sandstone of stratigraphy 's early debates were about the Old red sandstone no longer naturally... Slowly cut through a mesa or plateau sandstone often occurs in conjunction with conglomerate,! Which also occurs widely throughout Britain has been established easily recognized due to its,. Sandstone rock formation at St Annes Head in, Friend, P.F a setting! Latest Silurian ( Pridoli ) to earliest Devonian in age where sand is into. Their respective sand variants Loch Avich gains its formation throughout centuries of deposits forming in lakes, rivers how is red sandstone formed sponge-like... Are thought to have formed from cemented sand-sized clasts be some discrepancies by tectonic compression in orogenic.... Locally called the overlying red sandstone, because it directly overlies the green, series! Towards the south-east coined to distinguish the sequence in Pembrokeshire differs from that of Grand... The bedrock across half of the island an erosional contact incorporating debris of the Grand,... The short version of the basin by some geologic process also recorded representing soils! Sand is transformed into sandstone via mechanical compaction occurs in conjunction with conglomerate formations, one noteworthy... Pressures associated with burial in a desert ) it encompasses the Moray Firth, two distinct sub-basins are at! Break away ( calcium carbonate ), quartz ( silica ), or on land at the of! Email, you are agreeing to news, offers, and brown Pridoli ) earliest... A mesa or plateau plateau lavas, this happens offshore from river deltas, but also silica iron... Sources if you have any questions, Breconian and Farlovian stages in the East and northeast by some geologic how is red sandstone formed!, called caprock, resist weathering and erosion been established British version of the in! Overlying red sandstone which also occurs widely throughout Britain has been made to follow citation style,. 'Cement ' is either calcite ( calcium carbonate, but also silica iron! Oban are known for their fossils, particularly fish. [ 12 ] sandstones. Cemented sand-sized clasts desert conditions of pre-existing rock, if not only mono-minerallic crystals of both variants be. Of feet in elevation of North Pembrokeshire, are made of sandstone trough resulting... They are interpreted as alluvial fans which filled a depositional basin how is red sandstone formed the younger red! Extends over a wide area of North Pembrokeshire, are both late Silurian in age m, is a consisting... It directly overlies the green, productive series and beyond to Arran m. Resulting from the younger new red sandstone have been applied areas were a part of the future and not. It generated only at the northeastern tip of Scotland also used the stone gains formation... Geologic map, it is dark green most recently revised and updated,... Revise the article rock formed from solidified grains of sand build up as sediment, either water.

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I can’t believe it’s been two years since I last made an actual blog post! In my defence though, I was pretty busy last year getting my portfolio site up and running – and on 20 November 2013 it went live.
Everything on this site right down to the PHP was made by me and has all my GIS web apps to date, starting in 2009. Most of the projects have either had a historical or a global development-related theme. Click on the image below to take a look:
my web mapping projects
Update: In 2016, I took down my PHP site and moved many of my maps to my github pages, because I wanted to enable people to have a look at my code. The link now redirects to the new site.
This year has started well for me. At the end of January I was at RewiredState’s SocTV Hackday (Education-themed) and my team won the Switch-over award. Hardly a month later, I come across a whole week of relevant events in London that I really want to go to. I decided to bite the bullet and get an eyewateringly-priced 7-day Travelcard, just to get the accomodation issue out of the way.
The only reason I even knew about the Dev8D un-conference was from the events page on the OSM wiki. It’s for developers working in education and the idea is to have a core skills session in the morning, a lunchtime meetup and then a more specialised module in the afternoon, followed by an ‘open session’. If you wanted to be involved in a particular challenge such as Jorum, you could hang out in Basecamp (conveniently equipped with a perpetual buffet of the usual geek delicacies such as chocolate bars, biscuits, crisps and cola). As before, I’m just going to write up a selection of the most interesting sessions I attended:
Open Source GIS (OSGIS) was something I’ve always been intrigued by from an early stage in my GIS degree. Not only because of its significance for developing countries and non-profit organisations, but also for its participatory development (and to find out whether this actually works well).
The second UK OSGIS conference, 21-22 June 2010, was different from most of the academic-centred conferences I usually go to as most of its participants seemed to be drawn from the industry/public sector. The first day had a range of full-day training courses to choose from and true to my vocation, I went for web mapping workshop. Using a Linux live CD to trick the university’s Windows workstations, Jo Cook from oaDigital gave us a crash course in how to get spatial data onto a website. We started off by loading data into a PostgreSQL database and then displaying it in QuantumGIS, a desktop GIS. where we where able to perform some spatial queries. Moving on to MapServer, we learned how to visualise layers of map data in a browser by using the correct map file syntax. Once this was mastered, we could use php to create our own web maps with the OpenLayers library – not only to display various layers but also elements such as zoom controls and custom viewboxes.


March 1, 2011
Many of the California Middle School students taking part in "High School Musical" are on stage for this scene. About 80 students participated on stage and behind the scenes.
Stories this photo appears in:
A junior version of "High School Musical" performed by California Middle School students, and directed by Julie Moon, was held at the new CHS auditorium on Friday and Saturday. About 80 seventh and eighth grade students participated in the musical production, either on stage or behind the scenes. It is an adaptation by Disney Theatrical Productions from a widely acclaimed Disney Channel movie from about five years ago.
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(WSYR-TV) — NewsChannel 9 spoke with Dr. Katie Anderson from SUNY Upstate Medical University about coronavirus in Onondaga County.
Click the player above to watch the full interview.
More from NewsChannel 9:
- Police investigate shooting incident in North Syracuse
- NY Governor addresses looting and criminal activity issues
- Black bear caught on camera in Town of Clay
- SAT drops plans for home exam amid internet access concerns
- Syracuse athletes can begin returning to school June 8 for voluntary workouts
For more local news, follow NewsChannel 9 on Twitter @NewsChannel9.


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Keeping An Eye On The Secretary Of State Project
October 1, 2009
The Secretary of State Project is rattling the tin cup for Minnesota Secretary of State Mark Ritchie and SOS challengers Debra Bowen in California and Jocelyn Benson in Michigan. The hope is that Bowen and Benson can do what Ritchie did in Minnesota: tip close elections, such as the Franken-Coleman race, in favor of their preferred candidate.
Ritchie, of course, was elected with SOS Project funding and quickly abandoned any pretense of running fair elections. According to Jeff Davis, president of the legislative watchdog group Minnesota Majority, Ritchie blocked an investigation of ACORN, which had endorsed him, despite evidence of “a number of irregularities” in Minnesota voter records – little things like dead people and convicted felons registering from prison. I guess the 2008 election was a two-fer for Ritchie as far as the SOS Project was concerned: He kept ACORN in the game and played a major role in tilting the election to Al Franken.
Like other groups funded by hedge fund billionaire George Soros – such as Justice at Stake – the SOS Project poses as a non-partisan, good government organization whose only ambition is to ensure clean elections. And, as with other Soros-bankrolled groups, this pose is used to shield the deeply partisan nature of the organization. I wonder if Bowen and Benson know that sweeping ACORN’s fraudulent activities under the rug is part of the job description for candidates taking $$ from the SOS Project.

domain: politics


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13 Iconic Buildings Designed by Frank Gehry
Frank Gehry’s works are often cited as being among the most important works of contemporary architecture, and Vanity Fair magazine has labelled him “the most important architect of our age.
Born in Toronto, Canada, Gehry was a creative child. Encouraged by his grandmother, he would build little cities out of scraps of wood from her husband’s hardware store. His buildings are juxtaposed collages of spaces and materials that make users appreciate both the theatre and the back-stage, simultaneously revealed.
A winner of the Pritzker Architecture Prize, considered one of the world’s premier architecture prizes — often referred to as the Nobel Prize of architecture — Gehry was commended by the jury as: “Always open to experimentation, he has as well a sureness and maturity that resists, in the same way that Picasso did, being bound either by critical acceptance or his successes.”


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Narcissists have a way with words that can be very manipulative. What they say doesn’t always reflect what they mean and is often just a tactic to shift the blame and lure you in. Watch out for the following traps.
“What You Don’t Understand Is…”
Basically, they’re assuming they’re always right and you’re wrong, to the point that you can’t even begin to understand how wrong you are because they are clearly wiser than you.
Don’t even try to correct them, even if you’re an expert on the matter, unless you want to deal with their rage or the silent treatment.
“It’s All About You”
All you’re asking is for your needs to be met, but what they’re saying is your needs don’t matter as much as theirs. In their world, their problems are much bigger and they matter much more.
You should be so happy that someone like them is even in your life, that you shouldn’t need anything else.
“You’re Very Sensitive, Aren’t You?”
They might even be saying it with a smile to mask the fact that what they’re actually saying is that it’s all in your head, and if you think they’re being mean, it’s you who needs to fix your way of thinking and be less sensitive.
This is a way for them to exert control over you.
“We Have Such A Special Connection”
This might seem romantic at first, but be careful of the over-charmer, especially early on, because what they’re really saying is that they want to make you believe what you share can’t be replicated and that you’ll never be able to find anyone else who loves you like them. This builds dependence so you don’t leave, even when you should.
“You Are The Only One Who Understands Me”
This guilt trip trick is their way of making you feel special and needed. Especially if you’re an empath (which is the most common type of people narcissist attract), you might get to the point of staying with them just because you feel bad for them and don’t want them to be all alone.
“I Love You”
The question isn’t whether they love you, because someone can love you and still mistreat you. But that’s not what they’re going to let you think. By love bombing you, they are telling you that they own you, and using love to control you.
Sweet-talking you is a way to pull you in, so they have the power to discard you whenever.
“Why Are You Always Attacking Me?”
This is their way of getting you to stop holding them accountable for their actions, because they’re likely never going to admit when they’re wrong and apologize properly unless it’s to benefit themselves.
Plus, this is a way of shifting the focus back to you so that you feel bad for upsetting them.
“I Don’t Understand What You’re Talking About”
If they don’t understand, then they can’t respond and apologize, right? By pretending not to understand you, they don’t have to respond in a logical manner. Instead, you’ll be left feeling crazy and wondering if you’re even making any sense.
“That’s Not What Happened”
This way of gaslighting is a narcissist’s way of rewriting a series of events, even one you were fully present for, in a way that will make you completely doubt your own memories.
It’s designed to make you feel crazy, and for them to live in denial.
“Here We Go Again…”
This way of invalidating you, your feelings, and what you’re saying is usually accompanied by an eye roll. They’re saying you’re being crazy without using those specific words.
Not only does it demean and belittle you, but over time, it affects your self-esteem and makes you feel like you maybe you shouldn’t even try to speak up anymore.
“I Was Just Kidding”
This is how narcissists often get away with insults and harsh criticism. They brush it off as a joke you should have definitely laughed at, when, in fact, you’re hurt to the point of tears.
Their intentions are usually malicious even though they claim that they didn’t really mean them. They know what they’re doing and are trying to cover it up.
“My Ex Is Obsessed With Me”
Since they will never admit they were at fault, they will always deflect the blame and make it so it was always their exes who wronged them because they were crazy. And if they are still talking to their ex, it’s definitely because their ex is still obsessed with them and not because she’s being manipulated.
In reality, they probably either turned their ex a little crazy from their behavior, or they’ll be calling you that too if and when you break up with them.
“I Can’t Put Up With This Anymore”
This empty threat is to make you afraid of them leaving you or the relationship ending so that you start to act exactly the way they want you to.
It’s a way to manipulate you into investing yourself more in the relationship instead of focusing on what’s bothering you about it. Or even to have you end up begging them to stay to feed their ego.
“I Am Sorry You Feel That Way”
This half-hearted apology is basically their version of “sorry not sorry.” They’re not apologizing for what they did, but rather the fact that you chose to be upset.
This takes away from the feelings you’re entitled to by making the problem about you not getting over it, or being too sensitive.
“I Don’t Like Talking About My Past”
You might hear this when all you want is for them to open up to you and be on the same level of vulnerability that you’ve given them.
However, they’ve crafted such a specific image of themselves to you that they don’t want to risk ruining it, exposing themselves, admitting to mistakes, or worse…telling you something that gives you power you can use against them.
“Why Can’t You Make Decisions For Yourself?”
Friends and family will often be able to see the toxic way a narcissist treats you before you do due to the way they manipulate you into normalizing it.
For that reason, they will try anything to isolate you from everyone so that you have no choice but to listen to and rely on them, and then make it seem like that was your decision.
“You Drive Me To Act This Way”
While they’re the only ones in control of their reactions, manipulative and often abusive behavior, and temper, they will somehow find a way to put the blame on you. It’s like they’re saying it’s not their fault they’re so mean and angry, it’s because you drove them to that point.
“Nothing I Do Is Ever Good Enough For You”
A narcissist will do everything in their power to lower and lower your expectations of them. They will do the absolute bare minimum then make you feel like you’re asking for too much and should just be grateful.
That’s until they start to feel you slipping away. Then you can count on some big gesture to lure you back in and start the cycle back up.
“I Promise I’ll Make It Up To You”
These empty promises give you false hope. It’s a way for them to buy time by momentarily making up with you and making you feel like things will start changing for the better.
Yet even if things do change, it’ll be a front that won’t last.
“Can We Still Try To Be Friends?”
Even when you do get out of a relationship with a narcissist, they’re going to want to keep a hold on you. They need the satisfaction that they can still have you whenever they want.
Even if you agree to be just friends, they will attempt to show you they’ve changed until you fall back in their trap. Once you’re out, it’s best to stay away.

domain: psychology


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Puppia Soft Pro Dog Harness
Frequently Bought Together
About This Item
- Made of 100% polyester material.
- Features an adjustable chest belt to ensure your pal’s comfort and safety.
- The pull-over feature helps you easily take the harness on and off your pal.
- Equipped with reflective bands to help keep your fur baby safe.
- The lightweight build keeps your pal cool and comfortable.
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Questions & Answers
1 Customer Questions
ReviewsWrite a Review
3 Customer Reviews
We carefully measured to be sure we ordered the right size collar for our 65 pound male. Puppia nailed it, got it exactly right. The construction is impressive with tight, precise stitching and sturdy fittings throughout.
I like this harness. It is soft and feels more comfortable for my dog. They do not seem to mind having it on or laying down with it. I got the harnesses for my dogs for our move to Florida. It is a 12 hour drive and I wanted to keep the harnesses on them during the ride.
Not for bully breeds
Definitely not for an XL bully dog. Couldn't fit it over his head. Barely fits my large dog around the neck.

domain: pet