title: Subglacial Maze Origin in Low-Dip Marble Stripe Karst: Examples from Norway
abstract: Maze caves or network caves are enigmatic in their evolution, as they form flow nets rather than more efficient, direct point-to-point flow routes. Network caves are often characterized by uniform passage dimensions in several directions, which indicates simultaneous dissolution of most available fractures. Nonshauggrotta in Gildeska l, northern Norway, is formed in low-dip marble strata and situated as a relict in a topographical and hydrological hanging position, thus lacking a modern drainage
journal: Journal of Cave and Karst Studies