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Although a glacier may flow into a body of water, it forms only on land and is distinct from the much thinner sea ice and lake ice that form on the surface... |
(Kivalliq). Two of the lobes abut the adjacent Labrador and Baffin ice sheets. The primary lobes flow (1) towards Manitoba and Saskatchewan; (2) toward Hudson Bay;... |
lubricates the ice sheet so that it flows more rapidly. This process produces fast-flowing channels in the ice sheet — these are ice streams. In previous... |
called glacial flour. Lateral moraines are those formed at the side of the ice flow, and terminal moraines were formed at the foot, marking the maximum advance... |
Stanley bottle (section IceFlow) The Stanley IceFlow Tumbler is a newer product based on the success of the Stanley Quencher. With a similar insulated design, the IceFlow series utilizes... |
Glacier morphology (redirect from Ice dome) like ice caps, exhibit radial flow. As ice sheets expand over the ocean, they become ice shelves. Ice sheets contain 99% of all the freshwater ice found... |
Crevasse (redirect from Ice fissure) accelerate ice flow. Direct drains of water from the top of a glacier, known as moulins, can also contribute the lubrication and acceleration of ice flow. Longitudinal... |
Khumbu Icefall (redirect from Khumbu Ice Fall) (1 mi) away horizontally. The speed of ice flow and the precipitous elevation drop create a bergschrund (ice berg shoulder), characterized at the top... |
flow law, also referred to as Glen's flow law, is an empirically derived constitutive relation widely used as a model for the rheology of glacial ice... |
mountains to enable the ice sheet to flow out to the ocean through outlet glaciers. These glaciers regularly shed ice in what is known as ice calving. Sediment... |
Climate of Antarctica (section Ice cover) ice flows, albeit slowly, the ice within the ice sheet is younger than the age of the sheet itself. About 75% of the coastline of Antarctica is ice shelf... |
axis parallel to the orientation of ice flow and with an up-ice (stoss) face that is generally steeper than the down-ice (lee) face. Drumlins are typically... |
the flow of ice in an icefall may be measured in kilometres per year. Such rapid flow cannot be accommodated by plastic deformation of the ice. Instead... |
high-resolution measurement of changes in glacial structure, ice flow, and shifts in ice dynamics, all of which agree closely with ground observations... |
1941 that elongated clasts in tills tend to align with the direction of ice flow. Clasts in till may also show slight imbrication, with the clasts dipping... |
Antarctic ice sheet (EAIS), West Antarctic ice sheet (WAIS), and Antarctic Peninsula (AP), due to the large differences in topography, ice flow, and glacier... |
blue-ice area and remain there, or they fall elsewhere into the ice sheet and are transported to the blue-ice area by ice flow. Additionally, ice up to... |
Glacial erratic (section Ice-rafted erratic) of the ice flow route. They can be transported by ice rafting, which allows quantification of the extent of glacial flooding resulting from ice dam failures... |
large-scale geologic faults. However, the ice flow theories will be re-evaluated in light of new data from recent ice-penetrating radar surveys which revealed... |
An ice-marginal lava flow is a lava flow that comes into direct contact with a glacier or the margins of a large ice sheet. As the lava reaches the margins... |