Geo-morphology Flashcards
Where were continental glaciers in North America?
Canada was nearly completely covered by ice, as well as the northern part of the United States, both blanketed by the huge Laurentide Ice Sheet. Local glaciations existed in the Rocky Mountains and the Cordilleran Ice Sheet and as ice fields and ice caps in the Sierra Nevada in northern California.
Describe how continental glaciers move.
The pressure that turns snow into ice is responsible for the movement of a glacier due to the “push down” action. They move downslope in a number of directions and are not restricted to a channel or valley. They must expand because of the constant accumulation of ice and snow. Continental glaciers do not move as quickly as alpine glaciers because there is less slope and more mass involved. They move mostly by plastic flow. Plastic flow is 50 meters of ice that causes brittle ice to become like plastic.
What is a Drumlin?
Drumlin, oval or elongated hill believed to have been formed by the streamlined movement of glacial ice sheets across rock debris, or till.
How do drumlins indicate glacial direction?
The tapered end of each drumlin hill points in the direction of glacier flow.
What mountain formation is created at the top end of the glacier?
Glacial Horns
What deposit is left behind by an interglacial stream?
Glacial Till- unsorted clays, sands, silts, gravel and boulders
What happens when 2 glacial valleys intersect at a different height.
A Hanging Valley -
A hanging valley is elevated above another valley, with one end open to the valley below. There may be a cliff or steep formation where they meet. A river or stream may run through a hanging valley, forming a waterfall that enters the lower valley.
A cluster of 3 Cirques creates?
Arêtes- horn or pyramid peak. The 3 cirques erode back into a mountain.
Which moraine runs down the center of an alpine Glacier?
Medial Moraine
What is the source of moraine material?
Glacial till- unsorted debris- rocks, gravel, sand, boulder…
Which moraine is deposited at the sides of Glaciers?
Lateral Moraines
What happens to glacial debris many years after a Continental Glacier melts?
Moraines are left behind- small hills of debris(marks end of the glacier or the lateral path it took down the valley). Large amounts of sand and gravel, which were eroded from the mountainsides, are also left behind. ??? I think?
What do average global temperature ice ages require?
In fact, the difference between today’s average global temperature and the average global temperature during the last Ice Age is only about 5 degrees. Maybe 10 degrees Celsius during the ice age, 14.2 now?
What is basal slip?
Water acts as a hydraulic jack and lubricant allowing slipping along the ground (causes movement of glaciers)
What is Rock Flour?
Rock flour, or glacial flour, consists of fine-grained, silt-sized particles of rock, generated by mechanical grinding of bedrock by glacial erosion or by artificial grinding to a similar size.
What shape is a glacial valley?
U-shaped
What creates glacial till?
Till is derived from the erosion and entrainment of material by the moving ice of a glacier. It is deposited some distance down-ice to form terminal, lateral, medial and ground moraines. Short form: it is created by the moving of a glacier and the pushing forward of unsorted material and silt.
How does snow become ice?
Snow accumulates, then snow changes due to exposed elements, recrystallizing into sand-like snow (Firn/neve) then the pressure (50 m thick) from the weight will fuse the firn together into a solid mass forming ice.
What makes a glacier stationary?
The terminus of a glacier is stationary when accumulation (snow) at the top of the glacier is equal to ablation (melt) at the bottom of the glacier- Ice/Snow Balance Budgets.
What is a large, misplaced rock called that is left behind after a glacier has receded?
An Erratic
Which moraine is left behind at the furthest point of a glaciers progress?
Terminal Moraine
A truncated spur involves a glacial valley cutting perpendicular to a river valley. True or False?
True
Describe a Roche Mountonnee.
A roche moutonnée is a rock hill shaped by the passage of ice to give a smooth up-ice side and a rough, plucked and cliff-girt surface on the down-ice side. The upstream surface is often marked with striations.
Describes a Permafrost landscape.
Permafrost is soil, rock or sediment that is frozen for more than 2 years in a row. Permafrost forms in climates where the annual air temp is 0 °C or colder. Usually in the arctic, sub-arctic and Antarctic areas.
What causes a Pingo?
Pingos are created in a permafrost area when the pressure of freezing groundwater pushes up a layer of frozen ground. Pressure (pressure that forces groundwater to the surface without pumping) builds up under the permafrost layer, and, as the water rises, pushing up the overlying material, it freezes in a lens shape.