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  2. Glacial motion - Wikipedia

    en.wikipedia.org/wiki/Glacial_motion

    Studying glacial motion and the landforms that result requires tools from many different disciplines: physical geography, climatology, and geology are among the areas sometime grouped together and called earth science. During the Pleistocene (the last ice age), huge sheets of ice called continental glaciers advanced over much of the earth.

  3. Glacier morphology - Wikipedia

    en.wikipedia.org/wiki/Glacier_morphology

    Franz Josef Glacier in New Zealand Features of a glacial landscape. Glacier morphology, or the form a glacier takes, is influenced by temperature, precipitation, topography, and other factors. [1] The goal of glacial morphology is to gain a better understanding of glaciated landscapes and the way they are shaped. [2]

  4. Chatter mark - Wikipedia

    en.wikipedia.org/wiki/Chatter_mark

    In glacial geology, a chatter mark is a wedge-shaped mark (usually of a series of such marks) left by chipping of a bedrock surface by rock fragments carried in the base of a glacier (glacial plucking). Marks tend to be crescent-shaped and oriented at right angles to the direction of ice movement. [1] [2]

  5. Glacial landform - Wikipedia

    en.wikipedia.org/wiki/Glacial_landform

    If the glacial action erodes through, a spillway (or col) forms; Horn: a sharp peak connecting multiple glacier intersections, made up of multiple arêtes. Valley step: an abrupt change in the longitudinal slope of a glacial valley; Hanging Valleys: Formed by glacial meltwater eroding the land partially, often accompanied by a waterfall. [2]

  6. Glossary of geology - Wikipedia

    en.wikipedia.org/wiki/Glossary_of_geology

    Also called Indianite. A mineral from the lime-rich end of the plagioclase group of minerals. Anorthites are usually silicates of calcium and aluminium occurring in some basic igneous rocks, typically those produced by the contact metamorphism of impure calcareous sediments. anticline An arched fold in which the layers usually dip away from the fold axis. Contrast syncline. aphanic Having the ...

  7. Category:Glaciology - Wikipedia

    en.wikipedia.org/wiki/Category:Glaciology

    Palimpsest (geology) Palsa; Paraglacial; Pastonian Stage; Penitente (snow formation) Periglaciation; Glacial period; Phases of ice; Pingo; Plucking (glaciation) Polynya; Post-glacial rebound; Postglacial vegetation; Pre-Pastonian Stage; Pressure melting point; Pressure ridge (ice) Project Iceworm; Protalus rampart; Push moraine

  8. Glaciology - Wikipedia

    en.wikipedia.org/wiki/Glaciology

    Glaciology is an interdisciplinary Earth science that integrates geophysics, geology, physical geography, geomorphology, climatology, meteorology, hydrology, biology, and ecology. The impact of glaciers on people includes the fields of human geography and anthropology .

  9. Glacial striation - Wikipedia

    en.wikipedia.org/wiki/Glacial_striation

    Glacial striations are usually multiple, straight, and parallel, representing the movement of the glacier using rock fragments and sand grains, embedded in the base of the glacier, as cutting tools. Large amounts of coarse gravel and boulders carried along underneath the glacier provide the abrasive power to cut trough-like glacial grooves.