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  2. Glacial motion - Wikipedia

    en.wikipedia.org/wiki/Glacial_motion

    Glacial lakes have been rapidly forming on the surface of the debris-covered glaciers in this region during the last few decades. USGS researchers have found a strong correlation between increasing temperatures and glacial retreat in this region. Glacial motion is the motion of glaciers, which can be likened to rivers of ice. It has played an ...

  3. Timeline of glaciation - Wikipedia

    en.wikipedia.org/wiki/Timeline_of_glaciation

    Within ice ages, there exist periods of more severe glacial conditions and more temperate conditions, referred to as glacial periods and interglacial periods, respectively. The Earth is currently in such an interglacial period of the Quaternary glaciation, with the Last Glacial Period of the Quaternary having ended approximately 11,700 years ago.

  4. Glacier - Wikipedia

    en.wikipedia.org/wiki/Glacier

    Most of the important processes controlling glacial motion occur in the ice-bed contact—even though it is only a few meters thick. [40] The bed's temperature, roughness and softness define basal shear stress, which in turn defines whether movement of the glacier will be accommodated by motion in the sediments, or if it will be able to slide.

  5. Category:Glaciology - Wikipedia

    en.wikipedia.org/wiki/Category:Glaciology

    I. Ice; Ice age; Ice calving; Ice core; Ice core dating; List of ice cores; Ice divide; Ice drilling; Ice jam; Ice lens; Ice mass balance buoy; Ice segregation; Ice sheet

  6. Basal sliding - Wikipedia

    en.wikipedia.org/wiki/Basal_sliding

    Basal sliding is the act of a glacier sliding over the bed due to meltwater under the ice acting as a lubricant.This movement very much depends on the temperature of the area, the slope of the glacier, the bed roughness, the amount of meltwater from the glacier, and the glacier's size.

  7. 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]

  8. Moulin (geomorphology) - Wikipedia

    en.wikipedia.org/wiki/Moulin_(geomorphology)

    Water from moulins may help lubricate the base of the glacier, affecting glacial motion. Given an appropriate relationship between an ice sheet and the terrain, the head of water in a moulin can provide the power and medium with which a tunnel valley may be formed.

  9. Glaciology - Wikipedia

    en.wikipedia.org/wiki/Glaciology

    Areas of study within glaciology include glacial history and the reconstruction of past glaciation. A glaciologist is a person who studies glaciers. A glacial geologist studies glacial deposits and glacial erosive features on the landscape. Glaciology and glacial geology are key areas of polar research.