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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 ...
Modrac Lake (Bosnian: Jezero Modrac) is an artificial lake in Bosnia and Herzegovina.Located in the municipality of Lukavac, it is home to many species of fish and is popular with fishermen.
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.
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
Thổ Chu Island (Vietnamese: đảo Thổ Chu or đảo Thổ Châu) is the largest island of Thổ Chu Islands in the Gulf of Thailand. Here lies the administrative center of Thổ Châu Commune, Phú Quốc District, Kiên Giang Province, Vietnam. In the West, [1] the island is also known as Poulo Panjang or Pulo Panjang. [2] [3] [4]
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]
Glacial archaeology, or ice patch archaeology, is a new field in which artifacts emerge through melting ice as a result of climate change. These artifacts are usually well-preserved (due to their encasement in ice), but decay quickly once exposed to the elements. One of the first such discoveries was made by hikers in 1991, with Ötzi. Such ...
Thwaites Glacier is an unusually broad and vast Antarctic glacier located east of Mount Murphy, on the Walgreen Coast of Marie Byrd Land.It was initially sighted by polar researchers in 1940, mapped in 1959–1966 and officially named in 1967, after the late American glaciologist Fredrik T. Thwaites.