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A paternoster lake is one of a series of glacial lakes connected by a single stream or a braided stream system. The name comes from the word Paternoster, another name for the Lord's Prayer derived from the Latin words for the prayer's opening words, "Our Father"; Paternoster lakes are so called because of their resemblance to rosary beads, with ...
Kettle lake: Depression, formed by a block of ice separated from the main glacier, in which the lake forms; Tarn: A lake formed in a cirque by overdeepening; Paternoster lake: A series of lakes in a glacial valley, formed when a stream is dammed by successive recessional moraines left by an advancing or retreating glacier
The longest glacier in the Yosemite area ran down the Grand Canyon of the Tuolumne River for 60 miles (95 km), passing well beyond Hetch Hetchy Valley. Merced Glacier flowed out of Yosemite Valley and into the Merced River Gorge. Lee Vining Glacier carved Lee Vining Canyon and emptied into Lake Russell (the much enlarged ice age version of Mono ...
Within glacial valleys, depressions created by plucking and abrasion can be filled by lakes, called paternoster lakes. If a glacial valley runs into a large body of water, it forms a fjord. Typically glaciers deepen their valleys more than their smaller tributaries.
Six Lakes. The Six Lakes are a chain of six alpine and glacial Paternoster lakes in Custer County, Idaho, United States, located in the White Cloud Mountains in the Sawtooth National Recreation Area. The lakes are located on the upper portion of the Fourth of July Creek watershed, a tributary of the Salmon River and the outflow of Fourth of ...
Glacial lakes of the United States (3 C, 96 P) Great Lakes (30 C, 66 P) K. ... Paternoster lake; Supraglacial lake; Tarn (lake) + Glacial lake outburst flood; A.
The Four Lakes are a chain of four small glacial Paternoster lakes in Custer County, Idaho, United States, located in the White Cloud Mountains in the Sawtooth National Recreation Area. The lakes are located in the upper portion of the Little Boulder Creek watershed upstream of Quiet Lake and east of Patterson Peak.
Lake Agassiz (/ ˈæɡəsi / AG-ə-see) was a large proglacial lake that existed in central North America during the late Pleistocene, fed by meltwater from the retreating Laurentide Ice Sheet at the end of the last glacial period. At its peak, the lake's area was larger than all of the modern Great Lakes combined. [2]