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2021
Several hundred years after the last flood from glacial lake Missoula, there was at least one last flood that occurred during the breakup of the Okanogan Ice Lobe. The Okanogan Lobe retreated northward from the Waterville Plateau at the end of the Ice Age about 14,000 years ago.
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Several hundred years after the last flood from glacial lake Missoula, there was at least one last flood that occurred during the breakup of the Okanogan Ice Lobe. The Okanogan Lobe retreated northward from the Waterville Plateau at the end of the Ice Age about 14,000 years ago.
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Geological Society of America Bulletin, 1923
Lake Wayne and Lake Vanuxem Year by year the story of the Laurentian glacial lakes grows more complicated. The steadily falling waters of our youthful innocence are being replaced by a pulsating rise and fall due to rhythmic oscillations of the ice-front. One of these pulsations was long ago recognized by Fairchild[2][1] in his “free drainage” stage of
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Lake Wayne and Lake Vanuxem Year by year the story of the Laurentian glacial lakes grows more complicated. The steadily falling waters of our youthful innocence are being replaced by a pulsating rise and fall due to rhythmic oscillations of the ice-front. One of these pulsations was long ago recognized by Fairchild[2][1] in his “free drainage” stage of
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Glacial lake sedimentation, Austerdalsisen, Norway
Sedimentology, 1976ABSTRACTSediments deposited in a lake at the front of a glacier in the Svartisen area, Norway, have been studied between 1957 and 1974. Until 1959, they were almost completely covered by an outwash plain (sandur), but subsequent erosion has exposed glacial lake sediments more than 70 m deep within a rock basin about 2·5 km long and 1 km wide. The basin
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Geological Society of America Bulletin, 1895
Introduction. The study of the lacustrine history of the Genesee valley was undertaken in continuation of the work upon the glacial lakes in western New York* and with no expectation of making it the subject of a separate paper. The history is found, however, to be of remarkable and romantic character. The glacial waters alternately flowed to the gulf
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Introduction. The study of the lacustrine history of the Genesee valley was undertaken in continuation of the work upon the glacial lakes in western New York* and with no expectation of making it the subject of a separate paper. The history is found, however, to be of remarkable and romantic character. The glacial waters alternately flowed to the gulf
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Geological Society of America Bulletin, 1932
Introduction Cowanesque River flows eastward across Tioga County, in north central Pennsylvania, to join the Tioga at Lawrenceville. For 15 miles of its course, from Westfield to Nelson, the river meanders across flats three-quarters of a mile wide that broaden to 2 miles between Elkland and Osceola.
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Introduction Cowanesque River flows eastward across Tioga County, in north central Pennsylvania, to join the Tioga at Lawrenceville. For 15 miles of its course, from Westfield to Nelson, the river meanders across flats three-quarters of a mile wide that broaden to 2 miles between Elkland and Osceola.
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2021
Lake Missoula flood map produced by Eastern Washington University and the Ice Age Floods Institute.
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Lake Missoula flood map produced by Eastern Washington University and the Ice Age Floods Institute.
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Geological Society of America Bulletin, 1901
Introduction The reviewing and abstracting of the chapters of the final report of the Geological Survey of Minnesota, so far as they treat of the areal geology of the state, have brought vividly to mind some of the general physical features which have not been grouped nor discussed in their ensemble in any of the chapters of that report. Among these
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Introduction The reviewing and abstracting of the chapters of the final report of the Geological Survey of Minnesota, so far as they treat of the areal geology of the state, have brought vividly to mind some of the general physical features which have not been grouped nor discussed in their ensemble in any of the chapters of that report. Among these
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Depositional record of a glacial-lake outburst: Glacial Lake, Souris, North Dakota
Geological Society of America Bulletin, 1991Glacial Lake Souris, located in what is now North Dakota, was inundated by about 74 km3 of sediment-laden water from the outburst of Glacial Lake Regina (Saskatchewan). Glacial-lake outbursts were common during the late Pleistocene, but detailed studies of outburst-deposited sediments in lake environments have not been done.
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