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Encyclopedia > Withrow Moraine and Jameson Lake Drumlin Field
 The Withrow Moraine erratic on glacial till at the terminus of the Okanogan lobe.
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The Withrow Moraine erratic on glacial till at the terminus of the Okanogan lobe.

The Withrow Moraine and Jameson Lake Drumlin Field is a National Park Service designated privately-owned National Natural Landmark located in Douglas County, Washington state, United States. Withrow Moraine is the only Ice Age terminal moraine on the Waterville Plateau section of the Columbia Plateau. The drumlin field includes excellent examples of glacially-formed elongated hills. (Coordinates: Withrow Moraine intersects Jameson Lake - 47°41′15″N, 119°37′29″W ). Image File history File links Download high-resolution version (1473x646, 280 KB) Erratics on the terminal morraine with multiple w:kames at the terminus of the Okanagon Lobe on the Waterville Plateau. ... Image File history File links Download high-resolution version (1473x646, 280 KB) Erratics on the terminal morraine with multiple w:kames at the terminus of the Okanagon Lobe on the Waterville Plateau. ... The National Park Service (NPS) is the United States federal agency that manages all National Parks, many National Monuments, and other conservation and historical properties with various title designations. ... Caverns of Sonora National Natural Landmark The National Natural Landmark (NNL) program recognizes and encourages the conservation of outstanding examples of the United States natural history. ... Official language(s) None Capital Olympia Largest city Seattle Area  Ranked 18th  - Total 71,342 sq mi (184,824 km²)  - Width 240 miles (385 km)  - Length 360 miles (580 km)  - % water 6. ... Variations in CO2, temperature and dust from the Vostok ice core over the last 400 000 years For the animated movie, see Ice Age (movie). ... Drumlin in Cato, New York A drumlin (Gaelic druim the crest of a hill) is an elongated whale-shaped hill formed by glacial action. ... A glacier is a large, long-lasting river of ice that is formed on land and moves in response to gravity and undergoes internal deformation. ... A hill in Hungary with a hillside vintage garden For the landform that extends less than 600 metres above the surrounding terrain and that is smaller than a mountain, see the mountain article. ...

Contents

Geologic History

Drumlin left by Okanogan Lobe on the Waterville Plateau.
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Drumlin left by Okanogan Lobe on the Waterville Plateau.

Image File history File links Download high-resolution version (1266x1390, 538 KB) Photo of glacially created drumlin on the Waterville Plateau in Washington. ... Image File history File links Download high-resolution version (1266x1390, 538 KB) Photo of glacially created drumlin on the Waterville Plateau in Washington. ...

The plateau

The Withrow Moraine and Jameson Lake Drumlin Field National Natural Landmark is located on the Waterville Plateau, which lies in the northwest corner of the Columbia River Plateau. The plateau is formed on top of the Columbia River Basalt Group a large igneous province that lies across parts of the states of Washington, Oregon, and Idaho in the United States of America. During late Miocene and early Pliocene times, one of the largest flood basalts ever to appear on the earth's surface engulfed about 163,700 km² (63,000 mile²) of the Pacific Northwest, forming a large igneous province with an estimated volume of 174,300 km³. Eruptions were most vigorous from 17—14 million years ago, when over 99% of the basalt was released. Less extensive eruptions continued from 14—6 million years ago. These lava flows have been extensively exposed by the erosion resulting from the Missoula Floods, which laid bare many layers of the basalt flows on the edges of the plateau at Grand Coulee and Moses Coulee.[1][2] [3][4][5] The Washington towns of Spokane, Vantage, Yakima and Pasco, and the Oregon town of Pendleton, lie on the Columbia River Plateau. ... The Columbia River Basalt Group encompasses portions of 3 states. ... A large igneous province (LIP) is an extensive region of basalts resulting from flood basalt volcanism. ... Official language(s) None Capital Olympia Largest city Seattle Area  Ranked 18th  - Total 71,342 sq mi (184,824 km²)  - Width 240 miles (385 km)  - Length 360 miles (580 km)  - % water 6. ... Official language(s) None Capital Salem Largest city Portland Area  Ranked 9th  - Total 98,466 sq mi (255,026 km²)  - Width 260 miles (420 km)  - Length 360 miles (580 km)  - % water 2. ... This article or section does not cite its references or sources. ... The Miocene epoch is a period of time that extends from about 23 to 5. ... The Pliocene epoch (spelled Pleiocene in some older texts) is the period in the geologic timescale that extends from 5. ... A flood basalt is a giant volcanic eruption that coats large stretches of land with basalt lava. ... Earth (IPA: , often referred to as the Earth, Terra, the World or Planet Earth) is the third planet in the solar system in terms of distance from the Sun, and the fifth largest. ... A large igneous province (LIP) is an extensive region of basalts resulting from flood basalt volcanism. ... Glacial Lake Columbia (west) and Glacial Lake Missoula (east) are shown south of Cordilleran Ice Sheet. ... The Grand Coulee The Grand Coulee is an ancient river bed in the U.S. state of Washington. ... Three Devils grade in Moses Coulee, Washington. ...


The glacial history

Illustration of the glacial impacts.
Illustration of the glacial impacts.

Two million years ago the Pleistocene epoch began and Ice age glaciers invaded the area. They scoured the Columbia River Plateau, reaching as far south as the middle of the Waterville Plateau highlands above the Grand Coulee and south to the head of Moses Coulee. In some areas north of the Grand Coulee they were as much as 3 km (10000 feet) thick. Grooves in the exposed granite bedrock are still visible in the area from the movement of glaciers and numerous glacial erratics in the elevated to the Northwest of the coulee.[1][2][6] Image File history File links Download high-resolution version (515x697, 127 KB) Figure adapted from works of the United States Government, which are in the w:public domain combined with data from references. ... Image File history File links Download high-resolution version (515x697, 127 KB) Figure adapted from works of the United States Government, which are in the w:public domain combined with data from references. ... The Pleistocene epoch (IPA: ) is part of the geologic timescale. ... Variations in CO2, temperature and dust from the Vostok ice core over the last 400 000 years For the animated movie, see Ice Age (movie). ... Austrias longest glacier, the Pasterze, winds its 8 km (5 mile) route at the foot of Austrias highest mountain, the Grossglockner A glacier is a large, long-lasting river of ice that is formed on land and moves in response to gravity. ... Three Devils grade in Moses Coulee, Washington. ... The Grand Coulee The Grand Coulee is an ancient river bed in the U.S. state of Washington. ... A Glacial erratic is a piece of rock carried by glacial ice some distance from the rock outcrop from which it came. ...


Progress of the Okanogan Lobe of the Cordilleran Glacier

Terminal moraine with multiple kames at the terminus of the Okanogan Lobe on the Waterville Plateau.
Enlarge
Terminal moraine with multiple kames at the terminus of the Okanogan Lobe on the Waterville Plateau.

The Okanogan lobe of the Cordilleran Glacier moved down the Okanogan River valley, covering 500 mi² of the Waterville Plateau and blocked the ancient route of the Columbia River, backing up water to create Glacial Lake Columbia and Lake Spokane. Initially water discharged from Lake Columbia by running up through the head of Grand Coulee and down through Foster Coulee to rejoin the Columbia River. As the glacier moved further south, Foster Coulee was cut off and the Columbia River then discharged through Moses Coulee, which runs southward slightly to the east of the ancient and current course of the Columbia. As the Okanogan lobe grew, it blocked Moses Coulee as well; the Columbia found the next lowest route through the region which was eroded to become the modern Grand Coulee.[6] Image File history File links Download high-resolution version (1509x1132, 368 KB) Erratics on the terminal morraine of the Okanagon Lobe of the Cordilleran Glacier on the Waterville Plateau of Washington, USA. Photo taken by uploader in November 2006. ... Image File history File links Download high-resolution version (1509x1132, 368 KB) Erratics on the terminal morraine of the Okanagon Lobe of the Cordilleran Glacier on the Waterville Plateau of Washington, USA. Photo taken by uploader in November 2006. ... A kame among the glacial drift on the terminal morraine of the Okanagon Lobe of the Cordilerion Glacier on the Waterville Plateau of the Columbia Plateau in Washington, United States. ... The Cordilleran ice sheet was a major ice sheet that covered, during glacial periods of the Quaternary, a large area of North America. ... The Okanogan River (called the Okanagan River in its upper reaches in Canada) is a tributary of the Columbia River, approximately 115 mi (185 km) long, in southern British Columbia in Canada and north central Washington in the United States. ... Three Devils grade in Moses Coulee, Washington. ... The Grand Coulee The Grand Coulee is an ancient river bed in the U.S. state of Washington. ...


After the glacier

As the Okanogan lobe melted, the northern half of the Waterville Plateau, including the upper portions of Moses Coulee, were littered with clear evidence of its passing. The glacier left behind a blanket of glacial till, up to 50 feet thick in places. This glacial till, comprised of clay, silt, sand, gravel, cobblestones, and erratic boulders, covers most of the upper Moses Coulee. The melting glacier discharged both down Moses Coulee and into the Grand Coulee as is evident in the Sims Corner eskers and kames. [7] An erratic is a fragment of glacial till carried by ice, sometimes for hundreds of miles, and deposited on rocks of a different geologic composition. ... A Glacial erratic called Yeager Rock, Waterville Plateau, Washington, USA The Sims Corner Eskers and Kames National Natural Landmark includes excellent examples of Pleistocene ice stagnation landforms including numerous Glacial erratics terminal moraines, eskers and kames. ...


See also

This is a list of National Natural Landmarks in the United States by state or territory: // Beaver Creek Swamp Cathedral Caverns Dismals Canyon Mobile Tensaw River Bottom Lands Red Mountain Expressway Cut Shelta Cave Aniakchak Crater Arrigetch Peaks Bogoslof Island Clarence Rhode National Wildlife Range Illiamna Volcano Lake George Malaspina...

External links

  • U.S. National Park Service material on Withrow Moraine and Jameson Lake Drumlin Field

References

  1. ^ a b Alt, David. Glacial Lake Missoula & its Humongous Floods. Mountain Press Publishing Company. ISBN 0-87842-415-6.
  2. ^ a b Bjornstad, Bruce (2006). On the Trail of the Ice Age Floods: A Geological Guide to the Mid-Columbia Basin. Keokee Books; Sand Point, Idaho. ISBN 978-1-879628-27-4.
  3. ^ Portions of this article, including a figure, are adapted from works of the United States Government, which are in the public domain
  4. ^ Alt, David & Hyndman, Donald (1995). Northwest Exposures: a Geologic Story of the Northwest. Mountain Press Publishing Company. ISBN 0-87842-323-0.
  5. ^ Carson, Robert J. and Pogue, Kevin R. (1996). Flood Basalts and Glacier Floods:Roadside Geology of Parts of Walla Walla, Franklin, and Columbia Counties, Washington. Washington State Department of Natural Resources (Washington Division of Geology and Earth Resources Information Circular 90). ISBN none.
  6. ^ a b Mueller, Marge & Ted (1997). Fire, Faults and Floods. University of Idaho Press, Moscow, Idaho. ISBN 0-89301-206-8.
  7. ^ Washington history link.

A work of the United States Government is, as defined by United States copyright law, a work prepared by an officer or employee of the United States Government as part of that persons official duties. ... The public domain comprises the body of all creative works and other knowledge—writing, artwork, music, science, inventions, and others—in which no person or organization has any proprietary interest. ...

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