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A tunnel valley is a large, long, U-shaped valley originally cut under the glacial ice near the margin of continental ice sheets such as that now covering Antarctica and formerly covering portions of all continents during past glacial ages. A tunnel valley can be as long as , wide, and deep (its depth may vary along its length). Tunnel valleys were formed by subglacial erosion by water and served as subglacial drainage pathways carrying large volumes of melt water. Their cross-sections exhibit steep-sided flanks similar to fjord walls, and their flat bottoms are typical of subglacial glacial erosion. They presently appear as dry valleys, lakes, seabed depressions, and as areas filled with sediment. If they are filled with sediment, their lower layers are filled primarily with glacial, glaciofluvial or glaciolacustrine sediment, supplemented by upper layers of temperate infill. They can be found in areas formerly covered by glacial ice sheets including Africa, Asia, North America, Europe, Australia and offshore in the North Sea, the Atlantic and in waters near Antarctica. Tunnel valleys appear in the technical literature under several terms, including tunnel channels, subglacial valleys, iceways, snake coils and linear incisions. ==Significance== Understanding tunnel valleys is important because: * They serve as a marker for areas with the potential for effective oil exploration in Africa, * Their bedrock boundaries and glacial infill makes them effective aquifers in many regions. * Soil engineers must accommodate the variations which they exhibit when boring tunnels, establishing foundations, and * They provide one of several signatures marking the edge of former glaciations. Tunnel valleys play a useful role in identifying oil rich areas in Arabia and North Africa. The Upper Ordovician–Lower Silurian materials there contain a roughly thick, carbon-rich layer of black shale. Approximately 30% of the world's oil is found in these shale deposits. Although the origin of these deposits is still under study, it has been established that the shale routinely overlies glacial and glacio-marine sediment deposited ~445 million years before the present by the Hirnantian glaciation. The shale has been linked to glacial meltwater nutrient enrichment of the shallow marine environment. Hence the presence of tunnel valleys is an indicator of the presence of oil in these areas. Tunnel valleys represent a substantial fraction of all melt-water drainage from glaciers. Melt-water drainage influences the flow of glacial ice, which is important in understanding of the duration of glacial–interglacial periods and aids in identifying glacial cyclicity, a problem that is important to palaeoenvironmental investigations. Tunnel valleys are typically eroded into bedrock and filled with glacial debris of varying sizes. This configuration makes them excellent at capturing and storing water. Hence they serve an important role as aquifers across much of Northern Europe, Canada and the United States. Examples include Oak Ridges Moraine Aquifer, Spokane Valley-Rathdrum Prairie Aquifer, Mahomet Aquifer, the (Saginaw Lobe Aquifer ), and the (Corning Aquifer ). 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Tunnel valley」の詳細全文を読む スポンサード リンク
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