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...figure number|3}}In this photograph the site of two sills can be seen in a bedrock (Vaca Muerta Fm). Right on the sector focuses it can be clearly seen intens ...sumably has to do with three factors: pore pressure, level weakness is the bedrock (being shale is less competent ) and plans anisotropy generated in the shal

...location of cracks in ice, permafrost studies, the detailed mapping of the bedrock surface, the examination of soil stratification, and the mapping of contami ...a [[lateral]] and/or vertical freshwater-saltwater boundary, the depth to bedrock, and the identification and mapping of conductive groundwater contaminants.

| Valley fills on bedrock unconformities || 12-1400 m (39-4593 ft); most < 500 m (1640 ft) || 75 m-52

...ew and Recommendations for Nomenclature Use. Upper Paleozoic to Quaternary Bedrock, Norsk Polarinstitutt, Tromsø, p. 127–214.</ref>). This formation is aga

...It will be more effective cause every river bank certainly eroded and the bedrock can be exposed.

| Valley fills on bedrock unconformities || 12-1400 m (39-4593 ft); most < 500 m (1640 ft) || 75 m-52

| Valley fills on bedrock unconformities || 12-1400 m (39-4593 ft); most < 500 m (1640 ft) || 75 m-52

...important class of carbonate reservoirs. Caves present within a limestone bedrock are liable to collapse on compaction, creating a collapse [[breccia]] and w

...t Jabal ‘Unayzah, in the southwestern corner of the country, at 940 msl. [[Bedrock]] is exposed in these areas, largely [[Cenozoic]] but Mesozoic and [[Paleoz

|+ {{table number|1}}Average abundances of selected elements in bedrock, all values in ppm.<ref name=Khndare>Khandare, H. W., 2012, Medical geology