Records of the Geological Survey of India, Volume 141, Part 8The Survey, 2006 - Earthquakes Vols. 1- include Report of the Geological Survey, 1867- ; v. 32- include Review of the mineral production of India, 1898/1903- ; v. 75 consists of Professional papers, no. 1-16; v. 76 consists of Bulletins of economic minerals. |
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Page 28
... clay layer at the top . The clay layer has been eroded in the vicinity of the river channel . The intermediate level terrance T - 1 has been inferred to be an erosional remnant of the highest level terrace ( T - 2 ) and is preserved ...
... clay layer at the top . The clay layer has been eroded in the vicinity of the river channel . The intermediate level terrance T - 1 has been inferred to be an erosional remnant of the highest level terrace ( T - 2 ) and is preserved ...
Page 60
... clay whereas Channel Alluvium is represented by gray , iron stained , fine to coarse grained sands with clay pebbles restricted to active channels of streams . Earlier work in the area ( Geo - environmental appraisal studies and ...
... clay whereas Channel Alluvium is represented by gray , iron stained , fine to coarse grained sands with clay pebbles restricted to active channels of streams . Earlier work in the area ( Geo - environmental appraisal studies and ...
Page 147
... clay - soft sandstone sequence with thin pebbly beds of Siwalik group show sub - vertical disposition with profuse shearing , shattering , high angle conjugate shear joints with slikckensides . The cut off patches of sandstone and ...
... clay - soft sandstone sequence with thin pebbly beds of Siwalik group show sub - vertical disposition with profuse shearing , shattering , high angle conjugate shear joints with slikckensides . The cut off patches of sandstone and ...
Contents
प्रचालन जम्मू एवं कश्मीर द्वारा किए गए कार्यों का विहंगावलोकन | 1 |
Group of rocks in Pithoragarh Nainital Almora and Dehradun districts Uttarakhand | 135 |
Specialised thematic mapping of discontinuities across the lithostratigraphic sections | 141 |
Copyright | |
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