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. |
From inside the book
Results 1-3 of 66
Page 5
... slopes of the nala are occupied by slope wash / slope debris . The nala bed portions of the bridge alignments are occupied by nala borne materials . The thickness of the slope debris and nala borne materials above the rock mass was ...
... slopes of the nala are occupied by slope wash / slope debris . The nala bed portions of the bridge alignments are occupied by nala borne materials . The thickness of the slope debris and nala borne materials above the rock mass was ...
Page 31
... slope stability problem appears mainly due to weathered rock mass on the steep slope and presence of minor nala depressions developed along sheared / fractured and uncontrolled blasting in near vicinity . A gentler slope with berms ...
... slope stability problem appears mainly due to weathered rock mass on the steep slope and presence of minor nala depressions developed along sheared / fractured and uncontrolled blasting in near vicinity . A gentler slope with berms ...
Page 81
... slope . These conditions are ( i ) Fully drained slope ( Condition I ) ; ( ii ) Surface water 4X slope height behind the toe of the slope ( Condition - II ) and ( iii ) Saturated slope subjected to heavy surface recharge ( Condition III ) ...
... slope . These conditions are ( i ) Fully drained slope ( Condition I ) ; ( ii ) Surface water 4X slope height behind the toe of the slope ( Condition - II ) and ( iii ) Saturated slope subjected to heavy surface recharge ( Condition III ) ...
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 | |
3 other sections not shown