Ditemukan 912 dokumen yang sesuai dengan query
"Report of landslide and sinking at Tawaghat and its surrounding areas have been reported in past also with noticeable amount of loss of lives and properties. A sizeable landslide occurred in this region in December 1962. During August 1977, a major landslide came roaring down the main nala of Khela village and destroyed sheds and houses killing 44 persons and 76 head of cattles. About 150 acres of standing crops were washed out. Geological and geomorphological investigation showed that a large area was dislocated at the head of the nala, moving down the gradient and activating the boulder filled nala. The mass of the mountain scree that moved was perhaps resting already at a critical angle and the torrential rains had triggered the flow. In August 1979 again a major gravitational slide had occurred, seriously affecting Sinsa, Gachhila, and Syankuri village situated on the above slope.
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GEOUGM 20:59 (1990)
Artikel Jurnal Universitas Indonesia Library
"Under normal conditions, a geomorphic system establishes a steady state with well-adjusted energy and material flow. Rainfall supplies the potential energy to channels and gradient converts it into kinetic energy. Thus, as a result of this process, erosion occurs. Hence, the moment adjustment between energy and material will be disturbed, the system will be distorted and the result will be slope instability. The present paper has been designed to evaluate the mechanism of slope instability with special reference to Central Himalayan district of India.
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GEOUGM 19:58 (1989)
Artikel Jurnal Universitas Indonesia Library
"In general, hydrological cycle in forested areas is a complicated phenomenon. In Himalaya the vegetative cover plays a vital role in determining several hydrological characters. For the experimental study of oak and pine forests hydrology, two representative basins are selected in the Central Himalaya. After evaluating the hydrological properties of oak and pine forests, it is decuded that both the vegetationt types have different hydrological characteristics. However, with the destruction of vegetation and top soil, rainfall quickly runoff as stormflow instead of soaking into the soils."
GEOUGM 21:62 (1991)
Artikel Jurnal Universitas Indonesia Library
Bhanja, K.C.
Darjcelany: Oxford, 1948
398.36 BHA m
Buku Teks Universitas Indonesia Library
Dullemen, Inez van
Amsterdam: Querido, 1990
839.36 DUL k
Buku Teks Universitas Indonesia Library
Spear, Percival
Ann Arbor: The University of Michigan Press, 1961
954 Spe i
Buku Teks Universitas Indonesia Library
Brown, Joe David
New York: Time Incorporated, 1961
954 BRO i
Buku Teks SO Universitas Indonesia Library
Hobbs, Lisa
New York: McGraw-Hill, 1967
954 HOB i
Buku Teks SO Universitas Indonesia Library
Chichester: John Wiley & Sons, 1996
551.307 LAN
Buku Teks SO Universitas Indonesia Library
Segal, Ronald
New York : New American Library, 1966
309.154 SEG a
Buku Teks SO Universitas Indonesia Library