1999
DOI: 10.1023/a:1007076813975
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Cited by 22 publications
(13 citation statements)
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“…The Bhaktapur Municipality is located in the weak geological structure having number of fault lines, with low bearing capacity and loose soil structure as physical limitations (Chapagain et al 2010;Shrestha et al 1999). The basement of the district is formed by Precambrian to Devonian rock which are intensely folded, faulted and fractured igneous and meta-sedimentary rocks and overlain by Quaternary fluvio-lacustrine deposit with the thickness of 550-600 m (Chapagain et al 2010).…”
Section: Geology Of the Regionmentioning
confidence: 99%
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“…The Bhaktapur Municipality is located in the weak geological structure having number of fault lines, with low bearing capacity and loose soil structure as physical limitations (Chapagain et al 2010;Shrestha et al 1999). The basement of the district is formed by Precambrian to Devonian rock which are intensely folded, faulted and fractured igneous and meta-sedimentary rocks and overlain by Quaternary fluvio-lacustrine deposit with the thickness of 550-600 m (Chapagain et al 2010).…”
Section: Geology Of the Regionmentioning
confidence: 99%
“…Fault lines are spread around the municipality which possesses limitation for construction, making most of the settlement area vulnerable. The soil found in and around the municipality is suitable for crop cultivation Environ Earth Sci (Shrestha et al 1999). In the study area, sticky clay constitutes top soil along with fine and coarse sand followed by clay with pebbles, cobbles and boulders over consolidated hard rocks of quartzite, basalt, granite, etc.…”
Section: Geology Of the Regionmentioning
confidence: 99%
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“…The basin fill sediments of Kathmandu Valley are mainly divided into two formations; Quaternary and Plio-pleistocene formation, each with different lithologic, geotechnical properties (Shrestha et al, 1999). Based on the engineering and environmental geological map of Kathmandu Valley (Shrestha et al, 1998), the geological setting of Kathmandu Valley with different formations is shown in Fig. 3.…”
Section: Study Areamentioning
confidence: 99%
“…The shallow aquifer of the valley is recharged mainly by direct infiltration from precipitation therefore net recharge was estimated by using following formula: The aquifer media map was developed based on various sources regarding groundwater basin and geological formation map of Kathmandu (Shrestha et al, 1998;JICA, 1990;Jha et al, 1997). Rating value was assigned based on DRASTIC method.…”
Section: Model Input Parameters and Groundwater Vulnerability Indexmentioning
confidence: 99%