Morphometric analysis is mathematical evaluation and measurement of the earth’s shape, surface its landform’s dimension. Dhund river basin in Jaipur district Rajasthan India has been carried out to evaluate various morphometric parameters following linear, areal relief aspects. The drainage basin, which covers a total area about 1828 km2 lies eastern part with maximum minimum elevation 603 m 21...

The Kordkanlo Basin, one of the Atrak sub-basins, located in the northeastern of the Ghoochan city, the Khorasan Razavi Province; is situated in Kopet Dagh geologic zone. The overall objective of this study is to evaluate the morphotectonic effects on the drainage network of the basin, using morphometric indicators. In this research, morphometric quantitative indicators of hypsometric integral ...

This study used morphometric techniques to generate new information describing the evolution and hydrogeological behaviour of Limpopo River Basin in Botswana, based on analysis drainage surface features, form, size. Drainage basins provide basic their evolution, which, when quantified, yield interaction between tectonics, climatic, processes. networks were extracted from Shuttle Radar Topograph...

The seismic activity observed in the vicinity of Ulaanbaatar (UB) capital city has been increased since 2005. Several active faults have identified UB area. Most Mongolian population is concentrated around (1.5 million), which main political and economic center country. Hence, study hazard first importance for In this paper, we present GPR results obtained on Songino fault situated at 20 km wes...

On 30 October 2020, a strong earthquake of magnitude 7.0 occurred north Samos Island at the Eastern Aegean Sea, whose mechanism corresponds to an E-W normal fault dipping north. During aftershock period in December hydrographic survey off northern coastal margin was conducted onboard R/V NAFTILOS. The result detailed bathymetric map with 15 m grid interval and 50 isobaths morphological slope ma...

Article history: The Himalayan orogenic bel Received 27 September 2007 Received in revised form 14 April 2008 Accepted 16 April 2008 Available online 3 May 2008