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Showing posts from September, 2014

Slide show of Deluge in Jammu and Kashmir, India.

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Heavy rainfalls battered the western Himalayas last week due to a clash between monsoon currents and winds from the Caspian Sea.  by Dr. Nitish Priyadarshi Geologist Ranchi.

Deluge in Jammu and Kashmir.

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Inadequate surface drainage and encroachment in the floodplains has caused the floods of Kashmir. By Dr. Nitish Priyadarshi Geologist Ranchi . Heavy rainfalls battered the western Himalayas last week due to a clash between monsoon currents and winds from the Caspian Sea. The Srinagar weather station – in the summer capital of the Indian state of Jammu and Kashmir – recorded 250 mm of rain between September 3-6. For hundreds of million years Kashmir Valley is supposed to have remained under Tethys Sea and the high sedimentary-rock hills seen in the valley now were once under water. Geologists have come to believe that Kashmir Valley was earlier affected by earthquakes. Once there was such a devastating earthquake that it broke open the mountain wall at Baramulla and the water of the Satisar lake flowed out leaving behind latchstring mud on the margins of the mountains known as karewas. Thus came into existence the oval but irregular Valley of Kashmir. In September 2014, the ...

Geology of Pithoria hills near Ranchi city, India.

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The hills of Ranchi are generally small isolated residual hills.  By Dr. Nitish Priyadarshi.  Fig.1. A small hill in Pithoria. The hills of Ranchi are generally small isolated residual hills. In Ranchi hills are generally steepsided made of massive granite-gneiss. We have also found the hills which are not steepsided but a mere irregular pile of huge boulders were found on the hills especially in Pithoria area of Ranchi district. This is the result of highly jointed elements of granite gneiss. According to climatic geomorphologist like Tricart qualify such hills as inselbergs. They are steepsided residual hills made of massive granite-gneiss. But close by within a few kilometers or a few hundred meters we have residuals which are not steepsided inselbergs but a mere irregular pile of huge boulders. The rocks disintegrate along these joints under the hydrothermal and atmospheric effects thus leading to the formation of tors or rounded shapes of these ancient granite rocks a...