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The Precambrian rocks of India have been classified into two systems, namely the Dharwar system and the Archaean system (gneiss and schists). The Dharwar System. The rocks of the Dharwar system are mainly sedimentary in origin, [8] and occur in narrow elongated synclines resting on the gneisses found in Bellary district, Mysore and the Aravalis ...
Exposed gneiss hillock at Lal Bagh Geological Map of South India – The Dharwars of South India. The Archean gneisses and schists, which are the oldest rocks of the Indian Shield, constitute a considerable area of Peninsular India. The Dharwar (Super Group) and the Peninsular Gneissic Complex are the classified groups of the Precambrian rocks ...
Igneous rock (igneous from Latin igneus 'fiery'), or magmatic rock, is one of the three main rock types, the others being sedimentary and metamorphic. Igneous rocks are formed through the cooling and solidification of magma or lava. The magma can be derived from partial melts of existing rocks in either a planet's mantle or crust.
The Deccan is a plateau extending over an area of 422,000 km 2 (163,000 sq mi) and occupies the majority of the Indian peninsula.Shaped like an inverted triangle, it stretches from the Satpura and Vindhya Ranges in the north to the northern fringes of Tamil Nadu in the south.
Malani Igneous Suite Contact below Mehrangarh Fort in Jodhpur. Jodhpur Group-Malani Igneous Suite Contact of Aravalli range is a geological feature representing the last phase of igneous activity of Precambrian age in the Indian Subcontinent at the foot of the picturesque Mehrangarh Fort in Jodhpur city, the second largest city in Rajasthan after Jaipur.
4. “Monster Rock” near Film Nagar, Jubilee Hills; 5. “Obelisk”, Jubilee Hills; 6. “Mushroom Rock” inside the University of Hyderabad Campus; 7. Rock Park, on Old Bombay Road near Dargah Hussain Shah Wali; 8. Sentinel Rock, near Moula-Ali; 9. Rocks at Maula Ali's Dargah, Moula-Ali; 10. “Toadstool” next to Blue Cross, Jubilee Hills
The following is a list of rock types recognized by geologists.There is no agreed number of specific types of rock. Any unique combination of chemical composition, mineralogy, grain size, texture, or other distinguishing characteristics can describe a rock type.
The second model states that the rocks got to a certain point in subduction and then were forced back up through the channel they came down due to a space problem. The third model states that the thick continental crust of India further exacerbated the space problem and caused the corner flow of those rocks back up the channel.