Sendra Granite Sendra Granite Sendra Granite is a plutonic igneous rock population which is part of Delhi supergroup of meta-sedimentary rocks located along NH-8 in Rajasthan, India. It has undergone years of sculpting by wind and air. It was declared as a Geoheritage Site by the Geological Survey of India in 1977. It is located at a Latitude of -26° 05´ 3.6" N and a Longitude of -74° 13´ 17.8" E and is at a height of 429.6 ± 5.7 m above sea level. Sendra Granite is located in the Pali district of Rajasthan in the north-west of India. The Sendra Granite
Granite, Colorado between high, sheer rock outcroppings of buff/pink-colored Precambrian granite. Granite lies at the center of the Colorado Mineral Belt (CMB), a 50 mile-wide strip that runs north and south for 300 miles. Mineralization of the CMB came primarily by way of intrusions of Tertiary Period magmas. The primary ores of the CMB were generally deposited as mixed metal sulfide mineral veins containing pyrite, galena, sphalerite, chalcopyrite, and gold, silver, and copper. During the last glacial period native gold was freed from the host rock and deposited along the ancient roaring Arkansas River bed - much larger than it is today