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
Fall River granite a mixture of the flesh red and light green varieties; the former predominating: the quartz is light gray, and the mica, usually black... it works easily and has a lighter and more lively appearance than Quincy granite. The granite quarry industry in Fall River had been established by 1840, employing 30 people, with the rock being transported to places such as Newport, New Bedford, Providence, Bristol, and New York City. Several granite quarries operated in the area in the late 19th century, the largest of which was the Beattie Granite Quarry, located near what is now North Quarry Street, near