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The Marble Rocks is an area along the Narmada River in central India near the city of Jabalpur; in Bhedaghat of Jabalpur District, in the state of Madhya Pradesh. The river has carved the soft marble , creating a beautiful gorge of about 8 km (5.0 mi) in length.
[4] [3] The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, CaMg(CO 3) 2. Magnesian limestone is an obsolete and poorly-defined term used variously for dolomite, for limestone containing significant dolomite ( dolomitic limestone ), or for any other limestone ...
Jasper, an aggregate of microgranular quartz and/or cryptocrystalline chalcedony and other mineral phases, [1] [2] is an opaque, [3] impure variety of silica, usually red, yellow, brown or green in color; and rarely blue.
The Dhuandhar Falls is located on the Narmada River in Bhedaghat and are 30 meters high. The Narmada River, making its way through the world-famous Marble Rocks, narrows down and then plunges into a waterfall known as Dhuandhar.
Stones are still the mainstays of civil construction in India, with stones being used extensively in public buildings, hotels, and temples. They are increasingly being used in homes, with the use of stones now penetrating amongst the growing middle class of India. The success of the commercial stone industry solely depends on defects in rock/stone.
Oolite – Sedimentary rock formed from ooids; Rag-stone – Work done with stones that are quarried in thin pieces; Shelly limestone – Limestone containing many fossils; Travertine – Form of limestone deposited by mineral springs; Tufa – Porous limestone rock formed when carbonate minerals precipitate out of ambient temperature water
Granite is a natural source of radiation, like most natural stones. Potassium-40 is a radioactive isotope of weak emission, and a constituent of alkali feldspar , which in turn is a common component of granitic rocks, more abundant in alkali feldspar granite and syenites .
Marble is a rock resulting from metamorphism of sedimentary carbonate rocks, most commonly limestone or dolomite. Metamorphism causes variable re-crystallization of the original carbonate mineral grains. The resulting marble rock is typically composed of an interlocking mosaic of carbonate crystals.