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Copper ore is typically found in igneous rocks, such as basalt or granite, as well as in sedimentary rocks like shale. The most common type of rock where copper ore is extracted is called porphyry copper deposits, which are a combination of igneous and sedimentary rocks. These rocks contain copper minerals like chalcopyrite, bornite, and chalcocite, which are essential for copper extraction.
No, cyanotrichite is not an igneous rock. It is a secondary mineral that forms in oxidized copper deposits.
Copper is commonly found in igneous and sedimentary rocks, typically associated with areas of volcanic activity or hydrothermal deposits. It can also be found in some metamorphic rocks that have undergone mineral alterations.
No, in fact plenty of fossils are found in sedementary rocks.
because most intrusive igneous rock are found underground and diorite is found under the earth.
No. There some very old igneous rocks to be found also it is possible for an igneous rock to become a metamorphic rock. Further, igneous rocks can not be turned into a sedimentary rocks directly. They must first be weathered and eroded and only then their detritus and remnants can be deposited as a new sedimentary deposit.
Igneous rock is rock that formed from molten material. Volcanoes erupt lava and pyroclastic material, which forms extrusive igneous rock. Magma can solidify with in a volcano, forming intrusive igneous rock.
Zircon is ZrSiO4 and it is found in igneous rock>.<
No, metamorphic can be formed by either igneous or sedimetary rock.
A xenolith is a foreign inclusion in an igneous rock. A xenocryst is a crystal, resembling a phenocryst, in an igneous rock that is foreign to the body of rock in which it occurs. Xenocryst is just more specific, talking only about crystals, whereas a xenolith could be any type of inclusion
The beauty of the igneous rock is not always found. Only a few people appreciate it. Most people use is as a kitchen table. But, that way the beauty might be seen by everyone around.
Peacock ore, also known as bornite, is a sulfide mineral composed of copper, iron, and sulfur. It is not an igneous rock; instead, it is typically formed through hydrothermal processes in copper ore deposits.