it is normally found in Europe, Asia and there is a little bit in New Jersey
The mineral you are referring to is called "Epidote." It is a green mineral that typically forms prismatic crystals and is commonly found in metamorphic rocks. Epidote's luster can range from glassy to pearly.
Epidote is not an igneous rock; it is a mineral that typically forms in metamorphic rocks and is sometimes found in igneous rocks as an accessory mineral. It is often associated with the alteration of plagioclase feldspar and can occur in high-grade metamorphic environments. Epidote is known for its distinctive green color and is commonly used as a gemstone.
The protolith for greenstone is usually basaltic or andesitic volcanic rock that has undergone metamorphism, resulting in the formation of chlorite, epidote, and actinolite minerals that give greenstone its characteristic green color. These rocks are typically found in greenschist facies metamorphic environments.
Unakite is formed through the metamorphism of granite, which results in the alteration of minerals such as feldspar, epidote, and quartz. This process occurs deep within the Earth's crust under high pressure and temperatures. The distinctive pink and green colors of unakite are due to the presence of pink orthoclase feldspar and green epidote.
Skarns are typically composed of minerals such as garnet, pyroxene, amphibole, epidote, and scapolite. They can also contain sulfide minerals like pyrite, chalcopyrite, and sphalerite, as well as carbonate minerals like calcite and dolomite. The exact chemical composition of a skarn can vary depending on the specific parent rock and the alteration processes that have occurred.
The mineral you are referring to is called "Epidote." It is a green mineral that typically forms prismatic crystals and is commonly found in metamorphic rocks. Epidote's luster can range from glassy to pearly.
Epidote, a nonmtallic mineral, can be used as a gemstone.
Epidote is not an igneous rock; it is a mineral that typically forms in metamorphic rocks and is sometimes found in igneous rocks as an accessory mineral. It is often associated with the alteration of plagioclase feldspar and can occur in high-grade metamorphic environments. Epidote is known for its distinctive green color and is commonly used as a gemstone.
The only known use of Epidote is as a precious stone used in jewelry.
Epidote is formed from a set of minerals, and it is used to form other mineral types of its own kind by chemical reactions on it.
Ayers Rock is located in the Northern Territory in Australia. It is composed of arkose and conglomerates made up of basalt, chlorite, and epidote.
Yes
Minerals are not classified as metamorphic. The mid-oceanic ridges are generally considered to be areas where new basaltic crust is formed from uprising magma. The basalt is considered an igneous rock in classification.
The color pistachio green resembles the color of pistachio nuts, a pale green hue with hints of yellow. This color is often associated with being calming and natural, and can sometimes be found in minerals like apatite or jade.
The protolith for greenstone is usually basaltic or andesitic volcanic rock that has undergone metamorphism, resulting in the formation of chlorite, epidote, and actinolite minerals that give greenstone its characteristic green color. These rocks are typically found in greenschist facies metamorphic environments.
There are numerous silicate minerals with second letter "p", including sphene, epidote, spodumene and apophyllite.
Unakite is formed through the metamorphism of granite, which results in the alteration of minerals such as feldspar, epidote, and quartz. This process occurs deep within the Earth's crust under high pressure and temperatures. The distinctive pink and green colors of unakite are due to the presence of pink orthoclase feldspar and green epidote.