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Slate and schist.

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9y ago
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4mo ago
  1. Marble: Formed from the metamorphism of limestone, marble is characterized by its interlocking crystals of calcite or dolomite. It is often used in sculpture and building materials due to its beauty and durability.

  2. Schist: Schist is a metamorphic rock with foliated layers that are often rich in mica minerals like biotite or muscovite. It forms under conditions of high temperature and pressure, resulting in a coarse-grained texture and well-developed foliation planes. Schist is commonly found in regions where regional metamorphism has occurred.

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Q: 2 metamophic rocks
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Continue Learning about Earth Science

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Igneous, sedimentary, and metamorphic rocks are the three main types of rocks. Igneous rocks are formed from the cooling of molten rock, sedimentary rocks from the accumulation of sediment, and metamorphic rocks from the transformation of existing rocks under heat and pressure.


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The three main types of rocks found in the lithosphere are igneous rocks, which form from cooled and solidified magma; sedimentary rocks, which result from the accumulation and compression of sediments; and metamorphic rocks, which are formed from the alteration of existing rocks due to high pressure and temperature.


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Pathway 2 includes the major groups of sedimentary and metamorphic rocks. Sedimentary rocks are formed from the accumulation and consolidation of sediments, while metamorphic rocks are formed from the alteration of existing rocks through heat and pressure. Both of these rock types are commonly involved in the rock cycle and can contribute to the formation of other rock types.


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Two examples of non-foliated rocks are marble, which forms from the metamorphism of limestone, and quartzite, which forms from the metamorphism of sandstone. These rocks do not have a layered or banded appearance like foliated rocks such as schist or gneiss.


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Igneous rocks form when magma cools and solidifies either underground (intrusive rocks) or on the Earth's surface (extrusive rocks). Intrusive rocks cool slowly, allowing large crystals to form, while extrusive rocks cool quickly, resulting in tiny crystals or glassy textures.

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