The Granite Rock Cycle

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The granite rock cycle.

Lc geography core chapter 5 the rock cycle 30 terms. The granite pictured above is an example of this type of rock formation. Dublin region tertiary economic activities. An example of this transformation can be seen with granite an igneous rock.

Of course the granite we see today is near surface and thus at some point was uplifted causing overlying sediment to be shed via erosion. Granite is composed mainly of quartz and feldspar with minor amounts of mica amphiboles and other minerals. They can even be re melted to form new igneous rocks. Igneous rocks cycle after igneous rocks have been formed they can be transformed into metamorphic or sedimentary rocks.

Granite is an intrusive igneous rock which is widely distributed throughout earth s crust at a range of depths up to 31 mi 50 km. Granite s characteristic grainy structure and strength is the result of many individual crystalline structures which form tightly together as magma slowly cools within large deeply buried rock bodies known as. Other sets by this creator. This transition from high pressure and temperature to atmospheric temperature and pressure can cause the granite to slightly expand and crack.

Granite contains long and platy minerals that are not initially aligned but when enough pressure is added those minerals shift to all point in the same. The rock cycle is a series of processes that create and transform the types of rocks in earth s crust. It forms from the slow crystallization of magma below earth s surface. Spanish vocab 2 115 terms.

This mineral composition usually gives granite a red pink gray or white color with dark mineral grains visible throughout the rock. To find out about how these changes take place return to the rock cycle. Analogous to recycling a coke can where an old can.