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Ann [662]
3 years ago
5

trace the journey of a piece of granite through the rock cycle. Explain how this rock could be changed from an igneous rock to a

sedimentary rock and then to a metamorphic rock
Geography
1 answer:
viva [34]3 years ago
4 0
A granite can be transformed from an igneous rock to a sedimentary rock and then to a metamorphic rock or the sedimentary rock can be transformed back into granite again by metamorphism. First of all, a granite often occurs in mountains and is susceptible to weathering and erosion.. Weathering such as argillic weathering can help break t he rock down to its constituent minerals which are mostly quartz, orthoclase feldspar and biotite mica. This then gets washed down into the rivers and thence to the coast and gets deposited in a marine environment as part of a delta or alluvial fan, in the form of sand, silt, clay and gravel. As this sediment becomes compacted, it turns into rocks like sandstone, siltstone etc. With deeper burial and the addition of heat and pressure these rocks get converted into such metamorphic rocks as quartzites, slates and phyllites, etc. I have seen a meta sandstone grade into a granite in the Canadian Shield so granite can then form from metamorphic processes as well as igneous processes.
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Answer:

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Explanation:

Question 1:

B. Increased heat and pressure may change the sedimentary rock into metamorphic rock.

In a subduction zone, sediments are usually subject high temperatures and pressures by which they change into metamorphic rocks. Metamorphic rocks are described as changed rocks.

  • In a convergent zone when a plate subducts beneath another, the rock is forced into an environment where heat and pressure is elevated.
  • With available water, a metamorphic change occurs leading to metamorphic rocks.
  • Along a subducting rock, different facies of metamorphic transformations are observed.
  • This slowly goes from low grade to high grade metamorphic transformation.

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Metamorphic change brainly.com/question/869769

Question 2:

A. Weathering and erosion.

Weathering and erosion are external processes that must have carved the canyon area from the surroundings.

  • Weathering is the physical disintegration and chemical decomposition of rocks to form sediments and soils.
  • In the process of erosion, the rocks, sediments and soils are then carried away from their original position into other places.
  • These processes combines and interacts to form powerful forces that causes denudation.
  • The major agents here are wind, water, ice, glacier and gravity.

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Erosion brainly.com/question/2473244

Question 3:

C. Igneous rock becomes sedimentary rock.

This change is rock cycle change from igneous to sedimentary rocks. This entails the remains of pre-existing forming clasts of sedimentary rocks.

  • The granite that is disintegrated by the process of weathering is an igneous rock. These are rocks that forms through the cooling and solidification of molten magma.
  • The sandstone that results from this process is a sedimentary rock. Sedimentary rocks are usually derived from pre-existing rocks.
  • The process of lithification and sediment compaction under significant pressure causes the sediments to transform igneous rocks.

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Compaction brainly.com/question/9131992

Question 4:

D. Clastic sedimentary rock forms from sediment, not from the remains of organisms.

The problem with the classification is that clastic sedimentary rocks are formed from sediments and not remains of organisms. Clastic sedimentary rocks are derived from pre-existing rock materials.

  • Examples are sandstone, silt, gravel e.t.c
  • They formed from sediments that gathers from the weathering of pre-existing rocks.
  • The limestone that formed from the shells of organisms is a biochemical sedimentary rock and not a clastic.

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Question 5:

C. The grains of the rock are aligned in a layered patterns.

The best feature that shows that a metamorphic rock is foliated is the layered arrangement of mineral grains in the rock. Due to intense nature of pressure and temperature metamorphic rocks are subjected to, most their minerals are usually aligned.

  • Pressure can caused the long axis of some platy minerals to form a special texture giving them a schistose foliation.
  • Temperature and pressure can combine to form a sort of metamorphic foliation known as gneissic layering in which the mica domains and quartz rich domains alternate simultaneously.
  • In low grade metamorphism, we can a have sort of slaty cleavage developing too.

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Contact metamorphism brainly.com/question/1970623

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<u>Answer:</u>

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