SPEED LIMIT Academic Raceway Lesson Rock Forms 7 th Grade.

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SPEED LIMIT Academic Raceway Lesson Rock Forms 7 th Grade

description

The Rock Cycle The rock cycle is the process by which one rock type changes into another. Erosion begins and deposition into the Earth begins. 1 Sedimentary Rock : grains of sand and other sediment are eroded from the mountains and wash down a river to the sea. Over time, the sediment forms thick layers on the ocean floor. Eventually, the grains of sediment are pressed and cemented together, forming sedimentary rock. The rock cycle is the process by which one rock type changes into another. Erosion begins and deposition into the Earth begins. 1 Sedimentary Rock : grains of sand and other sediment are eroded from the mountains and wash down a river to the sea. Over time, the sediment forms thick layers on the ocean floor. Eventually, the grains of sediment are pressed and cemented together, forming sedimentary rock.

Transcript of SPEED LIMIT Academic Raceway Lesson Rock Forms 7 th Grade.

Page 1: SPEED LIMIT Academic Raceway Lesson Rock Forms 7 th Grade.

SPEEDLIMIT

Academic Raceway Lesson Rock Forms

7th Grade

Page 2: SPEED LIMIT Academic Raceway Lesson Rock Forms 7 th Grade.

The Rock Cycle

• The rock cycle is the process by which one rock type changes into another.

• Erosion begins and deposition into the Earth begins.

• 1 Sedimentary Rock : grains of sand and other sediment are eroded from the mountains and wash down a river to the sea. Over time, the sediment forms thick layers on the ocean floor. Eventually, the grains of sediment are pressed and cemented together, forming sedimentary rock.

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• Compaction and cementation begin and metamorphism results in 2 Metamorphic Rock – when large pieces of the Earth’s crust collide, some of the rock is forced downward. At these low levels, the intense heat and pressure “cooks” and squeezes the sedimentary rock, changing it into metamorphic rock.

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• 3 Magma : the hot liquid that forms when rock partially or completely melts is called magma. Where the metamorphic rock comes into contact with magma, the rock tends to melt. The material that began as a collection of sand grains now becomes part of the magma.

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• 4 Igneous Rock: The original sand grains from sedimentary have changed. Magma is usually less dense that the surrounding rock, so it tends to rise to higher levels of the Earth’s crust. Once there, it cools and solidifies, becoming igneous rock.

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• 5 Sediment: Erosion of the overlying rock exposes the igneous rock then weathers and wears away into grains of sand and clay. These grains of sediment are then transported and deposited elsewhere.

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Igneous Rock

• When magma cools below the Earth’s surface, the resulting rock is called intrusive.

• The texture of Igneous rocks differ from coarse grained to fine grained depending on the amount of time they had to cool.

• Igneous rocks that forms on the Earth’s surface are called extrusive.

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Sedimentary Rock

• The most noticeable feature of sedimentary rock is its layers, or strata.

• Sedimentary rock is classified by the way it is formed. There are three main ways in which it forms; Clastic, Chemical, and Organic.

• The most characteristic feature of sedimentary rock is stratification, or layering.

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Metamorphic Rock

• Meta-changed• Morphos-shape• One way rock can undergo metamorphism is by

coming into contact with magma.• All metamorphic rock has one of two textures:

foliated or Nonfoliated• Foliated : rocks that consist of minerals that are

aligned.• Nonfoliated : does not appear to have any

regular pattern.

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Lesson Review

• Rocks have been used for thousands of years, and they are just as valuable today.

• Rocks are classified into three main types-igneous, sedimentary, and metamorphic-depending on how they formed.

• The rock cycle describes the process by which a rock can change from one rock type to another.

• Scientists further classify rocks according to two criteria-composition and texture.

• Molten igneous material creates rock formations both below and above ground.