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Rocks and the Rock Cycle

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Page 1: Rocks and the Rock Cycle. Classifying Rocks By: Texture Grain size Shape Patterns Mineral Composition

Rocks and

the Rock Cycle

Page 2: Rocks and the Rock Cycle. Classifying Rocks By: Texture Grain size Shape Patterns Mineral Composition

Classifying Rocks

By: •Texture •Grain size •Shape•Patterns •Mineral Composition

Page 3: Rocks and the Rock Cycle. Classifying Rocks By: Texture Grain size Shape Patterns Mineral Composition

Texture•The look and feel of the rock’s surface.

•Rough, chalky, smooth or glassy.

Page 4: Rocks and the Rock Cycle. Classifying Rocks By: Texture Grain size Shape Patterns Mineral Composition

Grain Size

• The size of the actual grain in the rock.

• They are fined-grained, coarse-grained, or no visible grains.

Page 5: Rocks and the Rock Cycle. Classifying Rocks By: Texture Grain size Shape Patterns Mineral Composition

Grain Shape

•Is the way a grain looks on a rock.

Page 6: Rocks and the Rock Cycle. Classifying Rocks By: Texture Grain size Shape Patterns Mineral Composition

Grain Pattern

•The patterns of the grains form are wavy, swirling, or like a stack of planks.

•Some rocks have no visible grains even under a microscope.

Page 7: Rocks and the Rock Cycle. Classifying Rocks By: Texture Grain size Shape Patterns Mineral Composition

Mineral Composition

•Will show the mineral composition in the rocks.

•Minerals are found by a series of tests.

Page 8: Rocks and the Rock Cycle. Classifying Rocks By: Texture Grain size Shape Patterns Mineral Composition

Types of Rocks

There are three major types: • Igneous – a type of rock formed

from the cooling of lava. •Sedimentary – a type of rock

that forms when sediments are compacted.

•Metamorphic – forms when existing rocks are changed by heat and pressure.

Page 9: Rocks and the Rock Cycle. Classifying Rocks By: Texture Grain size Shape Patterns Mineral Composition

Igneous Rocks

•Classified according to their origin, texture, and mineral composition.

•Extrusive rocks – igneous rocks formed from lava that erupted onto the Earth’s surface.

•Basalt is the most common extrusive rock.

Page 10: Rocks and the Rock Cycle. Classifying Rocks By: Texture Grain size Shape Patterns Mineral Composition

Igneous Rocks

• Intrusive Rocks –formed when magma hardened under the Earth.

• Granite is most abundant intrusive rock in the continental crust.

• Granite forms the core of many mountain ranges.

Page 11: Rocks and the Rock Cycle. Classifying Rocks By: Texture Grain size Shape Patterns Mineral Composition

Igneous Rocks

•Basalt is an extrusive rock. •Magma that is high in silica usually forms lighted colored rocks such as granite.

•Many igneous rocks are hard, dense and durable.

Page 12: Rocks and the Rock Cycle. Classifying Rocks By: Texture Grain size Shape Patterns Mineral Composition

Igneous Rock Texture • Depends on the size and shape

of the mineral crystals. • Maybe glassy, coarse-grained,

or porphyritic. • Intrusive rocks have large

grains.• Slow cooling magma forms

coarse-grained rocks. • Extrusive rocks have a fine-

grained or glassy texture.

• Rapid cooling lava forms fine grained rocks.

Page 13: Rocks and the Rock Cycle. Classifying Rocks By: Texture Grain size Shape Patterns Mineral Composition

Igneous Rock Texture• Porphyritic rocks have both

fine-grains and large crystals scattered throughout.

• Porphyritic rocks form when intrusive rocks form in 2 stages.

• Magma begins to cool slowly making large crystals while the other materials around it cool quickly making a fine grained background.

Page 14: Rocks and the Rock Cycle. Classifying Rocks By: Texture Grain size Shape Patterns Mineral Composition

Sedimentary Rocks

What is it ? •Rocks formed from particles

deposited by water and wind. •Sediments are small pieces of

material that come from rocks or living things.

•Sediments may include shells, bones, leaves, stems, and other remains of living things.

Page 15: Rocks and the Rock Cycle. Classifying Rocks By: Texture Grain size Shape Patterns Mineral Composition

Erosion and Deposition

•Wind, water, and ice can carry sediment and deposit it in layers.

•Erosion breaks up rocks. •Deposition is the process by which sediment settles out of the water or wind.

Page 16: Rocks and the Rock Cycle. Classifying Rocks By: Texture Grain size Shape Patterns Mineral Composition

Compaction and Cementation

• Compaction and cementation over millions of years, thick layers of sediment build up Compaction is the process that presses sediments together. New layers help compact layers underneath. While being compacted minerals slowly dissolve in the water. Minerals seep into spaces between particles of sediment. This is called sedimentation.

Page 17: Rocks and the Rock Cycle. Classifying Rocks By: Texture Grain size Shape Patterns Mineral Composition

Types•There are 3 major groups of

sedimentary rocks.•Clastic forms when rock fragment

are squeezed together. •Organic forms from remains of

plants and animals. •Chemical form when minerals are

dissolved in a solution crystallize.

Page 18: Rocks and the Rock Cycle. Classifying Rocks By: Texture Grain size Shape Patterns Mineral Composition

Uses•Sandstone and limestone have been used as building materials. Limestone is also important when smelting iron ore.

Page 19: Rocks and the Rock Cycle. Classifying Rocks By: Texture Grain size Shape Patterns Mineral Composition

Metamorphic Rock

Page 20: Rocks and the Rock Cycle. Classifying Rocks By: Texture Grain size Shape Patterns Mineral Composition

What is a Metamorphic Rock?

• Any rock that can be changed into a metamorphic rock by heat and pressure.

• Can change from igneous, sedimentary, and other metamorphic rocks.

• The deeper the rock in the Earth the more heat and pressure.

Page 21: Rocks and the Rock Cycle. Classifying Rocks By: Texture Grain size Shape Patterns Mineral Composition

How to classify a Metamorphic Rock?

• Geologists classify metamorphic rocks by the arrangement of the grains that make up the rocks.

• Metamorphic rocks have their grains in bands said to be foliated.

• Metamorphic rocks without bands are called nonfoliated.

Page 22: Rocks and the Rock Cycle. Classifying Rocks By: Texture Grain size Shape Patterns Mineral Composition

Metamorphic Rocks

•Most of metamorphic rocks are extremely hard.

•Some examples are slate, gneiss and quartzite which come from shale, granite, and sandstone.

Page 23: Rocks and the Rock Cycle. Classifying Rocks By: Texture Grain size Shape Patterns Mineral Composition

Metamorphic Rocks

•Metamorphic rocks can be sued for many different things.

•The Taj Mahal in India is made from the metamorphic rock marble.

•Chalkboards, flooring, roofing, walkways are created from slate, which comes in different colors.

Page 24: Rocks and the Rock Cycle. Classifying Rocks By: Texture Grain size Shape Patterns Mineral Composition

Metamorphic Rocks

•Heat and pressure deep beneath the Earth’s surface can change any rock into metamorphic rocks.

Page 25: Rocks and the Rock Cycle. Classifying Rocks By: Texture Grain size Shape Patterns Mineral Composition

Rock Cycle•Forces with in the Earth build, destroy, and change rocks. The different paths a rock can take form the Rock Cycle.

Page 26: Rocks and the Rock Cycle. Classifying Rocks By: Texture Grain size Shape Patterns Mineral Composition
Page 27: Rocks and the Rock Cycle. Classifying Rocks By: Texture Grain size Shape Patterns Mineral Composition

Processes within the Rock Cycle

•Erosion•Melting•Heat and Pressure

Page 28: Rocks and the Rock Cycle. Classifying Rocks By: Texture Grain size Shape Patterns Mineral Composition

MeltingErosion

Page 29: Rocks and the Rock Cycle. Classifying Rocks By: Texture Grain size Shape Patterns Mineral Composition

Rock Cycle and Plate Tectonics

•Rock Cycle is driven by Plate Movement

•Plates press rocks into the mantle, forming magma.

•Plate movement creates the heat and pressure required for the formation of metamorphic rock.