Presentation is loading. Please wait.

Presentation is loading. Please wait.

Rocks.

Similar presentations


Presentation on theme: "Rocks."— Presentation transcript:

1 Rocks

2 Rocks Naturally occurring Solid mixture
Made of minerals, smaller rock fragments, organic matter, or glass

3 Rocks Grains Individual particles in rocks Texture
Refers to grain size and how the grains are arranged

4 Rocks Igneous Rocks 1. Formation
As magma or lava cools, mineral crystals form *Magma=molten rock inside earth *Lava=molten rock that erupts onto the surface

5 Rocks Igneous Rocks 2. Classification
Igneous rocks are classified by texture

6 Rocks Extrusive Rocks Fine-grained Small crystals
Formed from lava at the surface Cools quickly so crystals do not have time to increase in size

7

8 Rocks Intrusive Rocks Coarse-grained Large crystals
Formed from magma below the surface Cools slowly so crystals have time to increase in size

9

10

11 Intrusive Extrusive Rocks INSIDE the Earth Rocks OUTSIDE the Earth
Formed from magma Formed from lava Usually dark colored Usually light colored Usually dense Usually low density Mafic: magnesium and iron Felsic: feldspar Cools slowly Cools quickly Large grains Small or no grains (fine or glassy)

12 Rocks Igneous Rocks 3. Composition Minerals each rock contains
Often visible by color

13 Rocks Metamorphic Rocks 1. Formation When parent rocks are heated, squeezed (pressure), or exposed to hot fluids (magma/lava) Rocks don’t melt but texture and composition can be changed

14 Rocks 2. Classification Foliated
Metamorphic Rocks 2. Classification Foliated Distinct bands of light and dark minerals Results when uneven pressures cause flat minerals to line up Gives rock layered appearance

15 Rocks 2. Classification Nonfoliated Crystals become boxlike or square
Metamorphic Rocks 2. Classification Nonfoliated Crystals become boxlike or square Not flattened

16 Rocks Metamorphic Rocks

17 Rocks Sedimentary Rocks Sediments Lithification
Rock and mineral fragments that are loose and are suspended in water Lithification The process by which sediment turns into rock

18 Rocks Sedimentary Rocks 1. Formation Sediment formed by weathering
Moved by water, ice and wind Deposited in low areas Layers build up Dissolved minerals cement grains together Sedimentation Deposition Compaction Cementation

19 Rocks 2. Classification Texture (size of grains)
Sedimentary Rocks 2. Classification Texture Fine or coarse grained (size of grains) Rounded or angular grains (shape of grains)

20 Rocks 3. Composition Depends on minerals in the sediment
Sedimentary Rocks 3. Composition Depends on minerals in the sediment

21 Sedimentary Rock Mini Lab
Draw a 3 column chart. Column 1 can be small. List each rock number in column 1 on a chart. In column 2, describe each rock (2-3 bullet points). Describe texture (grain size and shape) as well as color. Gently scratch and #29 with the nail over black paper. What do you observe? Why does this happen? In column 3, explain why you think this rock is sedimentary. Use the characteristics of sedimentary rocks in your explanation.

22

23 Processes that change one rock type to another
Rocks The Rock Cycle Processes that change one rock type to another

24 Rocks The Rock Cycle Cooling and Crystallization Uplift
Weathering and Erosion Deposition Compaction and Cementation Temperature and Pressure Plate Tectonics

25 Rocks Cooling and Crystallization
The Rock Cycle Cooling and Crystallization Extrusive: when lava erupts, cools, and crystallizes on the surface Intrusive: when magma cools and crystallizes inside earth

26 Rocks Uplift Moving large amounts of rock up to earth’s surface
The Rock Cycle Uplift Moving large amounts of rock up to earth’s surface

27 Rocks Weathering and Erosion
The Rock Cycle Weathering and Erosion Glaciers, wind, rain break down rock and carries it to low areas

28 Rocks Deposition Laying of down sediment in a new location
The Rock Cycle Deposition Laying of down sediment in a new location Forms layers of sediment

29 Rocks Compaction and Cementation
The Rock Cycle Compaction and Cementation Weight of layers compacts or pushes grains closer As they crystallize, layers cement

30 Rocks Temperature (Heat) and Pressure
The Rock Cycle Temperature (Heat) and Pressure As temperature and pressure increase, rocks go through metamorphism

31 Rocks The Rock Cycle Plate Tectonics Processes that move tectonic plates also drive the rock cycle Main force = convection currents in the mantle

32


Download ppt "Rocks."

Similar presentations


Ads by Google