chapter 4. the rock cycle make sure your rock cycle is drawn!!
DESCRIPTION
The Rock Cycle Processes that shape the earth – Weathering- water, wind, ice, and heat break down rock – Erosion- process where water, wind, ice or gravity transports soil and sediment from one location to another – Deposition- process which material is at rest – Uplift- process where movement in the earth causes rocks from the inside of earth to moveTRANSCRIPT
Chapter 4
The Rock Cycle
• Make sure your rock cycle is drawn!!
The Rock Cycle
• Processes that shape the earth– Weathering- water, wind, ice, and heat break
down rock– Erosion- process where water, wind, ice or gravity
transports soil and sediment from one location to another
– Deposition- process which material is at rest– Uplift- process where movement in the earth
causes rocks from the inside of earth to move
The Rock Cycle
• Pg 92-93
The Rock Cycle
• Various paths to the rock cycle- pg 94• The rock cycle can vary and change in different
ways.• Three rock types– Sedimentary– Igneous– Metamorphic
Rock Cycle
After rock is classified into one of the 3 rock types it can be classified further- Composition- chemical makeup of a rock- Texture- size, shape, or position of a rock’s
grains
Igneous Rock
• Igneous rock begins as magma• Magma can form by– When rock is heated– When pressure is released– When rock changes compositions
Igneous Rock
• Composition and texture of igneous rock– Light colored rocks-less dense, rich in aluminum,
potassium, silicon, and sodium called felsic rocks– Dark colored rocks- mafic rocks, rich in calcium,
iron, and magnesium– Texture determined by how fast magma cools
Igneous Rock
• Igneous Rock Formations– Intrusive igneous rock: course grained texture,
cools slowly, pushes into rock below– Extrusive igneous rock: forms from magma that
erupts, cools rapidly
Sedimentary Rock
• Sedimentary rock forms near the surface of earth
• Materials that have been weathered form a natural cement that bonds rock and mineral fragments together
• Strata- most noticeable feature- layers
Sedimentary Rock
• Composition of Sedimentary rock- classified by way it is formed– Clastic- fragments of minerals together– Chemical- forms from solutions of dissolved
minerals and water– Organic- formed from fossils (limestone or coral)
coal is also organic
Sedimentary Rock
• Sedimentary rock structures– Most important feature of sedimentary rock-
stratification- rocks in layers– Sed. Rocks sometimes record motion of wind on
lakes, oceans, rivers, and sand dunes in features called ripple marks
– Mud cracks form when find grained sediments at the bottom of water are exposed to the air and dry out.
Metamorphic Rock
• Rocks in which the structure, texture, or composition have been changed.
• Contact metamorphism- heated with nearby magma, occurs near igneous intrusions
• Regional metamorphism- pressure builds up in a rock that is deep below the surface, occurs a distance away from earth’s surface
Metamorphic Rock
• Composition: occurs when temperature or pressure inside the earth’s crust change
• Texture: – Foliated- mineral grains arranged in planes or
bands – Nonfoliated- mineral grains not arranged in planes
or bands
Metamorphic Rock
• Deformation- change in the shape of a rock caused by a force placed on it. Folds or bends indicate a rock has been deformed.