THE EARTH!. EARTH’S LAYERS 1. CRUST: The rigid, rocky, thin outer layer. 23.5 miles thick.
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Transcript of THE EARTH!. EARTH’S LAYERS 1. CRUST: The rigid, rocky, thin outer layer. 23.5 miles thick.
2. MANTLE:
• Rocky layer containing magma• thickest layer under the crust• Made of metals• 1775 miles thick•1600-6700 degrees
Magma is molten material under the surface of the earth.
3. OUTER CORE:• Made of molten iron-nickel• surrounds the inner core• 1420 miles thick. Liquid.• 6700-8000 degrees.
4. INNER CORE:
• Center of the earth• solid iron-nickel• very hot and under
great pressure.• 767.5 miles thick•13,000 degrees
Convection
• Circular movement where hot air or magma rises and the cooler air sinks causing a circular pattern.
• Causes the plates to move.
1. Geosphere: the solid rocky surface and the inside of the planet.
2. Hydrosphere: earth’s water in seas and on land.
3. Atmosphere: the air that surrounds earth.
4. Biosphere: all living things on earth!5. Lithosphere: A layer that combines
the crust and the upper mantle.
•Pressure, density, and temperature increase the deeper into the surface of the earth.
•Pressure and density decrease the farther from earth.
SEDIMENTARYFORMS: *From
sediments compacting and
cementing together.
CHANGES:*under
weathering and erosion turns into sediments.
*Into metamorphic rocks under heat and pressure
EXAMPLES:
SandstoneLimestoneShale
IGNEOUSFORMS: *from
cooling magma
CHANGES:*under heat and
pressure turns into metamorphic rocks
*under weathering and erosion turns into sediments.
*can melt.
EXAMPLES:
GraniteBasaltPumiceObsidian
METAMORPHICFORMS: *under
heat and pressure
CHANGES:*can melt and
turn into magma
*under weathering and erosion turns into sediments.
*into Igneous rocks when magma cools
EXAMPLES:
QuartzSlateMarble
Continental Drift Theory:•Alfred Wegener first proposed the theory of continental drift, which states that parts of the Earth's crust slowly drift a top a liquid core. • Pangea—all landmasses connected.• Fossil records prove this to be true.
Plate Tectonic Theory• This theory explains the movement of the Earth's plates and also explains the cause of earthquakes, volcanoes, oceanic trenches, mountain range formation, and other geologic phenomenon.
Constructive processes:•Deposition•Mountain Building
Destructive processes• Weathering• Erosion• Mass Movement
TYPES OF CATASTROPHES:1. Volcano eruption2. Asteroid Impact
RESULTS FROM CATASTROPHES:
*change climate*causes mass extinction* noted in rock layers &
fossils
Three types of plate movement: Convergent: plates move together
causing mountain building
Divergent: plates moving apart
Lateral slipping (transform): plates slide beside each other, causing earthquakes
Caused by:Plates rubbing together
2 parts: Focus: the spot underground where
the earthquake begins.
Epicenter: the spot above ground where the earthquakes spreads out.
Caused by:Magma deep within the earth rises
to the surface due to the plates.
Volcanoes are located around plate boundaries
Types of volcanoes: a.Cinder coneb.Shield c.Composite
A. PHYSICAL WEATHERING 1. DEFINITION: Breaks rocks into
smaller and smaller pieces 2. Three types of Physical
Weatheringa. FROST WEDGING: b. ABRASION: c. LIVING ORGANISMS: plant roots, animals burrowing
B. CHEMICAL WEATHERING 1. DEFINITION: Changes rocks and
minerals into new chemical combinations
2. Three types of Chemical Weatheringa. SOLUTION WEATHERING: b. OXIDATION: oxygen combines with iron and water. Example: rusty nailsc. LICHENS AND MOSSES: release acid which breaks down rocks.
II EROSION A. Four Types of Erosion
1. GRAVITY: causes mass movement. 2. RUNNING WATER: carries particles
away and sorts them. MOST POWERFUL3. ICE: rocks frozen in ice contribute to physical weathering by abrasion. Glaciers4. WIND: particles are picked up and carried off.
III. DEPOSITIONA. Sand grains have formed due to weathering and erosion and have been transported by wind, water, and ice.
B. The sand is then deposited in a new area and forms sedimentary rocks.
A. sediments settle and form a flat, horizontal layer.B. The rock layer on the bottom is the oldest.C. The processes we observe today have occurred this way throughout Earth’s history.
IV. Other Rock Information
SOIL1. Soil is a layer of dirt between the
atmosphere and the bedrock in the tectonic plates.
2. Soil is found on the surface of the lithosphere.
SOIL3. It is made up of minerals (rock, clay, sand, silt), water, air, and organic (plants and animals) material.
4. There are many types of soil. Each unique by color, texture, and minerals.
SOIL5. Soil is formed slowly as rocks
erode.
6. Organic matter decays and mixes with inorganic material to form soil.
7. Soil is divided into layers. They are called horizons.
8. The bottom horizon develops first.
9. Humus is rich organic material.
Water1.Found on the earth:
oceans, seas2.Found under the earth:
streams, drains3.Found in the
atmosphere: vapor, clouds
Ocean Water1. Oceans cover about 70% of the earth’s surface.2. Oceans contain roughly 97% of earth’s water supply. 3. We are the only planet with water. 4. Oceans affect the weather and temperature of earth. 5. Oceans moderate the earth’s temperature by absorbing incoming solar radiation and stores it as heat energy.
Ocean Water6. Ocean currents are constantly moving and distribute heat energy around the world. 7. All the oceans are connected to each other. 8. As water flows in rivers it picks up small amounts of mineral salts from rocks and soil. Then it flows into the oceans and seas. Salt does not evaporate like water, which is why the ocean water gets salty.
Fresh Water1.Fresh water is located in
streams, lakes, and rivers. 2.Reservoirs store water for
future use. 3.Estuaries are where fresh
water and salt water mix.
2. 2. ERA:ERA: broad span of time broad span of time based on the life that existed. based on the life that existed. “Zoic” refers to animal life. “Zoic” refers to animal life.
3. 3. PERIOD:PERIOD: shorter spans of time shorter spans of time—based on earth’s crust and —based on earth’s crust and rock formation.rock formation.
4. 4. EPOCHEPOCH: based on layers of : based on layers of rock. Names are based on the rock. Names are based on the % of fossils in the rocks % of fossils in the rocks represented by animals and represented by animals and plants living today.plants living today.
FOSSILSFOSSILS
Any remains, trace or imprint of a plant or animal that has been
preserved in the earth.
Index FOSSILSIndex FOSSILS
A fossil found in only A fossil found in only one layer of rock in an one layer of rock in an area. It can identify the area. It can identify the age of the specific rock age of the specific rock
layer it is found in.layer it is found in.
Paleontologist: scientist who Paleontologist: scientist who studies fossils.studies fossils.
Geologist: scientist who studies Geologist: scientist who studies the earth…rocksthe earth…rocks