Rocks, Plate Tectonics

Magma

The molten mixture of rock-forming substances, gases, and water from the mantle.

Lava

Liquid magma that reaches the Earth's surface

Weathering

The chemical and physical processes that break down rock at the Earth's surface.

Erosion

The process by which water, wind, or gravity moves fragments of rock and soil

Deposition

The process by which sediments settle out of the water or wind that is carrying it, and is laid down in a new location

Sediment

Small, solid particles of materials from rocks or organisms which are moved by water or wind, resulting in erosion or deposition

Rock cycle

Set of natural processes that form, change, break down, and re-form rocks

How long does it take for rocks to change into different kinds of rocks?

Usually over a huge span of time: thousands to millions of years

Does the rock cycle have a beginning or end?

It has no beginning or ending but goes on continually; allows rocks to change from one form to another

How are igneous rocks formed?

Forms when molten rock cools and becomes solid.

Where can igneous rocks form?

Form on the surface of the Earth (extrusive) and on the inside of the Earth (intrusive)

How are sedimentary rocks formed?

Forms when pieces of older rocks, plants, and other loose material get pressed or cemented together

Where are older and younger layers of sediment located?

younger layers are found toward (or on) the surface of the Earth and older are found toward (or at) the bottom of the rock

Metamorphic rocks formation

This type of rock forms when heat or pressure cause older rocks (igneous or sedimentary) to change into new types of rocks.

Metamorphic rocks are located

These rocks can be found inside the Earth and/or raised to Earth's surface over time.

The layers of the Earth

inner core, outer core, mantle, crust

inner core

ball of hot, solid metals at the center of the Earth

Metals found in the inner core

Iron and nickel

How Earth's core be solid AND hot at the same time.

There is enormous pressure at the center of Earth. This squeezes the atoms of the metals so closely together that the core remains solid despite the intense heat

Pressure, temperature, and density change as move from the crust to the core.

It increases as you move from the crust to the core

Temperature, pressure, density change as move from the core to the crust.

It decreases as you move from the core to the crust

outer core

A layer of liquid metals that surrounds the inner core

Why the outer core is liquid.

The lower pressure allows the metals to remain liquid

Mantle

Earth's thickest layer, made of hot rock that is less dense than the metallic core

Describe the top part of the mantle and the region just below it.

The very top part of the mantle is cool and rigid. Just below that, the rock is hot and soft enough to move like a thick paste.

crust

Thinnest layer of the Earth. Made of cool rock

Two basic types of crust.

oceanic crust and continental crust

continental crust

Includes all continents and some major islands

oceanic crust

Includes all the ocean floors

Where the Earth's crust the thinnest.

Under the oceans (oceanic crust)

Where the Earth's crust the thickest.

Under continental mountain ranges (continental crust)

lithosphere

Earth's crust and the very top of the mantle
Most rigid of all the layers *Sits on top of the asthenosphere

asthenosphere

*Layer of hotter, softer rock in the upper mantle.
*Soft enough to flow slowly like hot tar

tectonic plates

Many broken large and small slabs of rock (lithosphere)

The crust make up most tectonic plates.

Continental crust (rises above the ocean) and oceanic crust (ocean floor)

Description of Earth 4.6 billion years ago.

Earth was a spinning mass of rocks and dust loosely held together.

Events over time to change the Earth to change the Earth's mass and turn it into a glowing ball of rock.

Many comets and asteroids crashed into its surface and added to its mass. These impacts, along with radioactive decay and Earth's gravity, produced intense heat. The young planet became a glowing ball of melted rock.

Where materials with greater density ended up. Give 2 examples of these denser materials.

Denser materials, such as iron and nickel, sank toward the center of Earth.

Where less dense materials that make up the Earth eventually ended up.

Less dense materials moved toward the surface.

Where materials that were not the most dense nor the least dense ended up during the formation of the Earth.

-Other materials settled between the planet's center and its surface.
-Slowly, Earth's main layers formed�the core, the mantle, and the crust

Pangaea

name of the super continent that existed 200 million years ago, the name means "all land

continental drift

the hypothesis that states that the continents once formed a single landmass, broke up, and drifted to their present locations

seafloor spreading

Hess's theory that new seafloor is formed when magma is forced upward toward the surface at a mid-ocean ridge, forcing the plates away from each other

convection current

the movement of a fluid, caused by differences in temperature and density, that transfers heat from one part of the fluid to another