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Chapter 3 rth’s Structure and Materi and a few Chapter 2

Chapter 3 Earth’s Structure and Materials and a few Chapter 2

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Page 1: Chapter 3 Earth’s Structure and Materials and a few Chapter 2

Chapter 3 Earth’s Structure and Materials

and a few Chapter 2

Page 4: Chapter 3 Earth’s Structure and Materials and a few Chapter 2

Lithosphere

A rigid layer made up of the uppermost part of the mantle and the crust.

Page 5: Chapter 3 Earth’s Structure and Materials and a few Chapter 2

Basalt

A dark, dense, igneous rock with fine texture, found in ocean crust.

Page 6: Chapter 3 Earth’s Structure and Materials and a few Chapter 2

Pressure

The force pushing on a surface divided by the area of that surface.

Page 7: Chapter 3 Earth’s Structure and Materials and a few Chapter 2

Granite

A usually light colored igneous rock that is found

in continental crust.

Page 9: Chapter 3 Earth’s Structure and Materials and a few Chapter 2

Inner Core

A dense sphere of solid iron and

nickel at the center of Earth.

Page 10: Chapter 3 Earth’s Structure and Materials and a few Chapter 2

MantleThe layer of hot, solid material between Earth’s

crust and core.

Page 12: Chapter 3 Earth’s Structure and Materials and a few Chapter 2

Seismic Wave Vibrations that travel through Earth carrying the

energy released during an earthquake.

Page 13: Chapter 3 Earth’s Structure and Materials and a few Chapter 2

Outer Core

A layer of molten iron

and nickel that surrounds the inner core of

Earth.

Page 14: Chapter 3 Earth’s Structure and Materials and a few Chapter 2

Crust

The layer of rock that forms Earth’s outer surface.

Page 15: Chapter 3 Earth’s Structure and Materials and a few Chapter 2

TO DESCRIBE A ROCK’S TEXTURE, GEOLOGISTS DETERMINE WHAT THREE THINGS:

SIZE, SHAPE, AND THE PATTERN OF THE ROCK’S GRAIN

Page 16: Chapter 3 Earth’s Structure and Materials and a few Chapter 2

Radiation

The transfer of energy by electromagnetic

waves.

Page 17: Chapter 3 Earth’s Structure and Materials and a few Chapter 2

Conduction

The transfer of thermal energy from one particle of matter to another

Page 18: Chapter 3 Earth’s Structure and Materials and a few Chapter 2

GrainThe particles of minerals or other rocks that give a rock its texture.

Page 20: Chapter 3 Earth’s Structure and Materials and a few Chapter 2

DensityThe

measurement of how much mass of a substance is

contained in a given volume.

Page 21: Chapter 3 Earth’s Structure and Materials and a few Chapter 2

What are two useful metamorphic rocks?

Marble and slate

Page 22: Chapter 3 Earth’s Structure and Materials and a few Chapter 2

Convection

The transfer of thermal energy by the movement of a fluid.

Page 23: Chapter 3 Earth’s Structure and Materials and a few Chapter 2

Rock-Forming Mineral

Any of the common minerals that make

up most of the rocks of Earth’s crust.

Page 24: Chapter 3 Earth’s Structure and Materials and a few Chapter 2

Asthenosphere

The soft layer of the mantle on which the lithosphere floats.

Page 25: Chapter 3 Earth’s Structure and Materials and a few Chapter 2

Texture

The look and feel of a rock’s surface, determined by the size, shape and

pattern of a rocks grains.

Page 26: Chapter 3 Earth’s Structure and Materials and a few Chapter 2

Igneous Rock

A type of rock that forms from the cooling of molten rock at or below the surface.

Page 27: Chapter 3 Earth’s Structure and Materials and a few Chapter 2

The most abundant type of intrusive rock in the continental crust is:

Granite

Page 28: Chapter 3 Earth’s Structure and Materials and a few Chapter 2

Sediment Earth

materials deposited by

erosion.

Page 29: Chapter 3 Earth’s Structure and Materials and a few Chapter 2

Forms from sand on the beaches, ocean floor, river beds, and sand dunes.

SANDSTONE

Page 31: Chapter 3 Earth’s Structure and Materials and a few Chapter 2

Metamorphic Rock

A type of rock that forms from an

existing rock that is changed by heat,

pressure, or chemical reaction.

Page 32: Chapter 3 Earth’s Structure and Materials and a few Chapter 2

Extrusive Rock Igneous rock that forms from lava on Earth’s surface

Page 34: Chapter 3 Earth’s Structure and Materials and a few Chapter 2

What step in the rock cycle would be required to change granite into sandstone?

Granite Particles settle on the ocean floor.

Page 35: Chapter 3 Earth’s Structure and Materials and a few Chapter 2

Intrusive Rock

Igneous rock that forms when magma hardens beneath Earth’s surface.

Page 36: Chapter 3 Earth’s Structure and Materials and a few Chapter 2

Convection Current The movement of a fluid caused by differences in

temperature, that transfers heat from one part of a fluid to another.

Page 37: Chapter 3 Earth’s Structure and Materials and a few Chapter 2

Sedimentary Rock

A type of rock that forms when particles from other rocks or the remains of plants and animals are pressed and cemented together.

Page 38: Chapter 3 Earth’s Structure and Materials and a few Chapter 2

Weathering

The chemical and physical processes that break down rock and other substances.

Page 39: Chapter 3 Earth’s Structure and Materials and a few Chapter 2

Rock fragments with rounded edges form this rock

CONGLOMERATE

Page 40: Chapter 3 Earth’s Structure and Materials and a few Chapter 2

ErosionThe process by which water, ice, wind, or gravity

moves weathered particles of rock and soil.

Page 41: Chapter 3 Earth’s Structure and Materials and a few Chapter 2

DepositionProcess in

which sediment is laid down in

new locations.

Page 42: Chapter 3 Earth’s Structure and Materials and a few Chapter 2

Formed in the ocean where many living things, such as coral, clam and oysters have hard shells made of the mineral calcite.

Limestone

Page 43: Chapter 3 Earth’s Structure and Materials and a few Chapter 2

Clastic Rock Sedimentary rock that forms when rock

fragments are squeezed together under high pressure.

Page 44: Chapter 3 Earth’s Structure and Materials and a few Chapter 2

Compaction

The process by which sediments are pressed together under their own weight

Page 45: Chapter 3 Earth’s Structure and Materials and a few Chapter 2

Foliated

Term used to describe metamorphic rocks that have grains arranged in parallel layers or bands.

Page 46: Chapter 3 Earth’s Structure and Materials and a few Chapter 2

Rock Cycle

A series of processes on the surface and inside the Earth that slowly changes rocks from one

kind to another.

Page 48: Chapter 3 Earth’s Structure and Materials and a few Chapter 2

Forms from tiny particles of clay and water deposits the clay in thin flat layers

SHALE

Page 49: Chapter 3 Earth’s Structure and Materials and a few Chapter 2

Cementation

The process by which dissolved

minerals crystallized and glue particles of

sediment together into one

mass.

Page 50: Chapter 3 Earth’s Structure and Materials and a few Chapter 2

Organic Rock

Sedimentary rock that form from

remains or organisms

deposited in thick layers.

Page 52: Chapter 3 Earth’s Structure and Materials and a few Chapter 2

Chemical Rock

Sedimentary rock that forms when minerals crystallize from a solution

Page 54: Chapter 3 Earth’s Structure and Materials and a few Chapter 2

Rock fragments with sharp edges form this rock.

BRECCIA