Chapter 5 Earth Science 7th Grade Flashcards

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1
Q

J. Tuzo Wilson

A

He observed that cracks in the continents are similar to those in the ocean floor.

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2
Q

Plates

A

Lithosphere is broken into separate sections. They fit together along cracks in the lithosphere. It carries continents or parts of the ocean floor.

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3
Q

Scientific Theory

A

It is a well tested concept that explains a wide range of observations.

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4
Q

Plate Tectonics

A

It states that pieces of Earth’s lithosphere is in slow constant motion, driven by the convection currents in the ocean. The theory explains the formation, movement, and subduction of Earth’s surface. Geologists think that movement of convection currents in the mantle is the major force that causes plate motion. As the plates move, they collide, pull apart, producing spectacular changes in the Earth’s surface.

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5
Q

Faults

A

It breaks in Earth’s crust where rocks have slipped past each other.

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6
Q

Divergent Boundaries

A

The place where 2 plates move apart from each other. It occurs on land. When it develops on land, 2 of Earth’s plates slide apart.

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7
Q

Rift Valley

A

It is a deep valley that forms along the divergent boundary.

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8
Q

Convergent Boundary

A

The place where 2 plates come together. The result is called a collision. When they collide the density of the plates determines which one is on top. The one that is more dense is the one that sinks.

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9
Q

Transform Boundary

A

The place where 2 plates lip past each other moving in opposite directions.

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10
Q

Plate Movements Over Time

A

Before Pangaea existed, other super continents formed and split apart over billions of years.

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11
Q

Plate Boundary

A

The line where the edges of Earth’s plates meet.

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12
Q

Mid-Ocean Ridge

A

It occurs between plates that are pulling apart. Undersea mountain chain where new ocean floor is, is produced.

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13
Q

Sonar

A

Device that bounces sound waves off underwater objects and then records echoes of those sound waves. Time it takes for the echo to arrive indicates distance to object.

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14
Q

Harry Hess

A

He is an american geologist that examined maps of the mid ocean ridge system. He made a conclusion that Wegener was right

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15
Q

Sea Floor Spreading

A

The sea floor spreads apart along both sides of the mid ocean ridge as new crust is added. The ocean floor is like a conveyor belt. It begins at mid ocean ridge forming a crack along the oceanic crust.

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16
Q

Alvin and Evidence from Molten Material

A

A small submarine, Alvin, was built to withstand the crushing pressures. The crew found strong rocks shaped like pillows. This type of form is only from when molten material hardens quickly after erupting under water.

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17
Q

Evidence from Magnetic Stripes

A

It is strips of magnetic iron that show how Earth’s poles have reversed themselves several times. It last happened 780,000 years ago. If suddenly reversed themselves, your compass needle would point south.

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18
Q

Evidence from Drilling Samples

A

Farther away from the mid ocean ridge the older the rocks were. The youngest rocks where in the center of the mid ocean ridge. This shows that sea floor spreading really has taken place.

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19
Q

Deep Ocean Trenches

A

The ocean floor plunges into deep underwater canyons. The ocean crust bends downwards.

20
Q

Subduction

A

The process of oceanic crust sinks beneath a deep ocean trench and back into the mantle at the convergent plate boundary. Sea floor spreading and subduction work together.

21
Q

How is heat transferred?

A

Heat is transferred from the movement of energy from one object to a cooler object.

22
Q

Radiation

A

The transfer of energy (heat) through open space.

23
Q

Conduction

A

It is the heat transfer within a material or between materials that are touching.

24
Q

Convection

A

It is the heat transfer by the movement of currents within a fluid (liquid or gas).

25
Q

Why does the density of a liquid or gas change with temperature?

A

The particles move faster and faster creating a heated gas or liquid. The density decreases. But when it cools, particles slow down making it cooler and closer together.

26
Q

What causes convection currents?

A

Heating and cooling of a gas or liquid, changes in the fluid’s density, and the force of gravity combines together to set convection currents in motion.

27
Q

What causes convection currents in Earth’s mantle?

A

Heat from the core and the mantle itself causes convection currents in the mantle.

28
Q

What did Alfred Wegener do?

A

He hypothesized that all the continents were once joined together in a single landmass and have since drifted apart.

29
Q

Continental Drift

A

It is continents moving slowly over Earth’s surface.

30
Q

Pangaea.

A

It means “all lands” and existed about 300 million years ago. The process slowly started moving to what we have today.

31
Q

Land Feature Evidence That Wegener Used To Support His Idea

A

He pieced together maps of South America and Africa. He noticed that mountain ranges matched up.

32
Q

Fossil Evidence That Wegener Used To Support His Idea

A

Glossopteris fossils were found in South America and Africa.

33
Q

Climate Evidence That Wegener Used To Support His Idea

A

The continents had close weather.

34
Q

Why was Wegener’s theory rejected most geologists of his time?

A

South Africa was once covered in continental glaciers. South Africa is supposedly known to be mild. Wegener said that South Africa was closer at one point in time. He couldn’t explain the force on how it happened. IT eventually became true.

35
Q

Evidence from Rock Samples

A

Rocks from inside Earth give geologists clues about Earth’s Structure. Geologists can make inferences about conditions deep inside Earth.

36
Q

Evidence from Seismic Waves

A

Geologists use an indirect method. When earthquakes occur, they produce seismic waves. Geologists record them and study how they travel through Earth. Earth’s interior is made up of several layers.

37
Q

Seismic Waves

A

Seismic Waves are vibrations that travel through Earth carrying the energy released during an earthquake.

38
Q

Temperature

A

The high temperatures inside Earth are the result of heat left over from the formation of Earth. In addition, radioactive substances inside Earth release energy.

39
Q

Pressure

A

It is the results from force pressing on an area.

40
Q

Earth’s Layers in Order

A
  1. Crust
  2. Lithosphere
  3. Asthenosphere
  4. Lower Mantle
  5. Outer Core
  6. Inner Core
41
Q

Crust

A

Hard and rigid, Earth’s outermost and thinnest layer, only a few miles thick under the ocean and averaging 20 miles thick under the continents. The layer of rock that forms outer skin. The layer of solid rock that includes dry land and ocean floor.

42
Q

Lithosphere

A

Uppermost part of the mantle. “Lithos” means stone in Greek. Made up of crust and a tiny bit of the upper mantle. This layer is divided into several constantly moving plates of solid rock that holds the continents and oceans.

43
Q

Asthenosphere

A

Plates of lithosphere move on this hot, malleable semi liquid zone in the upper mantle, directly underneath the lithosphere. It is a hot and under increasing pressure, less rigid, soft layer, “asthenes” means weak, and it is still a solid.

44
Q

Lower Mantle

A

It is solid, extends to the core, and is made up of the metals, iron and nickel.

45
Q

Outer Core

A

It is the layer of molten metal that surrounds the inner core. It is a liquid. The only liquid layer of the Earth. It is a sea of mostly iron and nickel.

46
Q

Inner Core.

A

It is a dense ball of solid metal. The intense pressure squeezes atoms of iron and nickel so much that they can not spread out and become a liquid. It is an extremely hot, solid sphere of mostly iron and nickel at the center of the Earth.