1. continental slope 2. salinity 3. ozone 4. nuclear 5. nonrenwable

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1. Continental Slope 2. Salinity 3. Ozone 4. Nuclear 5. Nonrenwable

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Page 1: 1. Continental Slope 2. Salinity 3. Ozone 4. Nuclear 5. Nonrenwable

1. Continental Slope

2. Salinity

3. Ozone

4. Nuclear

5. Nonrenwable

Page 2: 1. Continental Slope 2. Salinity 3. Ozone 4. Nuclear 5. Nonrenwable

Do Now 1. _____type of energy that uses heat from

fission reactions (alternative energy)

2. _____type of resource coal, natural gas, and petroleum(natural resources)

3. _____extends from the continental shelf and slopes steeply (ocean floor)

4._____second smallest ocean (oceans)

5. _____ layer of gases that protect the Earth from ultraviolet radiation (air pollution)

Page 3: 1. Continental Slope 2. Salinity 3. Ozone 4. Nuclear 5. Nonrenwable

Do Now 1. _____type of energy produced

from heat inside the earth (alternative energy)

2. _____type of resource soil, food crops, and animals (natural resources)

3. _____plowing fields in curves

4._____smallest ocean (oceans)

5. _____ the amount of salt in the ocean (oceans)

Page 4: 1. Continental Slope 2. Salinity 3. Ozone 4. Nuclear 5. Nonrenwable

Do Now 1. _____type of energy that changes heat

to steam by nuclear fission (alternative energy)

2. _____type of resource coal, natural gas, and petroleum (natural resources)

3. _____anchor soil to prevent erosion (human impact)

4._____second largest ocean (oceans)

5. _____ starts from the continents and slopes gently (ocean floor)

Page 5: 1. Continental Slope 2. Salinity 3. Ozone 4. Nuclear 5. Nonrenwable
Page 6: 1. Continental Slope 2. Salinity 3. Ozone 4. Nuclear 5. Nonrenwable

1. What is topography of the ocean?

1. Topography-the surface features of the ocean floor.

Page 7: 1. Continental Slope 2. Salinity 3. Ozone 4. Nuclear 5. Nonrenwable

2. FeaturesA. Continental Shelf

-Slopes gently down from the edge of a continent

Page 8: 1. Continental Slope 2. Salinity 3. Ozone 4. Nuclear 5. Nonrenwable

b. Continental Slope

Slopes steeply from the continental shelf

Page 9: 1. Continental Slope 2. Salinity 3. Ozone 4. Nuclear 5. Nonrenwable

It is the base of the continental slope and is made of large piles of sediment.

C. Continental Rise

Page 10: 1. Continental Slope 2. Salinity 3. Ozone 4. Nuclear 5. Nonrenwable

D. Submarine Canyon

Steep V shaped canyon that cuts through the continental shelf and continental slope

Page 11: 1. Continental Slope 2. Salinity 3. Ozone 4. Nuclear 5. Nonrenwable

E. Abyssal Plain

Flat ocean bottom covered with mud and the remains of marine organisms

Page 12: 1. Continental Slope 2. Salinity 3. Ozone 4. Nuclear 5. Nonrenwable

F. Seamount Steep walled, pointy, extinct volcano

The seamount’s shown here can reach up to just under 600 ft. of the surface. They are located off the coast of Alaska.

Page 13: 1. Continental Slope 2. Salinity 3. Ozone 4. Nuclear 5. Nonrenwable

G. Guyot

Flat topped seamount flattened by the action of waves

Page 14: 1. Continental Slope 2. Salinity 3. Ozone 4. Nuclear 5. Nonrenwable

H. Mid-Ocean Ridge

Longest Undersea mountain range Occurs at divergent boundaries

Page 15: 1. Continental Slope 2. Salinity 3. Ozone 4. Nuclear 5. Nonrenwable

Oceanic Ridges

Page 16: 1. Continental Slope 2. Salinity 3. Ozone 4. Nuclear 5. Nonrenwable

I. Rift Valley

Deep valley that forms between the mountains of a mid-ocean ridge

Page 17: 1. Continental Slope 2. Salinity 3. Ozone 4. Nuclear 5. Nonrenwable

J. Trench Steep sided narrow cut in the sea floor Deepest part of the ocean (Mariana Trench) Formed from convergent plate boundaries