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Usimov [2.4K]
3 years ago
15

Global winds that blow in fairly constant patterns are called

Geography
1 answer:
Nimfa-mama [501]3 years ago
8 0

Answer: it will be called wind i think .

Explanation:

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Suitable for farming A mountain rang B rural C arable D smog
satela [25.4K]

depends on the plant, most likley C

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3 years ago
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Which items are examples of human-environmental interaction? road construction meteorites home building coal deposits gold mines
notsponge [240]

Answer:

road construction

home building

gold mines

Explanation:

Human-environmental interaction is an age-long process that connects human activities with the rest of the ecosystem. The ecosystem is made of all living and non-living components.

Activities of humans have telling consequences on the ecosystem. They are necessary and important for the survival of human life and their overall well being. Almost all activities of man is constantly geared at shaping the environment they live in.

Road construction involves interaction with the geosphere and other component of the biosphere.

Building of homes is very similar to the road construction.

A gold mine is a perfect example of human-environmental interaction.

4 0
3 years ago
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The appearance of hot spots and volcanoes at Earth's surface is evidence of
meriva

Answer:

Mantel-plumes.

Explanation:

Hope this helps :)

8 0
3 years ago
Can someone please help with these questions
never [62]

Answer:

A. Provided them with much of their food

7 0
3 years ago
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Why does sedimentation continue to fill the basins, albeit typically rather slowly, during the post-rift phase?
Bond [772]

Answer:

Subsidence is so slow that there seems to have been no depression of the upper surface of the lithosphere, so depositional environments are mostly the

same as those in surrounding areas; the succession is just thicker. These

successions are also more complete, however—there are fewer and smaller

diastems—so at times the basin must have remained under water while surrounding areas were emergent. (A diastem is a brief interruption in

sedimentation, with little or no erosion before sedimentation resumes.)

Size, shape: rounded, equidimensional, hundreds of kilometers across

Sediment fill: shallow-water cratonal sediments (carbonates, shales, sandstones),

thicker and more complete than in adjacent areas of the craton but still

relatively thin, hundreds of meters.

Hopefully that helps!

5 0
3 years ago
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