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levacccp [35]
3 years ago
14

Between what depths does Earth's temperature increase the slowest?

Geography
1 answer:
Eddi Din [679]3 years ago
6 0
Pressure and temperature change inside earth as depth increases when <span>both temperature and pressure increase as you go down inside earth. Thank you for posting your question here at brainly. I hope the answer helps. </span>
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I believe the answer is True
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The asteroid belt separates the inner planets from the outer planets.<br> True<br> False
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Choose a landmark that was built in the last 250 years, such as Mount Rushmore, the Eiffel Tower, or the Statue of Liberty. How
Katen [24]

Answer:

<u>Past is key to future and landmarks are ket sign and indicators.</u>

Explanation:

  • Many landmarks have been built in the history of the earth such as the Mount Rushmore, Eiffel Tower, Statue of Liberty and many more the Burj Khalifa, and Berlin wall.  
  • Their basic construct was to put represent civilization like it's in Brazil statue of christ redeemer is know for peace and landmark of Stonehenge on easter island. It depicts a civilization's history and past experiences.
  • landmarks as a way of identifying the place with some characteristics that the place has to offer to the future generation so as they can understand and learn from them. They are marked on the history of the earth's surface.  
  • Some are known for sacrifice, some for rituals, some for freedom and others to represent the amount of power or dominance.
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3 years ago
Compare the natural conditions for the development of agriculture in Denmark and Hungary.​
beks73 [17]
I’m not sure. What story is that?
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3 years ago
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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