3. The soil erosion pictured here is the result of what?A. The transition between geologic eras and eons
B. Harvesting renewable resources at a rate greater than the sustainable yield
C. Harvesting renewable resources at a rate lower than the sustainable yield
D. A mudslide caused by excessive rains
3. The soil erosion pictured here is the result of - 1

Answers

Answer 1
Answer:

Answer:

B. Harvesting renewable resources at a rate greater than the sustainable yield

Explanation:

Answer 2
Answer:

Answer:

i believe it is b but the answer can also be d , its hard to tell because its a picture of a screen..


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Why it is difficult to breathe in sandstorm in UAE?​

Answers

Answer:

It's because you are breathing in dust particles, and sand particles that will make it harder to breath.

Explanation:

"Sandstorms contain sand and dust particles and when you're in one you will be breathing in those sand and dust particles" which is putting the particles in your nostrils and lungs which will make it harder to breath. The consequences of breathing in these particles will strengthen if you already have problems with breathing.

Hope this helps.

What were some of the problems with ancient maps?

Answers

Some of them were very hard to read and not quite right. Now a days they are a lot better
They weren't as accurate as they could be, in fact some were just based off of educated guesses.

Which evolved during the paleozoic era?

Answers

Fish, Arthropods, Amphibians, and Reptiles all evolved during the Paleozoic Era.

Hope this Helps!

Online exhibits : Geologic time scaleThe Paleozoic EraThe Paleozoic is bracketed by two of the most important events in the history of animal life. At its beginning, multicelled animals underwent a dramatic "explosion" in diversity, and almost all living animal phyla appeared within a few millions of years. At the other end of the Paleozoic, the largest mass extinction in history wiped out approximately 90% of all marine animal species. The causes of both these events are still not fully understood and the subject of much research and controversy. Roughly halfway in between, animals, fungi, and plants colonized the land, the insects took to the air, and the limestone shown in the photo at right was deposited near Burlington, Missouri.The Paleozoic took up over half — approximately 300 million years (542 mya to 251 mya)* — of the Phanerozoic. During the Paleozoic there were six major continental land masses; each of these consisted of different parts of the modern continents. For instance, at the beginning of the Paleozoic, today's western coast of North America ran east-west along the equator, while Africa was at the South Pole. These Paleozoic continents experienced tremendous mountain building along their margins, and numerous incursions and retreats of shallow seas across their interiors. Large limestone outcrops, like the one pictured here, are evidence of these periodic incursions of continental seas. The Paleozoic Era is bracketed by the times of global super-continents. The era opened with the breakup of the world-continent Pannotia and closed with the formation of Pangea, as the Earth's continents came together once again.Many Paleozoic rocks are economically important. For example, much of the limestone quarried for building and industrial purposes, as well as the coal deposits of western Europe and the eastern United States, were formed during the Paleozoic.The Paleozoic is divided into six periods: the Cambrian, Ordovician, Silurian, Devonian, Carboniferous (in the U.S., this is divided into the Mississippian and Pennsylvanian Periods), and Permian. Most of these names derive from locations where rocks of these ages were first studied. Cambria was the Latin name for Wales, and the Ordovices and Silures were two Welsh Celtic tribes. The Devonian is named for Devonshire, England. The Mississippian is named for the upper Mississippi River valley, not the state of Mississippi, which has very few rocks of this age; however, the Pennsylvanian is named for the state of Pennsylvania. The Permian was described from rocks in the region of Perm, a town in the Ural Mountains of Russia. The exception to this naming convention is the Carboniferous; its name means "coal-bearing," and this is a time when extensive coal beds were formed around the world

Explain sea breeze , and land breeze and the direction they blow RELATED TO AIR PRESSURE.

Answers

A sea breeze describes a wind that blows from the ocean inland towards land. This breeze occurs most often in the spring and summer months because of the greater temperature differences between the ocean and nearby land, particularly in the afternoon when the land is at maximum heating from the sun
Well sea brezze is from the ocean and lad brezze is mostly from wind and and air pressure is the high winds

How does a surface ocean current compare to a deep one? A. same density, but warmer and saltier B. same temperature, but saltier and less dense C. warmer, saltier, and denser D. warmer, less salty, and less dense

Answers

I can say it's A, I am 100% sure
D is your answer i belive ! :)

I need help please????

Answers

If Global Warming Shuts Down The Thermohline Circulation In The North Atlantic Ocean, The Result Could Be Catastrophic Climate Change. The Environmental Effects Depend Upon Whether The Shutdown Is Reversible Or Irreversible.