If many of the lakes in Florida are sinkhole lakes, what can you conclude about the geology beneath Florida's surface< Explain.

Answers

Answer 1

Answer: You can conclude that Florida lacks in bedrock because sinkholes form where there is low amount of such.

Related Questions

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List three examples of direct evidence of evolution.
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How does plate tectonics explain the creation of volcanic islands in the Pacific
Question 10Contact forces are forces acting upon two objects in contact. Which of the following does NOT represent a contact force?A.Pushing an object on the floor.B.Dropping a marble from the roofC.Kicking a soccer ball across a fieldD.The weight of a pen on a table

Which example provides scientific data about the earth's interior?A.
the motion of continents

B.
earth's orbit around the sun

C.
how seismic waves travel

D.
the size of volcanoes on the earth’s surface

Answers

The correct answer is C. How seismic waves travel

Explanation:

The Earth is composed of different layers that include the crust, the mantle, the outer core and the inner core, each of these layers and the features of them have been discovered throughout the years by topographers, and other experts mainly by studying seismic waves. This can be explained as seismic waves that occur due to earthquakes, eruptions, explosions and other phenomena, travel through the different layers of Earth and depending on which layer they are they display different features and speed which is the main information scientists used to determine the layers of Earth and other features of Earth's interior. Thus, it is how seismic waves travel the one that provides scientific data about the earth's interior.

how seismic waves travel are you from k12?

What general pattern of winds near the equator

Answers

The region of Earth receiving the Sun's direct rays is the equator. Here, air is heated and rises, leaving low pressure areas behind. Moving to about thirty degrees north and south of the equator, the warm air from the equator begins to cool and sink. Between thirty degrees latitude and the equator, most of the cooling sinking air moves back to the equator. The rest of the air flows toward the poles. The air movements toward the equator are called trade winds- warm, steady breezes that blow almost continuously. The Coriolis Effect makes the trade winds appear to be curving to the west, whether they are traveling to the equator from the south or north. The trade winds coming from the south and the north meet near the equator. These converging trade winds produce general upward winds as they are heated, so there are no steady surface winds. This area of calm is called the doldrums. Between thirty and sixty degrees latitude, the winds that move toward the poles appear to curve to the east. Because winds are named from the direction in which they originate, these winds are called prevailing westerlies. Prevailing westerlies in the Northern Hemisphere are responsible for many of the weather movements across the United States and Canada.(: hope i helped

In Iceland mid-Atlantic Ridge runs through the center of the country. What can you conclude about the appearance of Iceland many thousands of years from now

Answers

Iceland is a country that is located right above a mid-ocean ridge. This actually makes the country being divided in two parts geologically speaking, as the western half is part of the North American plate, while the eastern half is part of the Eurasian plate.

Iceland has formed because of intense volcanic activity at the mid-ocean ridge in the North Atlantic Ocean. As more and more magma has been propelled at the divergent boundary, the mid-ocean ridge has been growing in size, and over time it gradually became so high that it came out above the surface of the water.

The volcanic activity has continued, and it still is, and the volcanic eruptions constantly provide new lava flows, which create new crust, thus solidify the island and make it a long lasting one, not allowing the erosion to gradually level it and destroy it.

Answer:

hope this helps!

How is continental crust different from oceanic crust

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the oceanic crust is more dense compared to the continental crust.

Continental crust is the crust that moves the continents, and is less dense. Oceanic crust is the crust that contains oceans, and is more dense. With the O.C being less dense, if the two collide, the O.C will go under the C.C, forming a subduction zone.

poverty and lack of choices for alternative sources of income have led the porr t oexploit their environment to dangerous levels ture or false

Answers

true. look at africa.

Why don't the present shapes of the continents fit perfectly into a supercontinent?

Answers

The borders (coastlines) of the continents underwent a number of changes since the split. Often, chunks of land were washed away with water, slowly or in bigger portions. The coast was generally "smoothed" by the ocean currents too, and in some places more land was added with the material that the ocean currents brought.

Then, the tectonic plates continue to move, so this adds to the changes of the shape of the continents.

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Are African and Asian elephants endangered?

detemina cordonatele geografice ale punctului de confluenta a riurilor tigru si eufrat va rog frumos repede si corect va dau 20 de puncte