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Nataliya [291]
2 years ago
11

Sandstone, limestone, and conglomerate cobbles are found in a streambed in New York State where the surrounding bedrock is compo

sed of shales and siltstones. The most likely explanation for the presence of these cobbles is that they were
weathered from the surrounding bedrock

formed when shale and siltstone bedrock were eroded

transported to this area from another region

metamorphosed from shale and siltstone
Geography
1 answer:
Grace [21]2 years ago
8 0

Answer: transported to this area from another region

Explanation:

The surrounding area is made of shale and siltstones so the sandstone and limestone could not have formed in that area because they have different structures.

The sandstone and limestone as well as the conglomerate cobbles must therefore have been transported to this streambed from another area where they are able to form. They probably got to this area as a result of water erosion.

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Answer:

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3 years ago
What was most likely caused a change in the soil in the wheat field shown?
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Answer:

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2 years ago
A cone has a diameter of 6 centimeters and a height that is 5 times the diameter. Using 3.14 for pi, which of the following can
MariettaO [177]
The volume of the cone is calculated by the formula:

V = B*H/3
r=D/2 = 6/3 = 2
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8 0
3 years ago
Which European countries’ colonial possessions prevented the British from controlling the entire east coast of Africa from the G
Elanso [62]

Answer:

Italy and Portugal

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4 0
3 years ago
Why is weathering described as a passive or inactive agent of landform development?
Leona [35]
Weathering is described as a passive agent of landform development because it is not directly affecting it.
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2 years ago
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