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Gnom [1K]
3 years ago
5

What kind of soil is found in the c horizon of a soil profile

Geography
2 answers:
ASHA 777 [7]3 years ago
7 0
The types<span> of mineral matter </span>found<span> in </span>soil<span> are: organic material, inorganic material, parent material, ... All the </span>horizons<span> and layers (A, B, </span>C<span>) make up </span>soil profile<span>.</span>
viva [34]3 years ago
3 0
<span>The C horizon is at the bottom of soil profile. It consists of partially weathered rock. It doesn't contain much organic material and leaching doesn't occur to this point. The C horizon is the layer in soil profile that best describes parent material.</span><span />
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The spectrum of a blackbody has a peak wavelength of 2.80×10-7 meters. What is its temperature, in kelvins?
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Answer: 1.03\times 10^4K

Explanation:

Using Weins displacement law:

\lambda _{max}=\frac{b}{T}

where \lambda _{max} = wavelength  = 2.80\times 10^{-7}m

b = constant =2.897\times 10^{-3}mK

T = Temperature in Kelvin = ?

Putting the values we get:

2.80\times 10^{-7}m=\frac{2.897\times 10^{-3}mK}{T}

T=1.03\times 10^4K

Thus the temperature of the blackbody will be 1.03\times 10^4K

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Mt. redoubt’s seismic activity is due to the interaction of which two tectonic plates
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Answer:

Correct answer is: Due to interaction between Pacific and North American plate.

Explanation:

Mountain Redoubt is located in south Alaska. Mentioned mountain is in the vicinity of convergent plate boundary between North American and Pacific plate.

Convergent boundary means that those plates are <em>colliding</em>. One plate always slides beneath another, and in this case Pacific plate slides beneath North American. Area of collision is known as subduction zone.

Pacific plate is oceanic plate, and North American is continental plate. Oceanic plates <u>always slides</u> beneath continental ones. Reason for that is due to their density. Oceanic plates are denser, so they go under continental ones.

Pacific and North American plate interaction is typicall oceanic-continetal boundary where <em>earthquakes</em> (seismic activity) and <em>active volcanoes</em> are common. Some of the strongest earthquakes happened in this area. That was in 1964 in Prince William Sound in the south coast of Alaska. Magnitude was 9.2M, second strongest quake ever recorded in world's history.

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