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Flauer [41]
3 years ago
15

Which is one characteristic of deep ocean currents?

Biology
2 answers:
Hatshy [7]3 years ago
7 0

Answer: Deep ocean currents are affected by temperature but not by salinity.

Explanation: I think it's this because I know it takes a while for deep ocean currents to move so it isn't the first one.

k0ka [10]3 years ago
6 0

Answer:

D

Explanation: Took the test review and test for edg

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What are some examples of Homeostasis in humans?
masha68 [24]
Humans' internal body temperature is a great example of homeostasis. When an individual is healthy, his or her body temperature retains a temperature 98.6 degrees Fahrenheit. The body can control temperature by making or releasing heat.
7 0
3 years ago
Larger the size of an organism bigger the size of its cells. Do you agree with this statement? Give scientific reasons.
vodomira [7]

Answer:

Disagree.

Explanation:

Though some cells are bigger than others, they do not scale with size. For example if you look at skin cells on a dog they would be similar in size to a skin cell from a human. When an animal or species is bigger it is usually just made from more cells.

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how does aerobic and anaerobic respiration work together to provide a continuos work together to provide a continuous supply of
svetoff [14.1K]
Aerobic and anaerobic respiration each have advantages under specific conditions. Aerobic respiration produces far more ATP, but risks exposure to oxygen toxicity. Anaerobic respiration is less energy-efficient, but allows survival in habitats which lack oxygen.
Within the human body, both aerobic and anaerobic respiration are important.
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3 years ago
What processes turn atmospheres into clouds
bulgar [2K]

Answer:

am sorry I don't know this

5 0
3 years ago
_______________ refers to the tendency of a foundation material (such as soil) that is water-logged to lose its internal cohesio
dybincka [34]

Answer:

<u>Liquefaction</u> refers to the tendency of a foundation material (such as soil) that is water-logged to lose its internal cohesion and mechanically fail to provide support during earthquake shaking.

Explanation:

Liquefaction occurs when an unbound material (usually sand), which is saturated in water, loses its resistance to shear due to intense and rapid vibration (earthquake), which breaks its granular structure by reducing its inter-granular pressure and flow like a liquid because of an increase in pressure.

Liquefaction usually manifests itself in loose, saturated and non-cohesive soils, formed by young deposits of sands and sediments of similar particle sizes. If the soil is dense there will be less chances of liquefaction. Older deposits, in general, are more dense and cohesive. At higher density, more interstitial pressure is needed for liquefaction to occur.

8 0
3 years ago
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