Answer:
The eroded rock and soil materials that are transported downstream by a river are called its load. A river transports, or carries, its load in three different ways: in solution, in suspension, and in its bed load. Mineral matter that has been dissolved from bedrock is carried in solution.
Explanation:
Hydro-Water
Atomos-Gas
Litho-Ground
Id say one of the negative affects is how cold it is in a tundra biome so its harder to get food and overall harder to survive
The correct answer is that a neuron's nucleus is located in its cell body also known as the soma. The cell body of a neuron is not indifferent with cell bodies of other cells of the body, it also contains organelles such as the mitochondria and endoplasmic reticulum. The cell body also houses the neuron's nucleus which is where the genetic material of the cell is stored.
<em>The axon is a part of a neuron that propels the signals away from the cell body. The dendrites are parts of a neuron that receives signals from another neuron and propels the signal towards the cell body. Synaptic terminals are structures where the axon of a presynaptic neuron meet the dendrites of a postsynaptic neuron.</em>
Most people know that it is colder on top of a mountain compared to the ground, but few actually know why. And even less know that the atmosphere actually warms up again! The true temperature profile of the atmosphere is shown in the image.
The air at the surface up to around 10 kilometers is called the troposphere. The reason it is warmer at the surface is simple. The air is warmed by heat given off by the Earth! The farther away from the surface the air moves, the less heat there is to absorb.
From 10 to 20 kilometers the atmosphere is stable. This region is called the tropopause. From 20 to about 50 kilometers is the stratosphere. In this region the air actually warms with height! Ozone is concentrated in this part of the atmosphere and it absorbs ultraviolet light from the Sun. More light is absorbed at higher altitudes compared to the lower stratosphere, so the temperature increases.
But at 50 kilometers, the temperature levels out again in a region called the stratopause. At about 55 km, the mesosphere begins. In the mesosphere, the temperature decreases with height again, because there is very little ozone to warm up the air.
Finally, the mesopause divides the mesosphere from the thermosphere, which is the section of the atmosphere higher than 90 km. In this region, the temperature increases again! This time, it is molecular oxygen (O2) that causes the temperature increase. The oxygen absorbs light from the Sun, and since there is very little air in the thermosphere, just a little absorption can go a long way!