The landforms in the interior of the continents and at their margins mostly differ because of the difference in geological activity.
Explanation:
The landforms that are found in the interior of the continents tend to be old. They also are mostly consisted of sedimentary and metamorphic rocks. In general the erosion is much more evident and dominant, thus the landforms also are with lower elevations when compared with the ones on the edges. This is due to the lack of geological activity as the interiors of the continents tend to be far away from the plate boundaries.
The landforms on the edges of the continents tend to be younger in general. The reason for that are the subduction zones and intense geological activity. The intense geological activity is due to the close proximity of the plate boundaries. The landforms tend to be higher in general, and volcanic arcs are also a common sight.
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It would probably be hail since big blocks of ice could easily break the power lines
This isn't really a fair question. Everyone has some similar characteristics to others. Area doesn't matter except there traditions may be different.
Answer: The fluxes in hydrologic cycle does not include Fixation
Explanation: Hydrologic cycle is also known as the water cycle. It is the continuous movement of water on, below and above the earth's surface.
Fluxes in the hydrologic cycle simply mean how water moves in and out of the earth's surface.
The fluxes include;
- Infiltration: movement of water into the ground from the surface.
- Evaporation: This is the change of water from a liquid to a gas.
- Transpiration: This is the evaporation of liquid water from plants and trees into the Earth’s atmosphere.
- Uptake: This is the water taken from the groundwater flow and soil moisture.
