Usually it is fresh. There are exceptions: The Dead Sea (37% salinity) is so salty barely lives in it and the Salt lake near Salt Lake City is so salty people can easily and comfortably float in it.
<span>The answer is all of the above;
Volcanic eruptions can cause debris to flows and make earthquakes happen because of the instability it can bring to the land during lava flow. Lava can also carry some objects to different places.
Another result would be floods and landslides. Volcanic eruptions can pull out trees and plants that can cause erosion and floods. There would be insufficient plants left to consume water from heavy rains. Lava can also cause wildfires in forests.
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Aqua man's mother and father
Answer:
The absolute best time to view the Moon is a few days after the first quarter.
Explanation:
This is exactly when half the moon is lit. At this phase it is perfectly positioned in the night sky and there is enough light to reveal an astonishing amount of detail.
Answer:
A mid-ocean ridge (MOR) is a seafloor mountain system formed by plate tectonics. It typically has a depth of about 2,600 meters (8,500 ft) and rises about 2,000 meters (6,600 ft) above the deepest portion of an ocean basin. This feature is where seafloor spreading takes place along a divergent plate boundary. The rate of seafloor spreading determines the morphology of the crest of the mid-ocean ridge and its width in an ocean basin. The production of new seafloor and oceanic lithosphere results from mantle upwelling in response to plate separation. The melt rises as magma at the linear weakness between the separating plates, and emerges as lava, creating new oceanic crust and lithosphere upon cooling. The first discovered mid-ocean ridge was the Mid-Atlantic Ridge, which is a spreading center that bisects the North and South Atlantic basins; hence the origin of the name 'mid-ocean ridge'. Most oceanic spreading centers are not in the middle of their hosting ocean basis but regardless, are traditionally called mid-ocean ridges. Mid-ocean ridges around the globe are linked by plate tectonic boundaries and the trace of the ridges across the ocean floor appears similar to the seam of a baseball. The mid-ocean ridge system thus is the longest mountain range on Earth, reaching about 65,000 km (40,000 mi).
