Answer: The Turquoise Lake as seen nowadays in Colorado is a result of the 1850´s modern warming climate transition, lingering away from the Little Ice Age times occurred 500 years ago. This given period was characterized by snow blowing winds that accumulated ice through thermal compaction, generating the glaciers as we see them.
Explanation: Terminal and recessional moraines are the terminus of a glacial feature. Moraines are the sedimentar charges carried by melted glacials. Consequence of those is the repositioning of the snow downwards the valleys. The ice, initially attached to the glaciers and mountain tops, undergoes melting by seasonal and/or climate transition warming, resulting on circumstancial water deposits that place on the basin/lower areas of the mountain chains, forming lakes.
Answer:
Siltation is a process by which water becomes dirty as a result of fine mineral particles in the water. Explanation: When sediment, or silt, is suspended in water, this is an example of siltation.
Answer:
Explanation:
One of the first scenario is that the rock might not contain minerals that would result in the formation of foliations and lineations in the rock.
The bulk of a rock fabric depends on mineral orientations and their unique properties. This is why platy minerals play very important roles in defining the fabric of a rock.
Another scenario is that, the rock might have exceeded the extreme of metamorphism where melting is approached. All fabrics will eventually fan out and be destroyed.
The Mississippi-Missouri-Ohio river system is the largest and most significant river system in the world.
