The answer is Pennsylvanian. I worked on this before. The Pennsylvanian era is a subperiod of the Carboniferous Period. i really hope this helps :)
Answer:
B. Heat absorption increases as the albedo decreases
Explanation:
The ice has very high albedo. The reason for this is that it has white coloration, and the light coloration are highly reflective of the sunlight. As the ice melts though, the water surface increases, and the water, unlike the ice, has the capability of absorbing much more heat. With much more water, there will be much more absorption of heat, and since the water has low albedo on only 10, the albedo will decrease on a global level.
Answer:
1. New Orleans
2. Cleveland
Gypsum is a chemical sedimentary rock.