Answer:
Following are the solution to this question:
Explanation:
Throughout layers called sheets or stratification were placed silicate minerals. Any formal credit with a uniform lithology or texture is defined as asleep. Beds are built on top of one another by deposition with disk diffusion.
Physical danger rocks characteristics:
- Bedding is also a sedimentary stone's most obvious feature. It comprises of language service as major corridors marking the boundaries of various layers of the earth.
- Grade grounds are popular when sediment does have a sluggish stream accumulated.
- Fossils, and Fractures and ripples of decomposition, etc.
Các mảng kiến tạo của Trái đất đập vào nhau. Bên dưới mặt đất, vỏ Trái đất được tạo thành từ nhiều mảng kiến tạo. ... Kết quả của việc các mảng kiến tạo này bị vỡ vụn là các phiến đá khổng lồ bị đẩy lên không trung.
When plate hit each other that cam make a earthquakes
Storms could be produced in the future as the hot air moving across the water could carry the water vapor high into the atmosphere. Humidity would also be lower than expected if the hot front wasn’t right along the water.
Alluvial fan could be the answer. Alluvial fans are cone shaped deposits of sedimentary particles. The particles can be sand. silt, gravel or clay. These land-forms are formed at the mouth of canyons or in valleys where ephemeral streams can occasionally transport material to the mouth of the canyons. An ephemeral stream is one that is created after a shower of rain or other form of precipitation; they are not permanent streams. <span />
