Answer:
The answer is Batholithic intrusions
Explanation:
The Half Dome is an isolated mass suspended within the batholithic intrusions. Developed due to vertical jointing, exfoliation, and some glacial activity. Steep face of half dome began to take shape as thin slabs of rock b/w parallel vertical joints were loosened by weathering and mass wasting and fell away layer by layer. Tenaya Glacier cleared away exfoliation debris and talus flowing in direction parallel to trend of vertical joints, removed sheets of rock by plucking . Rounded back of Half Dome formed as curved shells of rock exfoliated
Answer D I believe! Have a nice day
Answer:
No.
Explanation:
Because it is something that I don't want to learn a lot about.
The answer should be ''The law of the conservation of energy''.
Answer:
The epicenter might be located near the Tennessee-Missouri-Kentucky (TN-MO-KY) tristate area.
