Answer:
The Goode homolosine projection (or interrupted Goode homolosine projection) is a pseudocylindrical, equal-area, composite map projection used for world maps. Normally it is presented with multiple interruptions. Its equal-area property makes it useful for presenting spatial distribution of phenomena.
Explanation:
The Goode homolosine projection (or interrupted Goode homolosine projection) is a pseudocylindrical, equal-area, composite map projection used for world maps. Normally it is presented with multiple interruptions. Its equal-area property makes it useful for presenting spatial distribution of phenomena.
I think it's B but I'm not to sure. hope that at least kinda helps.
Answer:
c. The oldest rocks are along a fault line
Explanation:
- As geology, the fault lines are the lines of displacement of rocks where the volume of rocks gets significantly displaced such as the subduction zones. Where the younger rocks are found at the surfaces and the older rocks are formed at the depths of the earth.
- They are also formed where the magma rise and they are of various types as the normal, reverse and the slip strike faults.
Step 1: Identify the decision. You realize that you need to make a decision. ...
Step 2: Gather relevant information. ...
Step 3: Identify the alternatives. ...
Step 4: Weigh the evidence. ...
Step 5: Choose among alternatives. ...
Step 6: Take action. ...
Step 7: Review your decision & its consequences.
