These are called Subduction zones.
An example of a transform (strike-slip) plate boundary is b) San Andreas fault.
I think that the answer is: Deep ocean water masses are classified based on flora's <span>calorific value.</span>
H=88 G=92 K=91 M=89
How you solve this is G is the same thing as 92 because it crosses each other same thing with K. Then after that you just subtract 180 by 92 to get H because the line angle equals to 180 same thing with M
