Answer:
i.
The passive continental margins are formed under divergent plate boundary setting. These are aseismic (less seismic) and often referred as the Atlantic-type margins having a distinct transition zone between the continental and oceanic crustal regions.
ii.
The active continental margins referred as the Pacific-type margins are the zones of seismically active convergent plate boundaries. These are characterized by subduction zones formed under variety of settings such as oceanic–oceanic, oceanic–continental, etc. and are mostly observed along the periphery of the Pacific Ocean.
iii.
Transform continental margins (sheared margins) are formed due to lateral plate movements or shearing motions during the continental breakup process in the divergent margin setting. Identifying this category of margins is also in a way important, as they represent an original offset in the line of continental breakup and can normally be traced laterally into an oceanic fracture zone (Bird, 2001). Further, transform margins are also noticed along the Pacific type continental margins.
Explanation:
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The answer is D, 5 degrees south, 15 degrees east.
That is because South Africa is mostly found on plateaus which means that the higher you go the colder it becomes. What this means is that during colder months, there will be many low temperatures because of the benguela currents and the differences in height.
Answer:
Facts are true statements that do not respond to our feelings and thoughts.
Opinions are our personal beliefs that do not need to be true in order for us to have them.
For example, a fact would be that the Earth is round and almost nothing can change that truth.
An opinion would be that cats are better than dogs because you like cats more.
Answer:
thicker
Explanation:
The continental crust is thicker and less dense than oceanic crust
