Answer:
I think its an opinion question. Look at a map of Canada and find a town or something that sounds interesting and do some research on it
Normal fault - a dip-slip fault in which the block above the fault has moved downward relative to the block below. This type of faulting occurs in response to extension and is often observed in the Western United States Basin and Range Province and along oceanic ridge systems.
Normal Fault Animation
thrust fault - a dip-slip fault in which the upper block, above the fault plane, moves up and over the lower block. This type of faulting is common in areas of compression, such as regions where one plate is being subducted under another as in Japan. When the dip angle is shallow, a reverse fault is often described as a thrust fault.
Thrust Fault Animation
Blind Thrust Fault Animation
strike-slip fault - a fault on which the two blocks slide past one another. The San Andreas Fault is an example of a right lateral fault.
Strike-slip Fault Animation
A left-lateral strike-slip fault is one on which the displacement of the far block is to the left when viewed from either side.
A right-lateral strike-slip fault is one on which the displacement of the far block is to the right when viewed from either side.
The spirits of the ancestors, animal spirits too
Headlands are known as high attacking waves, shores
that are rocky, forceful erosion and vertical sea cliffs. They are created when
the sea outbreaks on a coastline comprising of a group of hard and soft rocks. They
are surrounded by water.
<span>Bays on the other hand, are created when there is
less resistance of eroding soft rocks (e.g. sands and clays) forming a group of
stronger rocks (e.g. granite, chalk, limestone) into a headland. They are
surrounded by a land.</span>
