At a transform fault boundary, you would find a strike-slip fault. This type of fault is characterized by horizontal motion where two tectonic plates slide past each other. Earthquakes are commonly associated with transform fault boundaries due to the friction caused by the plates' movement.
You would be most likely to find a boundary between a continental and an oceanic plate along a convergent boundary, where the denser oceanic plate subducts beneath the less dense continental plate. This often leads to the formation of deep-sea trenches and volcanic activity.
You would most likely find a boundary between a continental and an oceanic plate at a convergent plate boundary, where the two types of plates collide. In this setting, the denser oceanic plate is typically subducted beneath the lighter continental plate, leading to geological features such as deep ocean trenches and volcanic mountain ranges. This interaction can also result in significant seismic activity.
A destructive plate boundary (WITH a subduction zone!)
Divergent plate boundaries are moving apart so you would expect normal faults to form. Where these have significance on a regional scale they are known as detachment faults. It is also common to find transform faults running at right angles to divergent boundaries that cause offsets in the boundary along its length. Please see the related links for more information.
Along a convergent plate boundary, you typically find a reverse fault or thrust fault. This type of fault occurs when the two tectonic plates are pushing against each other, causing one plate to be forced up and over the other plate. This movement can lead to earthquakes and mountain building.
In an ideal world this would be a margin that involves some element of compression, so you're looking at a compressional (orogenic) or subducting margin. Anywhere where the crust is thickened generally involves reverse, also known as thrust, faulting.
You would most likely find a reverse fault at a convergent tectonic boundary, where two tectonic plates are colliding and one plate is being forced up and over the other. Reverse faults are characterized by vertical displacement and compression.
You can find it on a convergent boundary
The plate boundary along the west coast of the US is a transform boundary where the Pacific Plate slides past the North American Plate. This boundary is characterized by the San Andreas Fault system, which is slowly moving as the plates grind past each other. Over time, this movement can cause earthquakes and shift the landscape along the boundary.
At a transform fault boundary, you would find a strike-slip fault. This type of fault is characterized by horizontal motion where two tectonic plates slide past each other. Earthquakes are commonly associated with transform fault boundaries due to the friction caused by the plates' movement.
I don´t know
You would be most likely to find a boundary between a continental and an oceanic plate along a convergent boundary, where the denser oceanic plate subducts beneath the less dense continental plate. This often leads to the formation of deep-sea trenches and volcanic activity.
You would most likely find a boundary between a continental and an oceanic plate at a convergent plate boundary, where the two types of plates collide. In this setting, the denser oceanic plate is typically subducted beneath the lighter continental plate, leading to geological features such as deep ocean trenches and volcanic mountain ranges. This interaction can also result in significant seismic activity.
A destructive plate boundary (WITH a subduction zone!)
Off the westcoast of North America
Divergent plate boundaries are moving apart so you would expect normal faults to form. Where these have significance on a regional scale they are known as detachment faults. It is also common to find transform faults running at right angles to divergent boundaries that cause offsets in the boundary along its length. Please see the related links for more information.