usually you find most of the zones of earthquakes and volcanoes at a plate boundary.
All three type of Earthquakes (Shallow-seated, Medium-seated and Deep-seated) occur only at the Convergent plate boundary. At divergent plate boundary we find mostly Shallow-seated Earthquakes only.
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.
Poseidōn is the God of the Seas and of Earthquakes.
The most deep focused earthquakes would be found at transform boundaries. The shallow focused earthquakes would be found at Divergent boundaries. And the intermediate focused earthquakes would be found at Convergent boundaries. By: A ninth grader.
At a convergent boundary, landforms such as mountains, deep ocean trenches, and volcanic arcs can be found. Tectonic activity includes the subduction of one plate under another, leading to the formation of these features. Earthquakes and volcanic eruptions are also common at convergent boundaries.
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.
I don´t know
You can find it on a convergent boundary
In statistics the class boundaries are numbers that separate classes without forming gaps. To find the lower, you subtract 0.5 and to find the upper, you add 0.5. If the class is 3-7 the lower class boundary would be 2.5 and the upper 7.5. The upper boundary of one class will equal the lower boundary of the next class.
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.
You would find a fault line at a transform plate boundary, where tectonic plates slide past each other horizontally. This movement can cause earthquakes due to the buildup and release of stress along the fault line.