Earthquakes are very common along transform boundaries. An example of a transform boundary is the San Andreas fault in California.
Bedrock structure and elevation
convergence plate boundary, where tectonic plates move towards each other and collide, leading to subduction zones which are highly constructive regions of volcanoes. Volcanoes also form at divergent plate boundaries. A good example being the numerous Icelandic volcanoes which have formed over he Mid Atlantic Ridge.
Convergent plate boundaries.
a imaginary line between regions
mountain areas: terrorist attacks avalanche landslides.plateau areas:cyclones, typhoons thunder storms, earthquake cyclones
Neighborhood adjacency cnnectivity paths regions and boundaries
regions don't have defined boundaries
Bedrock structure and elevation
Deserts receives less percipitation than Semiarid regions.
western
Deserts receive less precipitation than semiarid regions.
opinions about regions
People living in earthquake regions should prepare with emergency kits because an earthquake may happen at anytime.
Hot spots are unusually hot regions far from plate boundaries. The high temperature plumes melt rocks, magma rises, and melts through the Earth's crust, forming volcanoes, and thus creating volcanism.
Earthquake-Hazard Levels are the likeliness of earthquakes occurring in certain regions.
Earthquake-Hazard Levels are the likeliness of earthquakes occurring in certain regions.
There are a few different ways that regions are formed. Regions are formed based on boundaries that are placed based on population for example.