it takes a pee
Plate boundaries are associated with geological events such as earthquakes and creation of topographic features like the mountains, volcanoes, mid-ocean ridges, and oceanic trenches.
Three types of plate boundaries are spreading boundaries, colliding boundaries, and sliding boundaries. um actually they are divergent, convergent, and transform
There are three kinds of plate boundaries:spreading boundaries, colliding boundaries, and sliding boundaries. The platea move at amazing show rates, from about 1 to 24 centimeters per year. Thet have been moving for tens of millions of years.
There are three kinds of plate boundaries:spreading boundaries, colliding boundaries, and sliding boundaries. The platea move at amazing show rates, from about 1 to 24 centimeters per year. Thet have been moving for tens of millions of years.
Three types of plate boundaries are spreading boundaries, colliding boundaries, and sliding boundaries. um actually they are divergent, convergent, and transform
There are three kinds of plate boundaries:spreading boundaries, colliding boundaries, and sliding boundaries. The platea move at amazing show rates, from about 1 to 24 centimeters per year. Thet have been moving for tens of millions of years.
Earthquake normally happen at or near the boundaries of tectonic plates. Particularly those where two plates are sliding past each other (a transform boundary) or are colliding (a convergent boundary). They can also occur away from the boundaries of tectonic plates but these tend to be far rarer and of much smaller magnitude.
Collision boundaries form at tectonic plate boundaries where two plates are either converging, diverging, or sliding past each other. These boundaries are categorized as convergent boundaries, divergent boundaries, and transform boundaries, respectively.
Most earthquakes happen at the edge of tectonic plates, where the plates are colliding or sliding past each other. These areas are known as plate boundaries, and the stress and friction from the movement of the plates can lead to earthquakes.
Convergent, Divergent, and Transform also known as Spreading, Colliding, and Sliding
Forms when two lithosperic plates slide past eachother or when my mom dies
Transform plate boundaries are often described as horizontal sliding because the tectonic plates move laterally past each other rather than colliding or pulling apart. This lateral movement occurs along faults, where the stress from the sliding motion can lead to earthquakes. The plates do not create or destroy crust at these boundaries, which distinguishes them from divergent and convergent boundaries. Instead, they shift horizontally, resulting in the characteristic geological features associated with transform boundaries.