Margins of plates are action locations for earthquakes and are represented on a map.
Convection cells in the asthenosphere are represented in a cross-section view.
Divergent Margins occur when the asthenosphere is rising, creating new oceanic crust and lithosphere.
Mid-oceanic ridges are where the oceanic crust and lithosphere separate, forming new ocean basins.
Rift- valleys are where the continental crust and lithosphere separate, forming new continents.
Convergent Margins occur when the asthenosphere is sinking, destroying existing oceanic crust and lithosphere.
Trenches are where the oceanic crust and lithosphere subduct, forming new ocean basins.
Volcanic Island Arc or Chain is the leading edge of the over-riding plate.
Folded Mountain Chains, such as the Himalayas, are formed by the collision of tectonic plates.
Transform Faults are where plates sliding past one another horizontally.
San Andres Fault is an example of a natural process where water moves from within the ocean into the atmosphere, a process called infiltration.
The rock called "granite" is an igneous rock that erupts onto the surface to form the Earth's ocean basins.
The existence of "natural laws" that work throughout the Universe is a "fact" based upon utilization of the scientific method.
Basalt is an igneous rock enriched in Fe, while Granite is an igneous rock enriched in Si and contains quartz.
In science, numbers and units are referred to as "units" and can be compared using comparisons such as "too big" or "too small" on an Exponential Scale.
Density is represented as gm/cm3.
Convection Cells are the redistribution of heat generated by the movement of materials of differing density due to differences in temperature.
Plates are pieces of lithosphere moving as a coherent mass.