Horizontal sliding, in the context of plate tectonics, occurs along transform faults. Transform faults are a type of tectonic plate boundary where two plates slide horizontally past each other. These boundaries are characterized by intense seismic activity and may result in earthquakes. The most famous example of a transform fault is the San Andreas Fault in California, USA. To identify the location of horizontal sliding on the Earth, you can refer to a map that shows tectonic plate boundaries. There are several online resources, such as the US Geological Survey (USGS) website, that provide interactive maps showing plate boundaries and fault lines. By examining these maps, you can identify areas where horizontal sliding is taking place.
