A Guide to Understanding Lehmann Discontinuity
The Lehmann discontinuity is marked by an abrupt increase in seismic wave velocity. It occurs at depths of about 200 km (137 mi) from the
The Lehmann discontinuity is marked by an abrupt increase in seismic wave velocity. It occurs at depths of about 200 km (137 mi) from the
An ignimbrite or ash-flow tuff is a type of volcanic rock formed from pyroclastic flow deposits. It has poorly sorted pumice fragments, scattered lithic fragments,
The Mohorovičić (Mo‐HOR‐o‐VITCH‐itz) discontinuity is a boundary between the Earth’s crust and the upper mantle. An abrupt increase or jump in seismic wave velocity marks
The lithosphere is a colder, rigid, mechanically stronger solid outermost layer or shell of the Earth. In contrast, the asthenosphere is hotter, weaker, and ductile.
The lithosphere is the outermost, rigid, solid layer of the Earth. It is like the shell of a coconut or egg. Location-wise, this layer lies
The asthenosphere is one of the most special or unique layers of the Earth not known to other planets like Mars or Venus. It is
Bluestone is a generic, commercial, or cultural name for several types of blue-grayish colored rock. It may mean sandstones, slate, limestones, basalt, or diabase/dolerite rocks
Obsidian is a natural volcanic glass often called a volcanic or extrusive igneous rock. IUGS considers it a mineraloid since it has > 80% glass.
Hydrothermal metamorphism occurs when hot, water-rich fluids cause a change in the mineral assemblage and/or texture of existing parent (protolith) rocks. It usually has a