If you're a scientist who studies these phenomena, you probably know all about how to model their nucleation using the Discrete Element Method software ESyS Particle.
If you're a scientist who studies these phenomena, you probably know all about how to model their nucleation using the Discrete Element Method software ESyS Particle. One version of these phenomena is the subject of a landmark 1996 paper by Janusza that introduces "anticrack theory" as a means of understanding how the alpha-gamma phase transformation of olivine to spinel causes them. Amos Nur introduced the idea of a "storm" of these phenomena, and when they recur repeatedly, it is known as a "swarm" of them. In a subduction zone, the area where these phenomena are concentrated at low depths is known as the Wadati-Benioff Zone, which is home to the "deep focus" type. They also produce an acoustic Rayleigh wave and a horizontal shear Love wave, and they create waves that were used to locate the Gutenberg and Moho discontinuities. For 10 points, name these P- and S-wave making phenomena, the magnitude of which can be measured using the Modified Mercalli or Richter scales.
If you're a scientist who studies these phenomena, you probably know all about how to model their nucleation using the Discrete Element Method software ESyS Particle.
{earthquake}s [accept {temblor}; accept {tremor}]