Some pitchers simply recover quicker than others, so pitching off of three days rest will be a case by case issue. If the pitcher can do it, great, but no matter who is pitching on three days rest, watch them carefully. They may hit that proverbial wall a bit quicker than they would off of five days rest.ome pitchers simply recover quicker than others, so pitching off of three days rest will be a case by case issue. If the pitcher can do it, great, but no matter who is pitching on three days rest, watch them carefully. They may hit that proverbial wall a bit quicker than they would off of five days rest.
The asthenosphere is the highly viscous, mechanically weak and ductilely deforming region of the upper mantle of the Earth.The asthenosphere is generally solid although some of its regions could be melted (e.g. below mid-ocean ridge). The lower boundary of the asthenosphere is not well defined. The thickness of the asthenosphere depends mainly on the temperature is involved in plate tectonic movement and isostatic adjustments. For lecture on Asthenosphere visit
asthenosphere-the soft, flexible upper layer of the mantle, on which the tectonic plates move. continental drift-the theory that all of Earth's continents were once joined together into a single large landmass, and then moved apart, forming the continents we see today. convection-transfer of heat by movement of a fluid.ondwana-the southern continent formed when Pangaea split into two pieces. Laurasia-the northern continent formed when Pangaea split into two pieces. lithosphere-the rigid, brittle layer made up of the crust and the uppermost part of the mantle. It is broken up into pieces called tectonic plates.