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
What Is the Asthenosphere? The asthenosphere is part of the upper mantle located below the crust of the earth. The asthenosphere boundary is primarily defined by temperature, and it starts when the crust heats up to 1300Â° C. At this temperature the crust begins to melt and move more as a liquid. The asthenosphere is important in plate tectonics, as convection currents slowly move the tectonic plates that lie above.