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
The asthenosphere is the layer of the Earth that lies below the lithosphere. It is a layer of solid rock that has so much pressure and heat the rocks can flow like a liquid. The rocks are less dense than the rocks in the lithosphere. This allows the tectonic plates in the lithosphere to move around on the Earth's surface by floating on the rocks that are slowly flowing like a liquid. Tectonic plate interaction with the upper layers of the Earth, USGS. Earthquakes.