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. n. 1. (Geological Science) a thin semifluid layer of the earth (100-200 km thick), below the outer rigid lithosphere, forming part of the mantle and thought to be able to flow vertically and horizontally, enabling sections of lithosphere to subside, rise, and undergo lateral movement.See also isostasy.he upper part of the Earth's mantle. The asthenosphere lies beneath the lithosphere and consists of several hundred miles of partially molten rock. Because it is partially molten, seismic waves passing through this layer have slow velocities.