after strenuous exercise inexperienced athletes will quite often attempt to recover and resume normal breathing by bending over sitting down using the mechanics of ventitation, how would ypu modify the recovery practices of these athletes

This recovery practice could be modified by encouraging the inexperienced athletes to squart down rather than bending over or sitting down.

Explanation:

During exercise, energy is burnt and this is evident through the difficulty in breathing and sweating experienced by the athletes. Unfortunately, most inexperince athletes, attempt to recover by bending over or sitting down.

In other to improve the recovery practice, the can also squart down. This would encourage the adequate flow of air into their body. And, the blood circulation would be greatly improved leading to adequate flow of air into the blood system.

On the long run, their breathing difficulty would normalise faster in this approach rather than when they where bending over.

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the earth’s crust is broken into separate pieces called tectonic plates (fig. 7.14). recall that the crust is the solid, rocky, outer shell of the planet. it is composed of two distinctly different types of material: the less-dense continental crust and the more-dense oceanic crust. both types of crust rest atop solid, upper mantle material. the upper mantle, in turn, floats on a denser layer of lower mantle that is much like thick molten tar.

each tectonic plate is free-floating and can move independently. earthquakes and volcanoes are the direct result of the movement of tectonic plates at fault lines. the term fault is used to describe the boundary between tectonic plates. most of the earthquakes and volcanoes around the pacific ocean basin—a pattern known as the “ring of fire”—are due to the movement of tectonic plates in this region. other observable results of short-term plate movement include the gradual widening of the great rift lakes in eastern africa and the rising of the himalayan mountain range. the motion of plates can be described in four general patterns:

collision: when two continental plates are shoved together

subduction: when one plate plunges beneath another (fig. 7.15)

spreading: when two plates are pushed apart (fig. 7.15)

transform faulting: when two plates slide past each other (fig. 7.15)