Dating go with the flow


In addition to sedimentary structures that are normally associated with bedding planes, there are other such structures that result from deformation during or shortly after sedimentation but before induration of the sediment into rock. Everyday substances are ordinarily classed as either solids, liquids, or gases, and, under normal circumstances, gases and liquids flow relatively freely and solids deform when they are subjected to forces.

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Others might have such an experience while engaged in an activity such as painting, drawing, or writing.So what can you do to increase your chances of achieving flow?In his book, Csíkszentmihályi explains that flow is likely to occur when an individual is faced with a task that has clear goals that require specific responses.Most gases conform quite well to this relationship over a remarkably wide range of conditions.shear stresses can exist in such a “perfect fluid.” (Shear stresses involve the energy dissipated as adjacent planes of molecules slide across one another, as in the action of a card player spreading a pack of cards across a table.) Water, the most common liquid of all, has properties quite close to those of a perfect fluid.consist of molecules that, like those of the perfect fluid, are in contact with one another but do exert forces on one another so that shearing motions within the liquid are resisted.Plastic flow is also a central factor in the attempts to understand the movement and flow of rocks under conditions of high temperature and pressure that make them behave like ductile materials.

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