Social Studies, 05.01.2020 00:31 rainyfallaw

What was good about the cash only policy of cooperatives

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Every cooperative board of directors is charged with both protecting and utilizing the resources of the cooperative for its members. This simply stated prime directive is far from a simple task.

Balancing the needs of the member with the needs of the cooperative’s balance sheet is a tricky proposition at best. Establishing margins to cover actual costs along with additional net savings that will allow for future growth of services can be difficult, but past performance – together with reasonable expectations and realistic optimism – should drive financial projections.

With the help of the cooperative’s management, boards develop and approve business plans that will meet the organization’s goals. Most planning cycles are conducted annually, creating a budget that anticipates surpluses. New projects offering better services or products are financed along with long-term financing, either with new injections of capital or long-term borrowings. Unrealistic long-term financing projections can seriously interrupt the monthly and daily operations of a cooperative, therefore, understanding how current assets and liability affect the cash to cash cycle is a critical piece of knowledge that any board member needs. Current assets consist of cash, inventories and accounts receivable. Current liabilities include accounts payable for goods and services and the current portion of long or immediate term debt.

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Ibelieve the answer is battle of saratoga but i could be wrong

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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)

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