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erica [24]
3 years ago
9

An organization's budgeting process should include the expression of its major policies: A. in writing and in qualitative terms.

B. in writing and in subjective terms. C. both verbally and in writing. D> both in writing and through training sessions. E. None of these is correct
Geography
1 answer:
Greeley [361]3 years ago
8 0

Answer:

E.None of these is correct.

Explanation:

In the organization budgeting ,organization sets the activity to be perform and sets the future target which want achieve with in the specified time limit.In the simple words we can say that planning before starting anything or we can say that pre planning to achieve the targets.These all polices should be in written expression of quantitative terms which represents the limitation of our resources.

So from we can say that our option E is right.

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I think its Piedmont

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Label the two city-states Athens and Sparta. Turn to the map on page 387 in your book. In what modern country are Athens and Spa
tangare [24]

1. Athens is located in the southeastern part of Greece, while Sparta is located in the southern part of Greece.

Explanation:

Athens and Sparta were both ancient city-states. They were part of the Hellenic world, or ancient Greece as it is more often referred to. The two cities were competitors, and more often than not they were in bad relations than in good ones.

The people from neither Athens nor Sparta referred to them as Greeks, but instead they identified themselves with the city-state they belonged to, thus Athenians and Spartans. These two city-states were very different in their political organization and the way the people lived, with Athens being democracy, but also very restrictive to the women, while the Spartans were a militaristic monarchy, and the women had much more freedom.

Both of these ancient city-states were located on what is now Greece. Athens is in fact the capital of modern day Greece.

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2. The name of the country, Greece, doesn't appear on the map because there was no such country in existence until the mid 19th century.

Explanation:

Contrary to the popular belief, a country named Greece did not existed in the antique period. The country formed and started using this name only in the mid 19th century. Instead of one country in what is now Greece (without Macedonia and Western Thrace), there were multiple city-states, all of which had their own name and identity.

The city-states didn't had one common ethnic identity, but instead the people identified with the city-state in which  they were living in. A term that was used to somewhat describe all of the city-states was Hellenistic, which was based on the language.

This part of the Balkan Peninsula was actually the only one where there were no people that formed a unified country, usually in the form of kingdom. All of the other groups of people on the Balkan had their own kingdoms, such as:

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Please Help!
kvasek [131]

1. How were the continents during suilurien

Ans: During the Silurian , the Earth witnessed many changes in the way in which landmasses were distributed around the globe. Although there were no major volcanic events, a deglaciation and rise in sea levels occurring at that time produced varying periods of continent coverage and exposure. The variation of ocean levels occurred alongside the process of continental fragmentation and grouping that occurred from the Cambrian to the present.

At that time, the continents were distributed very differently than they are today. The Silurian world consisted of a vast north polar ocean and a south polar supercontinent (Gondwana) with a ring of approximately six continents. By the Silurian period, a large portion of the Rodinian landmass had become fragmented, and those fragments migrated toward the equatorial region. Most of these fragments were eventually assembled by a series of plate collisions into the super-continents of Laurussia and Laurasia. The modern Philippine islands were most likely inside the Arctic Circle, while Australia and Scandinavia resided in the tropics; South America and Africa were probably over the South Pole.

There was no major volcanic activity during the Silurian; however, the period is marked by major orogenic (mountain-building) events in eastern North America and in northwestern Europe, resulting in the formation of the mountain chains there. This was called the Caledonian Orogeny. In other areas, large igneous rock formations of the Middle Silurian arose, such as those in Central Europe, as well as light sedimentation throughout the Baltic region. While not characterized by dramatic tectonic activity, the Silurian world experienced gradual continental changes that would be the basis for greater global consequences in the future, such as those that created terrestrial ecosystems.

The Silurian oceans are also of particular interest for activity between the regions known as Laurentia, Baltica and Avalonia. The ocean basins between these areas substantially closed together, continuing a geologic trend that had begun much earlier. The new marine habitats produced by these profound changes in the Silurian seas provided the framework for significant biological events in the evolution of life. Coral reefs, for example, made their first appearances in the fossil record during this time.

The Silurian period was a time when the earth underwent considerable changes that had important repercussions for the environment and the life within it. The Silurian witnessed a relative stabilization of the world's general climate, ending the previous pattern of erratic climatic fluctuations. One significant feature of these changes was the melting of large glacial formations. This contributed to a substantial and significant rise in the levels of the major seas, creating many new marine habitats.

The Silurian period's condition of low continental elevations with a high global stand in sea level can be strongly distinguished from the present-day environment. This is a result of the flood of 65% of the shallow seas in North America during the Llandovery and Wenlock times. The shallow seas ranged from tropical to subtropical in climate. Commonly present in the shallow seas were coral mound reefs with associated carbonate sediments. Due to reduced circulation during the Ludlow and Pridoli times, the process of deposition of evaporites (salts) was set in motion. Some of these deposits are still found in northern Europe, Siberia, South China and Australia.

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