The physical environment has played a very big role in the settlement patters in Ukraine, as well the economic activities of the people that lived in this area.
The settlement patterns in Ukraine are relatively simple, as most of the settlements have been made on the banks of the large rivers, such as the Dnipro and Dniester, and Don, as well as on the coastlines of the Black Sea and the Sea of Azov. So we can say that the settlements have been built in close proximity to the larger water bodies.
The location of the settlements around the water bodies was not a coincidence, as these water bodies were used for trade, so the people living in Ukraine were heavily engaged in the trade that was going through their territory. Also, Ukraine is part of the Eurasian steppe, so people were trading a lot on land as well, especially because they were a transition zone between Asia and Europe.
Bangkok, the capital of the Southeast Asian country of Thailand, is influenced by the monsoons, and they are the dominant climatic factor in this region and gives it its climatic patters.
There's two seasons, a wet one, and a dry one. The wet season is characterized by heavy rainfall for a prolonged period of time, and those rains are brought by the wet and warm monsoons coming from east. The dry season is characterized by prolonged period of time that is warm and dry, and that is caused by the dry monsoon winds coming from the west.
During the wet season, the air pressure is higher because the rain increases the weight of the air.
During the dry season, the air pressure is lower because of the high evaporation, and the water vapor is lighter than the air itself, thus causing the air to weigh less.
Answer:
Tonal
Explanation:
for example, Tonal languages such as Chinese and Hausa use pitch to distinguish words in addition to intonation.
Rising intonation means the pitch of the voice increases over time; falling intonation means that the pitch decreases with time.
Answer:
Igneous rocks can be divided into four categories based on their chemical composition: felsic, intermediate, mafic, and ultramafic. The diagram of Bowen's reaction series (Figure 7.6) shows that differences in chemical composition correspond to differences in the types of minerals within an igneous rock.
Explanation:
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