Answer:
oxbow lake
Explanation:
The meander usually originates in the rivers located in the alluvial plains that have almost no slopes due to the sediments of the earth that commonly settle in the convex areas of the meander. However, in the concave areas, thanks to the operation of forces of centrifugal characteristics, greater erosion is generated and the banks are diminished.
If the natural action of the erosion of water and sediments causes two curvilinear channels to be found between them, the river will react through the area where the currents exert opposition and in this way it will originate a horseshoe lake or oxtail (in English usually called <u>oxbow lake</u>) because the sediments will block the entry of water and the exit of the previous meander, which will cause it to be outside the river path.
Answer:
Remittances represent a capital flow from the home country to the host country is a false statement.
Explanation:
Remittances represent a capital flow from the host country to the home country. This happens fairly often, and most found among migrants that have moved to another country to work by themselves, while their families have remained in the home country.
This process is positive on one side and negative on another. The positive aspect of it is that the migrants support their families and enable them a better life. The negative aspect is that they damage gradually the economy of the host country in which they work, as they take money out of it and send them to another country. If there is a higher percentage of people doing this in the long run, the economies of the host countries will face difficulties and will start to decline, which is not good for anyone.
Answer:
wdym why does it say 20 characters long man
Explanation:
what do you mean ??
The area of the rectangle would be 37.4 ft
Cambrian period do the Appalachian mountains first start to appear. The Paleozoic Era and the Phanerozoic Eon were both preceded by the Cambrian Period.
An crucial turning point in the evolution of life on Earth occurred during the Cambrian Period, when numerous invertebrate species and the first fish-like vertebrates first appeared in the fossil record. The greatest record of Cambrian animal fossils, including soft-bodied creatures, may be found in the Burgess Shale. The Paleozoic era's Cambrian phase saw the most rapid explosion of evolution ever recorded. A staggering diversity of life, including many of the main animal groupings still extant today, emerged during the Cambrian Explosion. The chordates, which include vertebrates (animals with backbones) like humans, were among them. According to some experts, the appearance of predators was made possible by a slight, possibly transient increase in oxygen that abruptly crossed an ecological threshold. Carnivory's emergence would have sparked an evolutionary arms race that produced the explosion of various body kinds and behaviours that now populate the oceans. The team comes to the conclusion that a scarcity of oxygen and toxic hydrogen sulphide killed off a large number of Cambrian species. It is believed that similar circumstances led to the devastating Permian extinction 251 million years ago. According to Gill, there were multiple instances of fast extinction in the second half of the Cambrian.
Learn more about Cambrian period here
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