Answer:
latitude 70 degrees N
latitude 50 degrees N
latitude 40 degrees N
latitude 30 degrees N
latitude 10 degrees N
Explanation:
The Latitude measures coordinate north or south of the Equator on a globe. It starts at 0 degrees at the equator to 90 degrees in the north and the South. So 10 degrees North and 10 degrees south are the closest to the equator while 90 degrees North and South are the farthest from the equator.
The meridian is made up of the North and South points on the horizon and forms a 90 degree angle with the celestial equator.
Answer:
The first truly detailed and comprehensive theory of continental drift was proposed in 1912 by Alfred Wegener, a German meteorologist. Bringing together a large mass of geologic and paleontological data, Wegener postulated that throughout most of geologic time there was only one continent, which he called Pangea.
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The answer is <span>nonconformity</span>
Answer:
The tension based on popular culture between the less developed and developed countries comes from the fact that the western (developed countries) perspective may become more dominant.
Explanation:
The process of globalization has brought in a lot of benefits to people from all over the world. Unfortunately, it has caused some serious problems as well, and these problems predominantly affect the less developed countries because they are less influential and less powerful. The main problem comes in the form of the loss of native cultures because of the spread of popular culture.
The western countries are more powerful, have managed to become part of the economies and societies of countries from all over the world, and this has also led to the advertising of their culture. While the advertising of popular culture may not affect middle-aged and elderly people, it has a great effect on the younger population. The youngsters see the popular culture from the western countries as 'cool' and superior to their native one, thus adopt it without a problem and neglect their native culture. The result of this is a sharp decline and bringing on the verge of extinction of many cultures around the globe.
estimating geoacoustic properties of sediments with a wide grain-size distribution using sediment organic content and the viscous grain shearing model
Interstitial organic matter (OM) is a common component of marine sediment and is frequently measured across a variety of fields.
It is especially common in sediments with high silt/clay fractions. OM hasn't been accounted for in sediment acoustics models despite the fact that it suspends silt and clay particles in the sediment matrix, adheres to mineral surfaces, and typically lives between mineral contacts, all of which are thought to affect geoacoustic characteristics.
Recent research on sediments from the Baltic Sea, Texas, seagrass-bearing sediments, and mud banks in Brazil has demonstrated that OM content (OC) corresponds strongly with sediment geoacoustic characteristics, including porosity and index of impedance.
Learn more about sediments here
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