Answer:B. coarse-grained
Explanation: Batholith is a part of igneous rock that is about 100 square kilometers in Length, they are often made by of felsic or intermediate rock types, such as granite, quartz monzonite, or diorite.
At the Half Dome of intrusive Batholiths one is expected to see coarse-grained Rock materials (rock or sand particles or grains with different sizes). Igneous rocks are very hard rocks such as the Batholiths are formed as a result of cooled magma.
Both types of measures have their respective values and limitations. Human Development Accounting is required to make a comprehensive assessment of human development conditions in any society, but it does not provide a single number to synthesize the state of affairs in some basic dimensions. Composite indices, on the other hand, provide a single number, but cannot provide a comprehensive picture of the state of human development in any situation. Focus measures are extremely good for advocacy, for initiating healthy competition among societies and for raising awareness, but not in providing a comprehensive picture. Breadth measures, on the other hand, are good for painting a comprehensive picture, but not for providing a single number for drawing attention.
Answer:
Latitude lines go up to 90 degrees at the North pole and 90 degrees down the South pole.
Explanation:
Humans, in order to satisfy their needs, have created imaginary lines across Earth. One of these lines cut Earth from north to south, thus are roughly vertical, while the other ones cut Earth from east to west, thus are horizontal. The lines that run from east to west are called latitude lines, while the ones that run fron north to south are called longitude lines.
The latitude lines start off from the Equator which cuts Earth into two equal parts - Northern Hemisphere and Southern Hemisphere. The Equator has 0 degrees latitude and the latitude lines extend to 90 degrees north and 90 degrees south. These lines are used for navigation, determining coordinates, but are also good indicators of Earth's climate zones and biomes.
Antartica is a polar climate.
Answer:
Scientists use waves to study the different layers of the earth. Usually, they use seismic waves, which are waves generated by earthquakes or nuclear-test explosions. The seismic waves are bent, sped up, or slowed down, or even reflected when they pass through the earth's layers.
Seismic waves are recorded by a machine called a seismograph, which tells us about the strength and speed of the seismic waves. ... Seismic waves travel at different speeds when they pass through different types of material, so by studying seismograms, scientists can learn a lot about Earth's internal structure.
Explanation:
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