Solid Earth. Long linear regions of geologic features are explained as plate boundaries. For example: Mid-ocean ridges, high regions on the seafloor where
Answer:
Explanation:
Enter the data to create a histogram. Then check all that apply.
A 1-column table with 10 rows. Column 1 is labeled runs with entries 1, 7, 1, 6, 1, 2, 8, 6, 8, 0.
The histogram has 1 cluster.
The histogram has 2 clusters.
The histogram has 1 peak.
The histogram has 4 peaks.
The histogram has 0 frequency from 4-5.
Answer:
Explained below
Explanation:
In physics, we know that waves usually change direction when are refracted or when they penetrate layers with different densities.
Therefore, when a seismic wave penetrates penetrates the boundary of the earth's interior, part of it will be sent back and part will be transmitted into the medium as refraction occurs. When we record the reflected and refracted ray, it enables the calculation of the position of major boundaries in the Earth's interior. This also helps in providing information about the solid & liquid character as well physical properties of the various layers in the medium.
The mostly lie inTajikistan
Answer:
In the winter days are shorter and night are longer in the northern hemisphere.
Explanation:
- In the northern hemisphere the summers are much warmed than the winters. As the earth is closet to the sun in July. Each past the winter solstices noon sun is a little higher over the south. Heating and cooling give us a practice indication of the changes at different latitudes.
- The latitude changes can be seen by the direction and duration of the suns rays, for the northern latitudes rays are much slating and for southern hemisphere they are more direct in winter.
