Answer:
question 1, continential plates are thicker than Oceanic plates
yes plate movments can affect people living on land
Explanation:
plate movements can affect people living on land because if they hit off eachother, it can cause earthquakes. if one slides under the other it can make mountains
<u>Answer:</u>
<em>Land & plant fossils found across oceans
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<u>Explanation:</u>
Abundant proof supports the significant conflicts of the ocean bottom spreading hypothesis. To begin with, tests of the profound seafloor show that basaltic maritime outside and overlying dregs become dynamically younger as the mid-sea edge is drawn nearer, and the silt spread is more slender close to the side. Second, the stone making up the sea depths is impressively younger than the landmasses, without any examples found 200M years, as appeared differently concerning most significant times of more than 3B years for the mainland rocks.
Answer:
When a wave is too steep to support itself, the wavefront collapses creating a <u> </u><u>break </u>that advances up the shoreline
Explanation:
When waves are tall, with a great slope that makes them unstable, they break. Braking waves might occur inshore or offshore.
- Offshore: Breaking waves in the deep sea occurs when the wind speed increases so fast that they exceed the speed of the waves. These last ones acquire additional energy from the winds increasing their slopes to the point of being so unstable that the water from the crest falls forward and breaks the wave. The most influencing factor in these breaking waves is the speed of the winds.
- Inshore: When waves are near the shore, the scarce water deepness increases the friction of the wave with the marine bottom, and consequently, the wave´s speed decreases progressively. The wave loses energy in the friction, the wave energy is concentrated in a lower length, and the wave grows in size. As it increases, it acquires a sharper slope. As deepness decreases, the wave base loses speed, but the crest does not. As the wave crest travels faster, the frontal face of the wave becomes concave. This change in shape continues until the wave can not support itself and it breaks. The break is not produced by the friction with the bottom, but by exceeding the slope limit values.
