Answer:
Five types of geological evidence that provide strong support for the concept of continental drift :-
Explanation:
1. Occurrences of plant and animal fossils throughout Gondwanaland.
2. Matching of continental coastlines of Africa and South America.
3. The occurrence of volcanic rocks of similar age on different continents.
4. Ancient occurrences of tropical plant fossils in rocks from high latitudes.
5. Continuity of rocks and geological structures extending from South America to Africa.
This evidence was given by the geologist of that time like the Alfred Wegener in his period and since then have been seen to date are the most trusted evidence in the evolutionary phase of supercontinents.
They are made up of mainly hydrogen and helium. They are called the gas giants
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Abyssal plains are large, flat features that cover about one third of the planet.
<h3>What are Abyssal plains?</h3>
- The broad, flat, sediment-covered regions of the deep ocean floor are known as abyssal plains.
- They have a slope of less than one foot of height variation for every thousand feet of travel, making them the flattest, featureless places on Earth.
- When tectonic plates separate, magma rises and forms new crust, filling the space that was left between the plates.
- When sediments from the shoreline pass over the continental shelf, tumble down the continental slope, and deposit on top of the more recent oceanic crust, they create an abyssal plane.
Learn more about Abyssal plains here:
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The border between the outer core and the inner core is about 5,100 km<span> below the surface of the Earth. (The crust is usually between 3 and 70 km thick, being thicker in the continents and thinner in the oceans,)
Hope this helps, </span>