Answer:
False. Antarctica is covered by 98% of ice.
Explanation:
I think that the answer is c, ridges!
The distance between each pair of points.
(-4, 6) and (three, -7) is (7, 9)
(-6,-5) and (2.0) is (8, 5)
Distance is a numerical measurement of how long way aside items or points are. In physics or regular utilization, the distance may additionally discuss with a bodily period or an estimation based on different criteria. the distance from point A to a degree B is now and again denoted as |AB|. the extent or amount of space among matters, points, strains, and so on. the nation or truth of being apart in space, as of 1 issue from every other; remoteness. a linear volume of space: Seven miles is a distance too incredible to stroll in an hour.
Distance between points is the period of the line segment that connects the two given points. Distance between two factors in coordinate geometry may be calculated by using finding the length of the road phase joining the given coordinates.
The distance of an object can be defined as the entire direction traveled by using an item. for example. if a car travels east for five km and takes a flip to travel north for every other eight km, the whole distance traveled via car shall be 13 km.
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Answer:
The answer is "Provide strong evidence for seafloor spreading".
Explanation:
The magnetic changes from east to west and vice versa are geomagnetic. geomagnetic reversals. And they can provide significant evidence of the expansion of sea bed in the rocks formed along the middle sea ridges by documenting the geomagnetic pattern of echo.
A new crust is developing from the magma explosion into the seafloor in the ocean along the mid-oceanic ridges along the mid-ocean ridges. When the magma cools, the minerals of ferromagnetism found in the magma will align as per the magnetosphere of this time.
In the event of geomagnetical revolutions, newly formed minerals will be reverse-aligned to early elements, thus registering the lithosphere on both sides of the mid-oceanic ridge. Lithosphere, one could argue, is a continual move away from oceanic crusts midway through.
