The correct answer is - No.
Winnipeg, Canada, is not further away from the Equator than Moscow, Russia, in fact Moscow is the city that is further away from the Equator. Moscow is on a latitude of 55.7558° North, while Winnipeg is on a latitude of 49.8951° North, thus putting Moscow by 5.8607° further away from the Equator than Winnipeg is.
Answer:
barchan
Explanation:
sand dunes make the wind erosion
The graphic below depicts the approximate location of marine magnetic anomalies in relation to mid-ocean ridges. Canada Crest of Juan de Fuca Ridge in the United States Crest of Ridge MIIN is that they appear in stripes that are offset along transform faults and parallel mid-ocean ridges.
<h3>What are marine magnetic anomalies?</h3>
An alteration in the strength of the Earth's magnetic field brought on by the magnetism of ocean floor rocks is known as a marine magnetic anomaly. Typically, marine magnetic anomalies make up 1% of the total geomagnetic field strength. The anomalies that surround mid-ocean ridges exhibit a recognisable pattern, according to magnetic measurements over the oceans. They consist of a sequence of stripes that run perpendicular to each ridge, formed by positive and negative anomalies in the magnetic field's strength. They frequently have symmetry about the ridge's axis.
<h3>Why are magnetic anomalies important?</h3>
Together, magnetic anomalies serve as the primary method for dating oceanic basins and create the groundwork for reconstructions of the earth's plates, which set significant limits on how the lithosphere, biosphere, hydrosphere, cryosphere, and global climate developed. The magnetometer, which can monitor the Earth's magnetic field and find changes brought on by magnetic anomalies, is generally considered to be the most important piece of measurement equipment.
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Answer:
Two primary materials that geologists use as clues to understand Earth's past are the geologic time scale and paleogeographic maps.
Explanation:
Answer:
Densidad.
Explanation:
The greater the density of an oceanic lithosphere plate, the greater the weight of that plate. This will affect the degree of subduction of that card. The higher the density, the greater the degree of subduction and the ability of the plate to descend, forcing the creation of prominent and well-defined trenches on the ocean floor.
The density of the plaque increases as the age of the plaque increases, so we can consider age, another factor in the formation of these trenches.
