The curved circulation of surface currents is caused by the <span>Earth's rotation.
</span><span>The 'Coriolis Effect' describes how Earth's rotation steers winds and surface currents (Figure 14.14). The Earth is a sphere that spins on its axis in a counterclockwise direction when seen from the North Pole. The further towards one of the poles you move from the equator, the shorter the distance around the Earth. This means that objects on the equator move faster than objects further from the equator. While wind or an ocean current moves, the Earth is spinning underneath it. As a result, an object moving north or south along the Earth will appear to move in a curve, instead of in a straight line. Wind or water that travels toward the poles from the equator is deflected to the east, while wind or water that travels toward the equator from the poles gets bent to the west. The Coriolis Effect bends the direction of surface currents.</span><span>
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Answer:
Tropical climates are better suited for a multitude of species of plants and animals.
Explanation:
The reason for this is tropical climates are easier to handle then harsh winters because almost all tropical climates are near the equator so it tends to stay warmer year round creating a year round growing period. Polar climates are harsher on the plants than the animals. Also consider this the fact that there would be no herbivore animals for predators to eat so that limits what can grow in the polar climates.
Answer:
C. Isasaalang-alang Ko Ang Klima Ng Isang Lugar.
Paliwanag:
Ang pinakamahusay na paraan upang paghiwalayin ang isang rehiyon ay batay sa klima sapagkat ang bawat rehiyon ay may magkakaibang klima dahil sa taas at distansya mula sa ekwador. Ang mga rehiyon na matatagpuan sa mataas na taas, ay may cool na klima habang sa kabilang banda, ang mga rehiyon na nasa ekwador o malapit sa ekwador na mayroong mainit at mainit na klima upang mapagpasyahan natin na ang klima ay isang mabuting kadahilanan upang paghiwalayin ang mga rehiyon.
The ocean floor and its depth vary a lot from place to place. Maybe it is expected that the central parts of the oceans would be the deepest parts of them, while the closer the ocean floor is to the land it will be shallower, but that is not the case.
The central parts of the oceans have mid-ocean ridges. The mid-ocean ridges are volcanic underwater mountain ranges. There is constant propelling of magma, and as the magma cools off quickly it creates new crust. This results in the mid-ocean ridges gaining heights of up to 1.5 km above the surrounding area.
The further away we move from the mid-ocean ridges, or rather being closer to the oceanic margins, the depth actually increases. The reason for this is the erosiove power of the water, but also the subduction zones. The erosion manages to flatten the ocean floor, thus making it deeper, while the subduction zones are the places where the oceanic plate is moving downward toward the mantle, and it create ocean trenches which are very deep, in fact the deepest parts of the oceans.
