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Explore Learning Gizmo Ocean Tides Answer Key explorelearning gizmos: math & science simulations ... explore the library ... these processes are explored in the nuclear reactions gizmo. in the.

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Tides and Water Levels On the far side of the Earth, inertia dominates, creating a second bulge. The relative distances and positions of the sun, moon and Earth all affect the size and magnitude of the Earth's two tidal bulges.

In the Gizmo, students see that the moon's gravity causes a “bulge” of water to form on the near and opposite sides of Earth. An observer experiences high tide when she rotates into one of these bulges, about every 12 hours. Low tides occur in the spaces between the bulges.

Gravity and inertia act in opposition on the Earth's oceans, creating tidal bulges on opposite sites of the planet. On the “near” side of the Earth (the side facing the moon), the gravitational force of the moon pulls the ocean's waters toward it, creating one bulge.

The alternating advance and retreat of seawater along a coastline is called a tide. High tide is when water advances to its furthest extent onto the shoreline. Low tide is when it recedes to its furthest extent. Some freshwater rivers and lakes can have tides, too.

Tides are very long-period waves that move through the ocean in response to the forces exerted by the moon and sun. Tides originate in the ocean and progress toward the coastlines where they appear as the regular rise and fall of the sea surface.

The Moon and Earth exert a gravitational pull on each other. On Earth, the Moon's gravitational pull causes the oceans to bulge out on both the side closest to the Moon and the side farthest from the Moon. These bulges create high tides. The low points are where low tides occur.

What are tides? Tides are daily changes in the elevation of the ocean surface. Ocean tides result from the gravitational attraction exerted upon earth by the moon and, to a lesser extent, by the sun.

tide, any of the cyclic deformations of one astronomical body caused by the gravitational forces exerted by others. The most familiar are the periodic variations in sea level on Earth that correspond to changes in the relative positions of the Moon and the Sun.

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