The Ninety East Ridge is a submarine volcanic ridge located in which ocean?
Indian Ocean
The question asks about the location of a significant geological feature known as the Ninety East Ridge. This feature is a submarine volcanic ridge, meaning it's a ridge found underwater on the ocean floor, formed by volcanic activity.
Ocean basins contain various geological structures, including mid-ocean ridges, abyssal plains, trenches, and submarine ridges like the Ninety East Ridge. Identifying the specific ocean where a feature like this is located is key to understanding marine geography.
Let's consider the options provided and determine which ocean hosts the Ninety East Ridge:
The Ninety East Ridge is a prominent, nearly linear underwater feature. Its name gives a strong hint about its approximate longitude. While not perfectly straight along 90 degrees East, it follows this general meridian for a long distance.
Based on geological surveys and oceanographic studies, the Ninety East Ridge is definitively located within the Indian Ocean.
| Ocean | Key Ridge Features | Ninety East Ridge Location |
|---|---|---|
| Pacific Ocean | East Pacific Rise, Hawaii-Emperor seamount chain | Not located here |
| Atlantic Ocean | Mid-Atlantic Ridge | Not located here |
| Arctic Ocean | Lomonosov Ridge, Gakkel Ridge | Not located here |
| Indian Ocean | Ninety East Ridge, Central Indian Ridge | Located here |
Therefore, the Ninety East Ridge is a significant geological feature of the Indian Ocean floor.
The question asks for the ocean where the Ninety East Ridge is located. By examining the options and recalling the major features of the world's oceans, we determine that the Ninety East Ridge is situated in the Indian Ocean.
| Feature Name | Type | Location | Approximate Longitude |
|---|---|---|---|
| Ninety East Ridge | Submarine Volcanic Ridge | Indian Ocean | 90° East |
Submarine ridges are elevated features on the ocean floor. They can be formed by various geological processes:
The Ninety East Ridge is notable for its exceptional linearity and length, stretching over 5,000 kilometers. It represents a crucial part of the Indian Ocean's geological history and structure.
In terms of geological time scale, the quaternary period consists of two epochs. They are:
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Statement II: Geostrophic wind is the horizontal wind velocity, in which the Coriolis force balances the horizontal pressure force.