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The study of the structures of deep-sea vents and of the life around them represents an intersection of which two fields of science?

The study of deep-sea vents represents an intersection of geology (for studying the structures of the vents) and biology (for studying the life around them). Geologists study the geological processes that form the vents, while biologists study the unique life forms that thrive in these extreme environments.


What is the difference between geysers and deep-sea vents that form chimneys?

Geysers are hot springs that intermittently erupt boiling water and steam from underground due to pressure build-up, often in volcanic areas. Deep-sea vents, also known as hydrothermal vents, are fissures on the ocean floor that release superheated water enriched with minerals. Chimneys at deep-sea vents are structures formed by minerals precipitating out of the vent fluids, whereas geysers do not typically form chimneys.


How do ocean ridges and deep-sea trenches support the theory of sea floor spreading?

Ocean ridges and deep-sea trenches support the theory of sea floor spreading through the process of plate tectonics. At ocean ridges, new oceanic crust is formed as magma rises and solidifies, pushing the existing crust apart. Deep-sea trenches are areas where old oceanic crust is being subducted back into the mantle, completing the cycle of sea floor spreading. This continuous movement of crust at ridges and trenches provides evidence for the theory of sea floor spreading and the movement of tectonic plates.


What does the theory of plate tectonics suggest about the creation of deep sea trenches?

The theory of plate tectonics suggests that deep sea trenches are formed at subduction zones, where one tectonic plate is forced beneath another. This process occurs as a result of the movement of tectonic plates, leading to the creation of deep sea trenches through the process of plate convergence.


What does the theory of plate tectonics suggest about the creation of deep-sea trenches?

The theory of plate tectonics suggests that deep-sea trenches are formed at subduction zones where one tectonic plate slides beneath another. This process occurs due to the movement of the Earth's lithosphere, leading to the formation of these deep topographic features.

Related Questions

What is the temperatures at deep sea vents?

Some deep sea vents can be hotter than 300 degrees C.


How are deep-sea vents formed?

Volcanic eruptions


What is the temperature at a deep sea vent?

Some deep sea vents can be hotter than 300 degrees C.


What do geysers and deep-sea vents that from chimneys have in common?

ajhfahfuhgsdiuhguhds


Water released from deep-sea vents has been heated by?

hot rocks deep in the crust.


Chemosynthetic communities in the ocean can be found?

surrounding deep-sea hydrothermal vents


Why are hydrothermal vents helpful to the deep sea ecology?

Hydrothermal vents allow underground heat sources to warm the ocean bottom which is necessary to support deep see ecology.


Propose a question that a scientist might ask about the variety of organisms found around deep sea vents?

lol your scerwed i have the same question in my pearson succes thing


What sea creature has no lungs no brain and no mouth?

Tube worms which live near deep sea hydrothermal vents


The study of the structures of deep-sea vents and of the life around them represents an intersection of which two fields of science?

The study of deep-sea vents represents an intersection of geology (for studying the structures of the vents) and biology (for studying the life around them). Geologists study the geological processes that form the vents, while biologists study the unique life forms that thrive in these extreme environments.


What is the primary source of energy for organisms that live near deep-sea vents?

hydrogen sulfide


What is an alvinocaridid?

An alvinocaridid is a member of the Alvinocarididae, a variety of shrimp which inhabits deep-sea hydrothermal vents.