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Where did the deep sea drilling project take place?
Between South Africa and South America
What is a deep sea vent?
i love this wedsite
A sentence for the word sponge?
The sea sponge was my oceans project topic. The sponge was so absorbent!
Why deep sea divers not using ordinary air?
Because they have a air tank to help them breath.
What deep sea animals are herbivores?
The Dugong, Manatee, Sea Horse, Leafy Dragon, Weedy dragon, and Parrot Fish are examples.A few more are:Green Sea TurtleSea UrchinPerwinkleSea SlugCoral ReefStellers Sea Cow
When did the deep sea drilling project take place?
in 1968
How long did the deep sea drilling project last?
15 years
What has the author Patricia Paluso written?
Patricia Paluso has written: 'A guide to publications and subsequent investigations of Deep Sea Drilling Project materials' -- subject(s): Bibliography, Deep Sea Drilling Project, Marine sediments, Paleontology
Where did the deep sea drilling project take place?
Between South Africa and South America
What is commonly used to determine the age of seafloor samples recovered by the deep-sea drilling project?
Radiometric dating using isotopes of elements such as potassium and argon is commonly used to determine the age of seafloor samples recovered by the deep-sea drilling project. This method calculates the age by measuring the ratio of parent to daughter isotopes in the samples.
What were the deep sea drilling project results?
The Deep Sea Drilling Project (DSDP), initiated in 1968, significantly advanced our understanding of the Earth's geology and oceanic processes. It provided crucial data on the age and composition of the ocean floor, confirming theories of plate tectonics and continental drift. The project recovered sediment cores that revealed climate change patterns and oceanic conditions over millions of years. Overall, DSDP laid the groundwork for subsequent oceanographic research and exploration initiatives, such as the Ocean Drilling Program.
What was the glomar challenger?
The Glomar Challenger was a deep-sea research vessel launched in 1968, primarily used for the Deep Sea Drilling Project (DSDP) conducted by the Scripps Institution of Oceanography. It played a crucial role in advancing the understanding of oceanic geology and plate tectonics by drilling into the ocean floor to collect core samples. The data obtained from these drilling expeditions provided significant insights into the Earth's history, continental drift, and the formation of oceanic crust. Its legacy continues to influence oceanographic research today.
What is the importance of the discovery of deep-sea drilling in understanding the current theory of plate tectonics?
The discovery of deep-sea drilling is important in understanding plate tectonics because it provides direct evidence of the movement of Earth's tectonic plates. By studying the rock samples obtained from deep-sea drilling, scientists can analyze the age and composition of the oceanic crust, which supports the theory of plate tectonics and helps explain how the Earth's surface is constantly changing and evolving.
Data collected by the drilling ship glomar challenger confirmed that?
Glomar Challenger was a deep sea research and scientific drilling vessel for oceanography and marine geology studies.
Where is basalt stone found?
Basalt is found in the mid-ocean islands and surrounding regions of the Hawaiian Islands and Iceland, as found by samples of lava flows found in drill cores recovered by vessels of the Deep Sea Drilling Project.
What was the name of the ship that drilled holes in the sea floor?
The ship that drilled holes in the sea floor is known as the "Glomar Challenger." It was used for the Deep Sea Drilling Project from 1968 to 1983, facilitating significant advancements in oceanic and geological research. The Glomar Challenger played a crucial role in understanding the structure and history of the ocean floor.
Early results of the deep sea drilling project clearly justified the conclusion that?
the theory of plate tectonics was confirmed, as drilling samples showed that the Earth's crust is composed of several distinct plates that are in constant motion. This provided key evidence supporting the idea of continental drift and the dynamic nature of the Earth's surface.
