An exploration of underwater life

Mickens The Earth is an ocean planet—more than 70 percent of the surface is covered by seawater.

An exploration of underwater life

So where did the idea come from?

Mapping the characteristics of the ocean basin has been difficult for several reasons. Researchers in the field define and measure such properties; prepare maps in order to identify patterns; and utilize these maps, measurements, and theoretical models to achieve a better grasp of how the Earth works as a whole.

Although its main goal was to search for deep-sea life by means of net tows and dredging, the findings of its physical and chemical studies expanded scientific knowledge of temperature and salinity distribution of the open seas.

An exploration of underwater life

Moreover, depth measurements by wire soundings were carried out all over the globe during the expedition. Investigators have produced global maps showing the distribution of surface winds as well as of heat and rainfall, which all work together to drive the ocean in its unceasing motion.

They have discovered that storms at the surface can penetrate deep into the ocean and, in fact, cause deep-sea sediments to be rippled and moved.

Earle, SylviaLearn about the pioneering life and work of American oceanographer and explorer Sylvia Earle. Without the moderating effect of the ocean, the steadily increasing input of carbon dioxide into the atmosphere due to the extensive burning of coal, oil, and natural gas would result in the rapid onset of the so-called greenhouse effect —i.

The field of marine biology has benefitted from the development of new sampling methods. Among these, broad ranging acoustical techniques have revealed diverse fish populations and their distribution, while direct, An exploration of underwater life up observation made possible by deep-sea submersibles has resulted in the discovery of unusual and unexpected species and phenomena.

In the area of geologyundersea exploration of the topography of the seafloor and its gravitational and magnetic properties has led to the recognition of global patterns of continental plate motion.

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These patterns form the basis of the concept of plate tectonicswhich synthesized earlier hypotheses of continental drift and seafloor spreading.

Earth scientists found that the mid-ocean centres of seafloor spreading also are sites of important metal deposits. The hydrothermal circulations associated with these centres produce sizable accumulations of metals important to the world economy, including zinc, copper, lead, silver, and gold.

Rich deposits of manganese, cobalt, nickel, and other commercially valuable metals have been found in nodules distributed over the entire ocean floor. The latter discovery proved to be a major factor in the establishment of the Convention of the Law of the Seawhich calls for the sharing of these resources among developed and developing nations alike.

Exploitation of these findings awaits only the introduction of commercially viable techniques for deep-sea mining and transportation. Basic elements of undersea exploration Platforms Undersea exploration of any kind must be conducted from platforms, in most cases, ships, buoys, aircraft, or satellites.

Typical oceanographic vessels capable of carrying out a full complement of underwater exploratory activities range in size from about 50 to metres.

An exploration of underwater life

They support scientific crews of 16 to 50 persons and generally permit a full spectrum of interdisciplinary studies. It has a displacement of 2, tons and can carry 25 scientists in addition to 25 crew members.

It is powered by a dual cycloidal propulsion system, which provides remarkable manoeuvrability. A converted commercial drill ship, it measures metres in length, has a displacement of 18, tons, and is equipped with a derrick that extends 62 metres above the waterline see photograph.

A computer-controlled dynamic positioning system enables the ship to remain over a specific location while drilling in water to depths as great as 8, metres. The drilling system of the ship is designed to collect cores from below the ocean floor; it can handle 9, metres of drill pipe.

Deep-sea exploration - Wikipedia

The vessel thus can sample most of the ocean floor, including the bottoms of deep ocean basins and trenches. It can operate in waves as high as eight metres, winds up to 23 metres per second, and currents as strong as 1.

It has been outfitted for use in ice so that it can conduct drilling operations in high latitudes. The ship can accommodate 50 scientists as well as the crew and drilling team, and its geophysical laboratories total nearly square metres.

It is a long narrow platform that is towed in a horizontal position to a research site. Once on location, the ballast tanks are flooded to flip the ship to a vertical position. Only 17 metres of the ship extend above the waterline, with the remaining 92 metres completely submerged.

The rise and fall of the waves cause a very small change in the displacement, resulting in a high degree of stability. This design type requires the use of twin submerged, streamlined hulls to support a structure that rides above the water surface.

The deck shape is entirely unconstrained by the hull shape, as is the case for conventional surface vessels. Ship motion is greatly reduced because of the depth of the submerged hulls.

For a given displacement, a SWATH-type vessel can provide twice the amount of deck space that a single-hull ship can, with only 10 percent of the motion of the single-hull design type.

In addition, a large centre opening, or well, can be used to display and recover instruments. Navigation Exploration of any kind is useful only when the location of the discoveries can be noted precisely.

Thus, navigation has always been a key to undersea exploration. There are various ways by which the position of a vessel at sea can be determined.The JIP was formed in to identify, conduct and support research to further to improve the scientific understanding of the potential impact of Exploration and Production (E&P) sound on marine life.

David Gallo shows jaw-dropping footage of amazing sea creatures, including a color-shifting cuttlefish, a perfectly camouflaged octopus, and a Times Square's worth of neon light displays from fish who live in the blackest depths of the ocean.

This short talk celebrates the pioneering work of ocean explorers like Edith Widder and Roger Hanlon. Canadian Invasion. We all have our reason(s) for finding our way to the water, for some it is a bucket list experience, for others it is a hobby to enjoy from time to time, and finally there are those it is a life changing part of who they are and it embeds into their DNA.

A hydrothermal vent is a fissure in a planet's surface from which geothermally heated water issues.

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Hydrothermal vents are commonly found near volcanically active places, areas where tectonic plates are moving apart at spreading centers, ocean basins, and hotspots.

Hydrothermal vents exist because the earth is both geologically active and has large amounts of water on its surface and within. Space Exploration For A Better Life For Mankind The whole idea of getting to know the space and it secrets and how it can benefit mankind is what space exploration is all about.

The need for exploring the space is as important as with the help of the information got we can help save a large number of lives and property through medical advancements. Deep-sea exploration advanced considerably in the s thanks to a series of technological inventions, ranging from sonar system to detect the presence of objects underwater through the use of sound to manned deep-diving submersibles such as DSV Alvin.

BBC - Future - Will we ever live in underwater cities?