Kerguelen Plateau, Southern Indian Ocean: Geologic History of a Large Igneous .
The Kerguelen Plateau is an upraised region of the seafloor that is located in the southern Indian Ocean. Up until 1988 little was known about this underwater plateau except for the hypothesis of scientists" that believed this plateau had been formed by volcanic eruptions, and at one point in history actually existed above-sea-level heights. It was not until a drilling operation, conducted by Ocean Drilling Program (ODP) drill ship JOIDES visited the Kerguelen Plateau that those hypothesis were proven accurate.
A Large Igneous Providence (LIP) is formed when magma wells up from deep beneath Earth's surface and forms molten rock. Scientist's discovered through drilling that there is not a specific time period that it takes an (LIP) to form, but rather different parts of an (LIP) can form at different times. For example, with the Kerguelen Plateau rock samples taken from different areas proved that some were as old as 110 million years, where as samples taken from other areas were only 35 million years old. Evidence recovered showed that the Kerguelen Plateau was once above sea-level, but became submerged over millions of years. Examples of other (LIPS) are Hawaii and Iceland. Hot spots are thought to be connected to a stable pattern of upwardly flowing pumes of warmer than average material from deep levels of the mantle. (LIPS) are extremely important for many reasons, in the case of the Kerguelen Plateau the most important is that by studying the Plateau scientists can get a direct and simple form of reference to reconstruct plate motions during the opening of the Indian Ocean.
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The Kerguelen Plateau lies in the remote sub Antarctic region of the Indian Ocean. At 2500 kilometers in length, the Kerguelen Plateau resembles Argentina in size and length. The Plateau was not formed by one massive volcanic event, but rather several intense episodes of volcanic eruptions.
This is wear the Deccan Plateau, The Easter and Western Ghats and the warm shores of the southern coasts of India. The Deccan Plateau is mostly made up of factories and plantations that make masses of products to sell to other countries. ... The last of the main river types of India are the Eastern Flowing Rivers of the Deccan Plateau. These rivers are formed up in the hills of the Deccan Plateau and flow eastward to the Bay of Bengal. ... This is the southern part of India and includes the Deccan plateau. ...
All three tribes have lived on the Columbia River Plateau for over 10,000 years (Tamástslikt). ... The Plateau culture groups call themselves bands, instead of tribes. ... The Umatilla tribe is part of a much larger culture group called the Plateau Culture. ... The Plateau cultures had a very distinctive type of dwelling called the "longhouse". ... The Umatilla Tribe and other plateau people began crossing the Rocky Mountains to the Great Plains to hunt for buffalo, while maintaining their traditional migratory patterns. ...
The rise period is followed by the fifth and final plateau period when the accumulation of phage particles ceases. This plateau can be seen as the latent period of the following multiplication cycle (Flint, 2000). ... Three of these periods - the latent period, the rise period and the plateau period -- are easily pictured using a plot of PFU/mL bacteria vs. elapsed time. ...
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The center of Spain forms a vast plateau extending from the Cantabrian Mountains in the north to the Sierra Morena in the south, and from the Portuguese border in the west. Except for some fertile valleys, the central plateau is arid and thinly populated. ...
DAY 1 The first day there wasn't much time to do anything, but I filtered the yellow stuff out of the mixture. I am pretty sure that it was sulfur. It didn't have much of an odor, but the mixture itself smelled like rubbing alcohol, isopropanol. DAY 2 On this day, I did fractional distillation ...