Drainage Basin

The land based part of the hydrological cycle is called the Drainage Basin System. A drainage basin is the name given to the area of land which is drained by a river. When water reaches the surface there are a number of routes which it may take in its journey to reach the river. These are shown in the diagram .

Drainage Basins have a number of distinct features . The edge of a drainage basin is characterised by the highest points of land around the river, this is known as the watershed. The point at which a river starts is called its source. As the river continues to flow down stream it may be joined by smaller rivers called tributaries. The point at which these smaller rivers join the main river is known as a confluence. As the river continues its journey, eventually reaches the sea – the point where the river flows into the sea is known as the river mouth.

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New View of Tectonic Plates Through Computer Modeling of Earth’s Mantle Flow, Plate Motions, and Fault Zones

Plate boundaries, which can be seen as narrow red lines are resolved using an adaptively refined mesh with 1km local resolution. Shown are the Pacific and the Australian tectonic plates and the New Hebrides and Tonga microplates. (Credit: Georg Stadler, Institute for Computational Engineering & Sciences, UT Austin)

Computational scientists and geophysicists at the University of Texas at Austin and the California Institute of Technology (Caltech) have developed new computer algorithms that for the first time allow for the simultaneous modeling of Earth’s mantle flow, large-scale tectonic plate motions, and the behavior of individual fault zones, to produce an unprecedented view of plate tectonics and the forces that drive it.

A paper describing the whole-earth model and its underlying algorithms will be published in the August 27 issue of the journal Science and also featured on the cover.The work “illustrates the interplay between making important advances in science and pushing the envelope of computational science.

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Sinabung erupts in Sumatra

Mount Sinabung volcano on Sumatra erupted shortly after midnight local time on 29 August 2010, producing lava and throwing ash 1500 metres above the summit. Local inhabitants fleeing their homes have spoken of ’thick black smoke, small stones and sulphur’ being produced by the volcano, according to AFP: one local man reportedly died as a result of breathing difficulties suffered during the eruption.

Mount Sinabung is a 2460-metre stratovolcano in northern Sumatra, about 60 km SW of the city of Medan. An uncertain eruption is given by the Global Volcanism Program for 1881 and sulphurous gas emissions were apparently reported from the summit in 1912, but there are no historical records of confirmed eruptive activity.

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Gems and The Moh’s Scale

In the old days, people believed gems held magical powers. Gems are very valuable.

Diamond is the hardest naturally occurring substance with a hardness of 10. Its crystal system is cubic because it has 4 equidistant neighboring crystals. Its specific gravity is 3.5. The word diamond means adamas in Greek, meaning “unconquerable”. That’s why Napoleon wanted the Regent, or Pitt diamond set into the hilt of his sword.

Topaz-the name for this substance is a misnomer. The word topaz actually means Zabargad in Greek, which is an island in the Red Sea, a source of peridot. Topaz’s crystal structure is orthorhombic. The hardness of topaz is 8, though it can be broken easily due to its 1 perfect direction of cleavage. The specific gravity is 3.52-3.56, which is very close to diamond’s.

Tourmaline is a very interesting gem. It has a trigonal crystal system and a hardness of 7-7.5. Its specific gravity is 3-3.25. What is really interesting is that if this gem was heated, one side would be positively charged, the other negatively. That’s why there is a watermelon tourmaline. Since it can produce electricity, it has a tendency to attract dust.

Quartz is really just silicon dioxide. Quartz is an igneous rock and its hardness is 7. Its crystal system is trigonal and its specific gravity is 2.65. Quartz is hard to break and has no cleavage. Quartz is the main percentage of dust. Therefore, dust can damage gems with a hardness of 6.99 and lower. Quartz is only pure when it is colorless. Rose quartz has iron and titanium too. Smoky quartz has aluminum.

The Moh’s Scale

The Moh’s Scale is the scale that organizes the rocks in order of hardness with 10 being the hardest and 1 the softest. In other words, diamond is the hardest and talc is the softest. This is an easy way to see which rocks are harder than others.

The Moh’s Scale is not to scale though. Diamond is a lot harder than corundum but corundum isn’t much harder than quartz.

1. Talc

2. Gypsum

3. Calcite

4. Flourite

5. Apatite

6. Orthoclase

7. Topaz

8. Quartz

9. Corundum

10. Diamond

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