(1) Geheimnis: German, Italian as confidential. ( 2 ) the Atacama Trench : also known as Peru - Chile trench or trench eastern Pacific. South Pacific eastern edge of the deep trench. Extends from north to south, from the northern coast of Peru and Chile about 160 km. Length of 5,900 km, with an average width of 100 km, the deepest located at latitude 23-18 ', longitude 71-41 ', 8,064 meters deep. (3) "DieValkyrise", " speeding Valkyrie ": " speeding of the Valkyries" is the opera " The Valkyrie " (DieValkyrise) Chapter famously music, also known as Flight of the Valkyries, the performance of the Valkyries who riding a winged horse ride in the sky between the image of nike air max 1 weapon in the lightning flashes and thunder of laughter nike air max 95 weird hybrid of a...... in this music, Wagner give full play to the trombone, trumpet mainly brass sound, the band's accompaniment, brilliant sound performance of the Valkyries metal flying in the air of the elegant and chic, with a strong sense of mythology and space.
(4) PerCurrent: Peru cold (PerCurrent) also known as the Humboldt cold, cold is the most powerful one. nike air max 90 Starts latitude 45 - so romantic West, close to the west coast of South America, after Chile, Peru, Ecuador and other countries until the equatorial waters of the north, near the Galapagos Islands, 3700 to 5500 km long ocean currents, more than 370 kilometers wide, the flow rate 0.9 kilometers per hour. In the northward flow of the process, due to the Coriolis force effect, to be prevailing southerly and southeasterly winds along the coast, surface waters off the west coast, so that the average of the middle 100 meters per second on the pan of cold water to the surface water temperature is very low.
As the water on the pan brought a lot of nitrate,nike air max 95, phosphate and other nutrients made to promote plankton blooms, provide a rich food for fish, so the coast of Peru became world famous fishing grounds. As the water continuity and incompressible characteristics of a marine area of seawater density differences due to wind or other reasons stream left, adjacent sea to replenish the water to flow to form compensating stream. Compensation streams have horizontal or a vertical. Compensation stream is divided into vertical upwelling and downwelling.
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