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Download PDF by Voevodin, V.V: Álgebra lineal

By Voevodin, V.V

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There are bays in breached and drowned sinkholes on the limestones of the NW coast of Gozo in Malta. 28). Smoothly curved coastlines have formed where incoming refracted waves have shaped the outlines of depositional coasts, as on the Ninety Mile Beach and in Discovery Bay, SE Australia. 9). On some coasts the smooth curvature extends across cliffed sectors in soft rock formations as well as along the intervening beaches, as in Hawke Bay on the east coast of North Island, New Zealand, and Te Waewae Bay in South Island, New Zealand.

SW swell generated by gales south of Africa is transmitted across the Indian Ocean to the southern coasts of India and Sri Lanka and the western coast of Thailand. It reaches the southern coasts of Sumatra and Java, and other Indonesian islands as far east as Timor. SW swell originating south of Australia and New Zealand moves across the Pacific Ocean to coasts between Chile, California and Alaska. On the way it breaks on the shores of many Pacific islands. The stormy waters south of South America produce SW swell across the Atlantic Ocean to West Africa and Western Europe (Portugal to the Hebrides), and up to the south coast of Iceland.

The same is true of curved coasts beside the Caspian Sea, the Sea of Azov, the Red Sea, the Arabian Gulf and much of the Gulf of Mexico. 9) (Black and Rosenberg, 1992), or coastal lagoons such as Lake Wellington (Gippsland Lakes). Similar features are seen in the lagoons (termed limans) of the Ukrainian Black Sea coast. The curved outlines are determined by the resultant directions of waves that come from various directions, and are orthogonal to the maximum fetch. There may be secondary smoothing 20 CH 2 COASTAL PROCESSES by longshore currents, generated by waves coming in on either side of the maximum fetch and causing longshore movements of beach sediment.

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Álgebra lineal by Voevodin, V.V


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