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It is a historically important site on the North Shore, as well as providing a view of Waimea Bay and the Waianae Mountain range. Waimea Bay is located along Kamehameha Highway. The bay is on the north-west side of the highway (at the entrance point). The Waimea Bay shoreline has been experiencing erosion due to both man made and natural causes ...
Traditional land divisions in ancient Hawaii were agricultural units that ran from the seashore to mountains. The shoreline areas of Kapālama were later developed into part of Honolulu harbor. The upland areas of Kapālama developed into ‘Ālewa Heights, and the main campus of Kamehameha Schools. [4]
The area was named after the dominating geological feature Kohala Mountain, [3] the oldest of Hawaiʻi Island's five major volcanic mountains. The current districts cover the north and western sides of the mountain, 20°7′55″N 155°47′38″W / 20.13194°N 155.79389°W / 20.13194; -155.
Diurnal wind system variation in the Appalachian mountain range. Mountain and valley breezes form through a process similar to sea and land breezes. During the day, the sun heats up mountain air rapidly while the valley remains relatively cooler. Convection causes it to rise, causing a valley breeze. At night, the process is reversed.
In 1850 an American doctor and missionary Dr. Gerrit P. Judd purchased 622 acres of ranch land at Kualoa for $1300, and also the island of Mokoliʻi just offshore, from King Kamehameha III. Dr. Judd was the first person to translate medical journals into the Hawaiian language for King Kamehameha and so the king was very grateful for his works.
The depth of the actual valley walls at the seashore range from 300 m (1,000 ft) at the Waipiʻo Valley Lookout at the southeastern corner of Kohala mountain, to a high of over 500 m (1,600 ft) in Honopue, then diminishing to less than 150 m (490 ft) at Pololu Lookout at the northern end of the valleys.
California's mountain ranges influence the climate as well: moisture-laden air from the west cools as it ascends the mountains, dropping moisture; some of the rainiest parts of the state are west-facing mountain slopes. Northwestern California has a temperate climate with rainfall of 15 inches (380 mm) to 50 inches (1,300 mm) per year.
The Hawaiian–Emperor seamount chain is a mostly undersea mountain range in the Pacific Ocean that reaches above sea level in Hawaii.It is composed of the Hawaiian ridge, consisting of the islands of the Hawaiian chain northwest to Kure Atoll, and the Emperor Seamounts: together they form a vast underwater mountain region of islands and intervening seamounts, atolls, shallows, banks and reefs ...