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Kohala is 606 km 2 (234 sq mi) in area and 14,000 km 3 (3,400 cu mi) in volume, and thus constitutes just under 6% of the island of Hawaii. [1] Kohala is a shield volcano cut by multiple deep gorges, which are the product of thousands of years of erosion. Unlike the typical symmetry of other Hawaiian volcanoes, Kohala is shaped like a foot.
After hundreds of thousands of years of dormancy, Koʻolau volcano began to erupt again. Some thirty eruptions over the past 500,000 years or so have created many of the landmarks around eastern Oʻahu, such as Diamond Head, Koko Head (Hanauma Bay), Koko Crater, Punchbowl Crater, Tantalus, and Āliapaʻakai, and are collectively known as the Honolulu Volcanic Series, or simply Honolulu ...
Kohala (Hawaiian pronunciation:) is the name of the northwest peninsula of the island of Hawaiʻi in the Hawaiian Archipelago. In ancient Hawaii it was often ruled by an independent High Chief called the Aliʻi Nui. In modern times it is divided into two districts of Hawaii County: North Kohala and South Kohala.
By 1937, the Kohala Sugar Company had consolidated into the mill at Māhukona, and became Mahukona Terminals Ltd. In 1941 the port closed for World War II. On October 29, 1945, the railroad closed. [4] The town, which once consisted of about 40 families, was abandoned in the 1950s. [11] In 1956 the harbor was closed.
The Hawaiʻi hotspot is a volcanic hotspot located near the namesake Hawaiian Islands, in the northern Pacific Ocean.One of the best known and intensively studied hotspots in the world, [1] [2] the Hawaii plume is responsible for the creation of the Hawaiian–Emperor seamount chain, a 6,200-kilometer (3,900 mi) mostly undersea volcanic mountain range.
ʻUpolu Point is the most northern point on the island of Hawaiʻi in the Hawaiian Islands. [1] It is an extruding landform created by cooled lava from an old eruption from Kohala volcano.
The oldest volcano on the island, Kohala, is more than a million years old, [17] while Kīlauea, the youngest, is between 300,000 and 600,000 years of age. [16] Kamaʻehuakanaloa (the ruddy, reddish child of Kanaloa, [18] formerly Lōʻihi), on the island's flank, is younger and has yet to breach the surface. [19]
Like the neighboring Koʻolau, the Waiʻanae Range is not a mountain range in the sense most people are familiar with, as the mountain range as a whole was created from a single volcano rather than plate tectonics. The oldest lava dated from the volcano are about 3.9 million years old. About 3.2 million years ago, the volcano's activity changed ...
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