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The Hālona Blowhole was formed thousands of years ago during the period of volcanic activity in Oahu, [8] with Koko Crater 's lava flowing into the ocean. [9] The lava tubes extend into the ocean which are narrow at the top. [9] There is also a narrow rift along the base of the cliff which was formed by a large section of rock that broke away ...
Blowhole (geology) In geology, a blowhole or marine geyser is formed as sea caves grow landward and upward into vertical shafts and expose themselves toward the surface, which can result in hydraulic compression of seawater that is released through a port from the top of the blowhole. [1] The geometry of the cave and blowhole along with tide ...
Huge waves slam the cliffs near the Halona Blowhole, Friday, Aug. 24, 2018, in Waimanalo, Hawaii. As Hurricane Lane approaches Oahu. Large ocean swells impacted the coastline.
Koko Head. Koko Head is the headland that defines the eastern side of Maunalua Bay along the southeastern side of the Island of Oahu in Hawaii. On its western slope is the community of Portlock, a part of Hawaiʻi Kai. Koko Head (at 642 ft or 196 m) is an ancient tuff cone that is somewhat dwarfed by its neighboring tuff cone, Koko Crater, with ...
Comparison of free off-line satellite navigation software. This article contains a list with gratis (but not necessarily open source) satellite navigation (or "GPS") software for a range of devices (PC, laptop, tablet PC, mobile phone, handheld PC (Pocket PC, Palm)). Some of the free software mentioned here does not have detailed maps (or maps ...
Nakalele Point is a land mass on the eastern edge of the northern tip of the island of Maui in the state of Hawaiʻi. In Hawaiian, Nakalele or Nā-kālele means "the leaning". The Point is known for its blowhole and has become notable for its dangerous conditions when waves crash in. The point and blowhole are located just east of Poelua Bay.
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A blowhole is a cavity formed when a joint between a sea cave (formed by erosion) and the land surface above the cave becomes enlarged. The sea cave and the land surface become conjoined when the roof of the cave collapses. Blowholes are formed by the process of erosion. When waves enter the mouth of the cave they will be funneled up towards ...