Kaʻena Ridge, also referred to as the Kaʻena Volcano, is a submerged remnant of an ancient shield volcano that is to the north of and once comprised the northern section of the Hawaiian Island of Oʻahu.
Kaʻena Ridge | |
---|---|
Kaʻena Ridge Location of Kaʻena Volcano in the Hawaiian Islands | |
Highest point | |
Elevation | −3,937 ft (−1,200 m) |
Coordinates | 21°49′19″N 158°46′19″W |
Geography | |
Location | Hawaii US |
Geology | |
Mountain type | Submerged shield volcano |
Last eruption | Pleistocene |
Ka'ena Ridge was the oldest of the three volcanoes to form Oahu and it was also the shortest when it grew out of sea level. It was about 3,000 ft.[1]
Activity from Kaʻena began roughly 5 million years ago.[2][3] Despite being Oahu's oldest volcano, it broke sea level 400,000 years after the Waiʻanae did.[2] This is due to Kaʻena being built on a lower sea depth, whereas other Oahu volcanoes were built on pre-existing ridges.[3]
Around 3 million years ago, Kaʻena, Waiʻanae and Koʻolau were simultaneously emerged. Kaʻena would later submerge below sea level at an unknown date.[2]
In its current state, the crest of the Ka'ena Ridge extends 35-55 km wide and is located 75-100 km northwest of Kaena Point, the westernmost tip of Oahu.[4]
Hawaiian volcanism topics (list) | ||
---|---|---|
Windward Isles |
| |
Leeward Isles | ||
Emperor Seamounts |
| |
Notable eruptions and vents |
| |
Topics |
|
This Hawaiʻi state location article is a stub. You can help Wikipedia by expanding it. |
This volcanology article is a stub. You can help Wikipedia by expanding it. |