Koʻolau Range

Koʻolau Range is a name given to the dormant fragmented remnant of the eastern or windward shield volcano of the Hawaiian island of Oʻahu. It was designated a National Natural Landmark in 1972.[3]

Koʻolau Range
View of Koʻolau Range from offshore Lanikai (windward coast)
Highest point
Peak	Konahuanui
Elevation	3,150 ft (960 m) [1]
Prominence	2,303 ft (702 m) [2]
Listing
Coordinates	21°27′0″N 157°54′0″W
Geography
Koʻolau Range Hawaiian Islands
Location	Oahu, Hawaii, US
Parent range	Hawaiian Islands
Topo map	USGS Kilohana (HI)
Geology
Age of rock	1.7 Ma
Mountain type	Dormant shield volcano
Volcanic arc/belt	Hawaiian-Emperor seamount chain
Last eruption	32,000 - 10,000 BP
Climbing
Easiest route	trail
U.S. National Natural Landmark
Designated	1972

Geology

It is not a mountain range in the normal sense, because it was formed as a single mountain called Koʻolau Volcano (koʻolau means "windward" in Hawaiian, cognate of the toponym Tokelau). What remains of Koʻolau is the western half of the original volcano that was destroyed in prehistoric times when the entire eastern half—including much of the summit caldera—slid cataclysmically into the Pacific Ocean. Remains of this ancient volcano lie as massive fragments strewn nearly 100 miles (160 km) over the ocean floor to the northeast of Oʻahu. Kāneʻohe Bay is what remains of the ancient volcano's summit caldera after the slide. The modern Koʻolau mountain forms Oʻahu's windward coast and rises behind the leeward coast city of Honolulu — on its leeward slopes and valleys are located most of Honolulu's residential neighborhoods.

View of Koʻolau Range from the top. Kāneʻohe is visible on the right side.

The volcano is thought to have first erupted on the ocean floor more than 2.5 million years ago. It eventually reached sea level and continued to grow in elevation until about 1.7 million years ago, when the volcano became dormant. The volcano remained dormant for hundreds of thousands of years, during which time erosion ate away at the initially smooth slopes of the shield-shaped mountain; and the entire mass subsided considerably. The highest elevation perhaps exceeded 3,000 meters (9,800 ft); today, the summit of the tallest peak, Puʻu Konahuanui is only 945 meters (3,100 ft).

Honolulu Volcanics

Main article: Honolulu Volcanics

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 Volcanics.[4] According to the US Geological Survey, the most recent eruptions in this series of activity occurred between about 70,000 to 100,000 years ago.[5] There is a possibility that Koʻolau volcano could erupt again; however, the chance of such an eruption occurring in "our lifetimes, or even those of many future generations" is remote.[5]

Transportation

There are three roads that tunnel through the southern part of the Koʻolau Range, connecting Honolulu to the Windward Coast. From leeward to windward:

• Hawaii Route 61 (Pali Highway)
• Hawaii Route 63 (Likelike Highway)
• Interstate H-3

Gallery

• 
  View of Koʻolau Range with Koko Crater and Maunalua (Hawaii Kai) visible.
• 
  Nuʻuanu Pali, a section of the Koʻolau Range. (Click to enlarge)

References

1. "Koolau Range". Peakbagger.
2. "Konahuanui". Peakbagger.
3. "National Natural Landmark". National Park Service. Retrieved 12 December 2012.
4. "Xenoliths in the Honolulu Volcanic Series, Hawaii". Oxford University Press. 3 February 1970. Retrieved 2014-09-25.
5. "A geologic tour of the Hawaiian Islands: O'ahu". Hawaiian Volcano Observatory. US Geological Survey. 14 January 2016. Retrieved 23 October 2019.