Showing posts with label ancient coral reef. Show all posts
Showing posts with label ancient coral reef. Show all posts

Saturday, January 10, 2015

Ancient Karst Reef Sinkholes On The Ewa Plain Hold Secrets To Oahu’s Earliest Residents

Looking Back by Looking Down 

By Chad Pata, August 22, 2014  Go Kapolei Magazine


In general, sinkholes are created over centuries as the acidity of rainwater eats away at the limestone, causing underground caverns to form and eventually give way to the weight of the earth above them.

Here in Kapolei, anyone who has ever put a shovel in the ground knows that the entire plain is made up of an ancient reef that dried up as ocean waters receded 120,000 years ago. This weathered karst, as it is known, is a limestone substrate that through the centuries was eaten away by the rains creating thousands of vertical bell-shaped caves or sinkholes.

While they are—geologically speaking—of some interest, their true value comes from their unintended ability to serve as a trap for animals. Due to their vertical nature, once a creature found itself in such a place, there was little chance of escape as scaling the walls was impossible and rare is the bird that can hover straight up like a helicopter to escape these narrow confines.

So what we had was a perfect repository to collect fossils of the wildlife that occupied these islands long before the Polynesians ever set foot on this volcanic chain.

Unfortunately, 99 percent of these “fossil tombs” have either been bulldozed for agricultural lands, lain over with concrete for development or simply lost to the ever-shifting sands of time, which brings us back to our little six-acre plot in Kapolei.

They were first discovered in the 1970s by Jennie Peterson, an archaeologist with Bishop Museum, as she was doing an environmental impact study on the once-proposed Deep Draft Harbor, but the history of the sinkholes would be written by local zoologist Dr. Alan Ziegler who spent decades exploring, documenting and teaching others about the wonders to be found out here on the Plain.

Eventually, the Smithsonian got involved with the project and the preeminent avian paleontologists Storrs Olson and Helen James came in to examine the remains.

What they found was astounding. More than 40 extinct species were interned in the sinkholes and of whose existence no one had known until they were discovered here.

There were remains of sea eagles and hawks, flightless rails and finches, and most shocking of all the moa nalo, which in Hawaiian means “lost fowl.” It was a three-foot tall flightless goose-like duck with a head like a tortoise. Many of the remains were in articulated form, as they had most likely died in the sinkhole after having fallen in, giving scientists an unadulterated look into our distant past.

“Back in the day, with all these birds, it must have been quite a raucous place!” says Marjorie Ziegler, daughter of Alan and executive director for the Conservation Council for Hawai‘i who hopes to oversee the care of the preserve one day.

Many of these remains now reside in Washington, D.C. at the Smithsonian and while the important artifacts have been removed, there is still much for future generations to learn at this holdover from pre-human contact Hawai‘i.

For years the CCH and Hawai‘i Nature Center led tours to the sinkholes, allowing children a chance to play archaeologists for a day. Ladders would be set up, many of the holes are 8-feet deep, and the kids would descend into the depths to use trawls, scoop sand and bring buckets of it to the surface.


Here they would use screens to discover the bones of Hawaiian petryls, the ‘ua‘u, that is only found on neighbor islands now and the beaks of long-gone crows who used to call O‘ahu home. They would always return the remains to the sinkhole to allow the next group to discover them.

But in recent years, invasive species of plants have overgrown the property, the holes are obscured by weeds making it difficult to find them or, even worse, hard to see their openings until you are falling into one.

The sea air and vandals have ravaged the fencing; and while still protected on paper, Ziegler is concerned about what could happen to this valuable natural resource.
“I worry less about homeless people setting up camp in there than about the accidental bulldozer collapsing them,” says Ziegler.

The holdup on the turnover of the land to the DLNR is a modern-world one.

The property cannot be conveyed until the surrounding land is subdivided and the subdivision cannot happen until there is improved road access to the surrounding industrial park development. This development, named Kapolei Harborside is planned to happen over the next decade, so while the plan is still to turn the land over to the DLNR, it may be some time before the public gets to visit this important bit of our area’s history.

When this lot at the corner of Malakole and Hanua streets is officially turned over, Ziegler and her team at CCH have big plans for the sinkholes starting with clearing the land of all the invasive species, including many large kiawe trees, and marking the sinks so that the visitors can be safe when visiting.

Next will be to build an educational area where kupuna can talk about these extinct species before kids go visit the sinkholes. And here, Ziegler’s visions can finally be realized, as amongst the remains our ancient past, the minds of our future can grow.

For more on the Conservation Council for Hawai‘i, log on to www.conservehi.org





SINKHOLE BIRDS THAT ARE EXTINCT

Extinct species of birds from sinkholes on the 'Ewa Plain:

Pterodroma jugabilis, a medium-sized petrel
Thambetochen xanion, a large flightless species of waterfowl (moa nalo)
Branta (uncertain species), a weak-flying goose, closely related to the nene
Porzana ziegleri, a small flightless rail
Porzana ralphorum, a large flightless rail
Circus dossenus, a small harrier, apparently adapted to feed on forest birds
Grallistrix geleches, a long-legged, bird-eating owl
Corvus impluviatus, a raven-sized crow with a deep, arched bill
Corvus viriosus, a raven-sized crow with a long, straight bill
Myadestes oahuensis, the O'ahu thrush
Moho apicalis, the O'ahu 'o'o (a honeyeater)
Chaetoptila (related to) angustipluma, a large honeyeater
Telespiza persecutrix, a small finch similar to the Laysan and Nihoa finches
Chloridops wahi, a grosbeak finch similar to the extinct Kona finch of the Big Island.
Chloridops regiskongi, a grosbeak finch with a really large bill, nicknamed King Kong finch.
Rhodacanthis litotes, similar to the extinct koa-finches of the Big Island.
Xestospiza fastigialis, a finch with a conical bill that was once common on O'ahu, Moloka'i and Maui.
Hemignathus upupirostris, an 'akialoa (Hawaiian honeycreeper with a long, thin, decurved bill)
Aidemedia chascax, a Hawaiian honeycreeper with a long, straight bill
Aidemedia zanclops, a Hawaiian honeycreeper with a sickle-shaped bill
Ciridops (uncertain species), a short-billed, strong-legged Hawaiian honeycreeper of a type previously known only from the Big Island.

SINKHOLE BIRDS STILL THRIVING

Sinkhole birds that are not extinct:

Pterodroma sandwichensis, the Hawaiian petrel; not previously known from O'ahu but bones are abundant in the sinkholes, showing that the region once had a major colony.
Haliaeetus (related to) albicilla, the white-tailed sea eagle. These eagles were either resident in the Islands or were regular visitors in the past. (A sea eagle was spotted on Kaua'i and possibly on O'ahu late last year and earlier this year.)
Telespiza cantans, the Laysan finch, known historically only from Laysan Island.
Loxioides bailleui, the Palila, known historically only from high-elevation Big Island mamane-naio forest.

Source: Helen James, Smithsonian Institution


Oahu's Ewa Plain Karst Sinkholes And Caves Yield Extinct Bird Fossils

US Fish Wildlife Demonstrates How 

Ewa Plain Karst Can Be Restored










Thursday, December 25, 2014

The Ewa Plain Karst is the largest of several karsts on the island of Oahu

The Ewa Plain Karst is the largest of several karsts on the island of Oahu

Yet one of the least known! (The reason: Ewa developers oppose studies)



Anne Wiley, Michigan State University doctoral student, left, and Andreanna Welch, doctoral student at the University of Maryland, look around in an Ewa sinkhole 

Despite its impressive extent and archaeological and palaeontological values, the Ewa Karst is almost entirely unknown to karstographers and speleologists. 

(Pre-printed from The Cave Conservationist - February 1998)


The Ewa Karst is the largest of several karsts on the well-populated island of Oahu, yet one of the least known (Halliday, 1994). Its exact dimensions are uncertain because geological maps show considerable upslope areas as alluvium and some shore areas as sand. 

However it clearly covers at least 50 km2 in the southwest corner of the island of Oahu (Figure 1). It is a semitropical littoral karst formed on porous, permeable algal and coralline reef deposits formed during at least three high stands of sea level (Figure 2), perhaps with a higher content of sand-sized clasts of foraminifera than contemporaneous Caribbean deposits (Chester Lao, written communication, 1997). 

Some artesian flow is said to be present, confined by clay layers (Chester Lao, oral communication, 1997). The U.S. Geological Survey Ewa Quadrangle shows numerous sinking streams and closed depressions within the Karst. Some of the former are artificial: the result of past water diversion for farming, ranching and domestic use. Some of the depressions are man made also. Most of the land surface of the karst has been subjected to more than a century of extensive reworking by man.

In 1955, the late Harold S. Palmer (Professor of Geology at the University of Hawaii) told me he had seen a meter-long stalactite said to have come from a cave in the Ewa Karst (Halliday, 1955, 1958). Extensive bibliographic and some field investigations have yielded no information about this cave and it is not known if it still exists. In 1970, Macdonald and Ahhott mentioned the presence of small caves in calcarenite and aeolianite in this and several other karstic localities (Macdonald and Abbott, 1970) but did not amplify. 

Sinkholes of Kalaeloa

by | Mar 29, 2009
http://hawaiianforest.com/wp/sinkholes-of-kalaeloa/

I explored the kiawe forests of Kalaeloa — the former Barber’s Point Naval Air Station — to investigate the innumerable sinkholes in the limestone that were once home to rare native land snails.

Limestone, the remnants of coral reefs when the sea level was higher, underlies the greater part of Kalaeloa and the Ewa Plain.   Located in the rain shadow of the Koolau and Waianae Mountains, Kalaeloa is located in the driest corner of Oahu, receiving less than 20 inches of rain per year.  While the surface of the land is dry and hot for most of the year, just below the surface lies ground water which seeps from the mountains under the Ewa Plain.

Beacons from the Ewa Plains

September 22, 2012

http://studiamirabilium.com/2012/09/22/beacons-from-the-ewa-plains/

Not too many people think of the natural wonders of Hawai’i when they see the Ewa Plains. The present is dominant by such thoughts as commute times, median home prices, proximity to good schools. People do think of its rich past: many extinct native birds have been found fossilized in the uplifted limestone plains. But it’s these wonderful plants, an akoko here, a rare naio there, that offer beacons of hope for a great future.

Honolulu Cave Adventure: Punynari Explores Moiliili (Honolulu, Hawaii) Karst 

Fantastic Must See Oahu Karst Cave Videos And Photos 

Bio Diversity: The Moiliili Karst Formation

Mōʻiliʻili Karst Water Cave


Hiking Hawaii: Moiliili (Honolulu, Hawaii) Karst Cave


Video and Links: Mo'ili'ili Underground Caverns Video 


Karst Cave Hiking Adventure: Moili'ili Karst Exploration 






Monday, December 22, 2014

Evidence Of Large Karst Sinkholes In Ewa Gentry Community Properties

Evidence Of Large Karst Sinkholes In Ewa Gentry Community Properties - Updated to 2021

Ewa Cultural History Historian  John M. Bond

A fascinating look at some of the major sinkholes in the Ewa area.
The entire Ewa Plain is approximately 25 square miles of sinkholes and caves,
some very big and some very small. 

The Ewa Gentry area was built 
over numerous huge karst sinkhole caves as early cultural oral history 
will tell you, and also visible on old USGS maps. One of the really big ones still 
exists and has never been filled in.


Holomua Elementary School which is directly north of this big
sinkhole is known for being haunted with mysterious sounds and
noises. This is likely due to the large underground karst cave
channels that carry rainwater from the mountains and dumps into
the shoreline. 

This area has one of the largest subsurface waterways
that emptied into the Puuloa reef area. Puuloa was known for
large caves, including royal burial caves, and the massive rain
water discharge feed the copious amounts of limu that once
existed there. 

Limu feeds the ecosystem of the fisheries however
much of this has since been destroyed by developments.

Image Below: Holomua Elementary School seen mauka (north) of this 
huge Ewa Plain sinkhole cave site.


It has been used as a flood drainage basin- with the water traveling out through 
the porous karst to the Ewa Puuloa shoreline near the entrance to Pearl Harbor.



This particular development in the Honolulu Star Advertiser story of October 2021
 is directly south of a huge Karst sinkhole cave site as was documented in
this Kanehili Ewa Karst blog in 2014 and now updated.

One of the largest still existing huge deep sinkhole caves is directly adjacent 
(north) to this Gentry development project. I was told many years ago that 
this was left undeveloped because it drains water from the nearby developments. 

However many others like it were filled in and over time rains cause the coral fill to 
subside and wash away exposing pipes underground to corrosion and breaking 
under stress which causes water leaks and eventually breaks. 

This happens all over Oahu's south shore because it is all ancient
coral reef and the subsurface water erosion is continuous 
causing water and sewer pipes to corrode and break, usually flooding streets.


The karst in this area is especially dense with lots of evidence of ancient sea creatures



This site along Kapolei Parkway was later filled up and turned into Geiger 
park as they probably didn't want to put homes over it.



This site exhibits classic groundwater near the surface as it is near the 
Kalo'i waterway that empties by Hau Bush Ewa shoreline park.


Ewa Haseko Corp Digs Big Giant Hole In The Ewa Karst 

And Then Fills It Back Up!


Barbers Point - Kalaeloa - Ewa Beach, The Major Karst Sinkhole Ponds And Reef Blue Holes

https://ewa-hawaii-karst.blogspot.com/2015/08/barbers-point-kalaeloa-sinkholes.html

Fantastic Must See Oahu Karst Cave Videos And Photos 

Bio Diversity: The Moiliili Karst Formation

Mōʻiliʻili Karst Water Cave


Hiking Hawaii: Moiliili (Honolulu, Hawaii) Karst Cave


Video and Links: Mo'ili'ili Underground Caverns Video 


Karst Cave Hiking Adventure: Moili'ili Karst Exploration