Archive

May 15, 2019 by Peter T Young Leave a Comment

Māhā‘ulepū Heritage Trail

Māhā‘ulepū is an ahupua‘a (historic Hawaiian land division) and watershed running from the Hā‘upu mountain range to the shoreline on Kauai’s southeast coast.

The whole coast was populated by native Hawaiians when the first westerner, explorer Captain James Cook, sailed through Kauai waters to land in Waimea in 1778.

Cook’s arrival set the stage for an influx of newcomers from around the world and catalyzed a dramatic transformation of Hawai‘i’s land use and demographics.

By 1850, American entrepreneurs launched large-scale sugar plantations in southeast Kauai. Their efforts heralded the beginning of Hawai‘i’s plantation era, which lasted into the late 20th century.

Kauai’s South Shore coastline features a fascinating hike along the Māhā‘ulepū Heritage Trail, a 4-mile round trip stretching from Keoneloa Bay to Kawailoa Bay.

A range of natural and cultural resources reflect the state’s evolution through the periods of Hawaiian settlement and expansion, Western contact, and plantation life. The following summarizes some of them.

1. Keoneloa Bay – “Long Sand, Long Beach”

This is a long stretch of sandy beach on the far eastern end of the Po‘ipū resort area, fronted by The Grand Hyatt Kauai Resort & Spa and a county park facility.

It is also known as Shipwreck Beach, named for the wreckage an old, wooden fishing boat on the beach back in the 1970s (that has long since disappeared.)

2. Makahuena – “Rough Face” & Makawehi – “Calm Face”

The unusual cliff formations were formed from sand dunes that have been weathered by wind and surf over the centuries. These ancient limestone sea cliffs have been virtually sandblasted by a combination of wind, salt and water.

Today Makawehi point is being undercut by continual wave erosion. The huge blocks of limestone that lie at the base of these cliffs are examples of that erosion.

3. Pā‘ā Dunes – “Fence of Lava Rock” or “Dry and Rocky”

About 8,000 years ago, dunes began forming atop Makawehi as sections of the sandy shoreline accumulated a reddish fossil soil overlay.

The tradewinds blowing from the northeast or mauka (mountain) side of this area have had the most dominant influence determining the shape of the dunes along this section of coast, with kona winds from the southwest having a minor influence.

4. Pinnacles

Sandstone-limestone pinnacles are usually formed by rain-water washing down along vertical fractures in the limestone. Pinnacles can be seen in stark formation to the right of a small bay just before the climb to the golf course.

5. Heiau Ho‘ouluia – “Fishing Temple”

This site is thought to have been a place of worship where fish were offered to the god of the sea, to ensure good fishing.

6. Punahoa – “To Bind or Lash”

Punahoa is composed of a very thick accumulation of coastal sand dunes that formed around 350,000 years ago. They are the oldest sand dunes of this region, carved by the tradewinds which formed all the dunes of this coast.

Along this area are short pieces of pipe anchored into the lava rock to hold fishing poles. This shoreline has been popular for centuries among local fishermen, catching primarily shoreline game fish such as ulua, papio (juvenile ulua) and oio.

7. Makauwahi Sinkhole – “Fear, Break Through”

The Makauwahi Sinkhole is a small portion of the largest limestone cave found in Hawaii. Paleoecological and archaeological excavations of the sediment that has filled the pond in the sinkhole put its age at some 10,000 years, and have revealed at least 45 species of bird life.

More importantly, the findings of this study show how the first humans that inhabited Kauai affected the pre-human natural environment. It is one of only a handful of sites in the world that show such impact.

8. Māhā‘ulepū Beach-“And Falling Together”

Māhā‘ulepū’s name comes from a legendary battle that occurred in the 1300s when Kalaunuio Hua, a Big Island ruler, made an attempt to take over all the Hawaiian islands.

By nightfall, it was evident that Kalaunuio Hua had lost the battle and became a prisoner to Kukona. Thus began the historical distinction of Kauai as an island that was never conquered.

9. Wai‘ōpili Petroglyphs – “Water Against”

In 1887, Kauai resident JK Farley discovered carved drawings or petroglyphs on a rock at Māhā‘ulepū Beach near the mouth of the Wai‘ōpili Stream. The carvings are normally covered by beach sand, but if tides and ocean conditions are right the petroglyphs can occasionally be seen.

North of Māhā‘ulepū Beach is a large petroglyph boulder which contains two cup-like carvings at the top. One of the carvings contains a pecked out groove from the cup and runs along the edge of the boulder.

The Māhā‘ulepū Heritage Trail is a project of the Po‘ipū Beach Foundation.

Follow Peter T Young on Facebook

Follow Peter T Young on Google+

Follow Peter T Young on LinkedIn

Follow Peter T Young on Blogger

Māhā‘ulepū Village as drawn by Hiram Bingham-1824

1-Keoneloa Bay

2-Makawehi

3-Paa Dunes

4-Pinnacles

5-Heiau Hoouluia

6-Punahoa

7-Makauwahi Sinkhole

8-Mahaulepu Beach

9-Waiopli Petroglyphs

Mahaulepu_Heritage_Trail-Map

May 14, 2019 by Peter T Young Leave a Comment

Out Of This World

Man landed on the Moon, remote rovers traversed portions of the Martian surface and now some folks are dreaming of, preparing for and testing opportunities of having humans landing on Mars.

Of course, the best way to study the Martian surface and its climate is to go there, and as a part of a necessary activity before humans travel to Mars, planetary scientists study places on the Earth that are like the Martian surface.

Before getting there, scientists need to test and experiment with terrestrial soils to best prepare for human occupation on Mars.

Soils are used in testing rover vehicles, food production and equipment maintenance.

Since voyagers will not be able to transport sufficient amounts of food on their flight, they will need to grow their own food – kind of like ET Agriculture (the ultimate in subsistence, self-sufficient farming.)

Based on soil evaluation and testing, scientists believe it is possible to grow plants on Mars in technologically advanced, controlled environments that could keep the plants warm and give the plants enough atmosphere, light and water to live.

It turns out Mauna Kea Volcano is one of the few places on the Earth that is similar to what scientists currently know about the surface and soil make-up of Mars.

Scientists have made extensive worldwide searches for naturally-occurring equivalents for Martian surface materials and have concluded that weathered volcanic ash from the Island of Hawai‘i are uniquely suitable for Martian simulants.

Mauna Kea has color (a reddish-brown,) mineralogy, chemical composition, particle size, density and magnetic properties similar to the oxidized soil of Mars.

Samples of volcanic ash from Iceland, Alaska, Antarctica, Mexico, New Mexico and Hawai‘i were collected and investigated by NASA since the 1970s.

While Mauna Kea summit has the best examples of volcanic ash similar to the Martian soils, due to sensitivity of extracting from the summit, a cinder cone (Pu‘u Nene) adjacent to the old section of Saddle Road was selected (now bypassed, due to the recent realignment between Mauna Kea Access Road and Mauna Kea State Park.)

It was found that material from Pu‘u Nene on the lower part of Mauka Kea matched Martian characteristics better than any other site tested. The material found on Pu‘u Nene has a particular composition of “palagonite” and may be unique in the world.

The ash is used by various agencies, including NASA, and also schools and private firms conducting experiments (primarily for rover studies and to determine if the palagonite ash could support plant growth) or teaching about Mars.

While I was at DLNR, after a Contested Case Hearing on the matter, we issued a Conservation Use Permit to hand quarry (using shovels) volcanic ash from Pu‘u Nene cinder cone for these scientific studies.

The Property is located in the Resource subzone of the Conservation District. Mining is an expressly identified use in the Resource subzone of the Conservation District.

Pu‘u Nene has been extensively quarried for cinders that were used, among other things, to pave Saddle Road in the 1940s; it is dominated by alien vegetation, has no archaeological or cultural sites, and there is very little native vegetation at the site.
Although the Humu‘ula saddle area itself has a storied past, there is no known Hawaiian name for Pu‘u Nene. It was, therefore, concluded that it was a modern term, perhaps given by L. “Bill” Bryan who served as manager of the Civilian Conservation Corps and as Territorial Forester on the Island of Hawai‘i between the 1930s to the 1960s.

Native Hawaiian testimonies, survey records and cartographic resources reveal that this general area of pu‘u, or cinder cone hills, are known as ‘Oma‘okoili (literally, “resting in the saddle.”)

In the hand quarrying operation, rather than extract directly from the surface, researchers extract the ash about 2-3 feet below the soil layer.

After it is quarried, it is processed by passing it through a series of stainless steel sieves to separate it by granule size into fine-grade and medium-grade ash. It is then distributed to research and educational projects and facilities.

This isn’t the first time NASA looked to Hawai‘i, and Mauna Kea in particular, for extra-terrestrial travel preparations.

During the Apollo lunar landing series, astronauts were trained on Mauna Kea and regarded the area as the most lunarlike that they had observed. (Apollo 11 was the spaceflight in which American astronauts Neil Armstrong and Buzz Aldrin became the first to land on the Moon, on July 20, 1969.)

NASA teams have operated tools, instruments and systems on Mauna Kea; each one aimed to better understand potential space resources, limit the amount of resources humans would have to carry with them beyond low Earth orbit and also protect hardware once is gets there.

Different rovers were tested on Mauna Kea. In 2011, ‘Curiosity’ was launched and eventually landed on Mars on August 5, 2012, carrying laboratory instruments to analyze samples of rocks, soil and atmosphere, and investigate whether Mars has ever offered environmental conditions favorable for microbial life.

“When NASA’s Curiosity rover began using its on-board instrument to analyze the chemical composition of the rocks and soil on Mars, the results bore a striking resemblance to those obtained during previous tests of the Chemistry and Mineralogy instrument on Hawaii’s Mauna Kea volcano.” (SpaceNews)

Follow Peter T Young on Facebook

Follow Peter T Young on Google+

Follow Peter T Young on LinkedIn

Follow Peter T Young on Blogger

NASA and its international partners are using Mauna Kea for equipment testing to advance future space exploration (NASA-Amber Philman)

Testing of equipment on Mauna Kea, a remote and cold dormant volcano on Hawaii-(NASA-Amber Philman)

Astronauts-James-A.-Lovell-Jr.-left-commander-and-Fred-W.-Haise-Jr.-lunar-module-pilot-carry-out-a-simulation-of-a-lunar-traverse-WC

Astrogeologist Dr. Jim Rice studying Mars-like features on Earth-(Courtesy NASA-JPL-Caltech)

Apollo_Astronaut_Alan_Shepard-Training_on_the_Big_Island-(pisces-hilo-hawaii-edu)

Apollo 13 Astronauts Fred Haise and Jim Lovell observe features of a lava flow during a geology field training trip-(NASA)

Curiosity – The Next Mars Rover-(Courtesy NASA-JPL-Caltech)

Self-portrait of NASA’s Curiosity rover taken on Sol 2082 (June 15, 2018)

Puu_Nene_GoogleEarth

May 13, 2019 by Peter T Young 1 Comment

Baldwin House

Dwight Baldwin was born on September 29, 1798 to Seth Baldwin (1775 –1832,) (a framer) and Rhoda Hull Baldwin in Durham, Connecticut, and moved to Durham, New York, in 1804. His father, He was the second of 12 children. (Baldwin Genealogy)

He was employed with his father on the farm, enjoying the benefits of the common school, and generally in winter of a select school, till the age of sixteen. In the fall of 1814, he commenced the study of Latin, with a view to prepare for College.

The last of his teachers being a graduate of Williams College, he was induced to enter at Williams, where he spent two years; and then he left Williams and entered Yale College, where he graduated in September, 1821.

By the recommendation of President Day, the next two years he was employed as Principal of the Academy in Kingston, Ulster County, NY. A third year was spent in teaching a select school in Catskill, Greene county. He then devoted himself to the study of medicine, at the same time teaching a select school in Durham, NY.

Then, he got caught in the religious fervor; about the first of March, 1826, he found relief in believing in an Almighty Redeemer, a hope which has never forsaken him. Religion became the all-absorbing subject of his thought by day and by night. (Baldwin Genealogy)

He soon came to the decision to join a mission, and September 3, of that year, he united with the Congregational Church in Durham, NY, and soon after he entered the Theological Seminary at Auburn, where he spent three years, offering his services into the American Board of Boston for a Foreign Mission … and they were accepted.

He did not have time to await official recognition of his medical degree so at direction of the Prudential Committee he took his diploma as Master of Science. He was ordained at Utica, NY on October 6, 1830.

He was introduced by a friend to Charlotte Fowler, daughter of Deacon Solomon Fowler of North Branford, Connecticut, and a few weeks later was married to her on December 3, 1830. Twenty-five days later they set sail with the Fourth Company of missionaries to Hawaiʻi on the ship ‘New England;’ he arrived at Honolulu, June 7, 1831. (Baldwin)

They ended up in Maui. Construction on the coral-and-rock Baldwin House began in 1834 and was completed in 1835; it’s the oldest house in Lāhainā.

The thick walls were made of coral and stone. The structure was sturdy consisting of hand-hewn timbers. In 1840, a bedroom and study was added, and in 1849, an entire second story was completed.

The faithful restoration of the Baldwin Home by the Lāhainā Restoration Foundation is based on careful documentary and archeological research.

It is part of the Lāhainā National Historical American Buildings Survey. It was deeded to the Lāhainā Restoration Foundation by the HP Baldwin Estate in 1967. It can never be sold and will remain in the Public Domain in perpetuity.

The home itself, the household furniture, the aged photographs and artifacts, the displays and library present a picture of the missionary who was both a physician and a constructive community force.

His educational background coupled with many natural abilities guided him to be helpful in the establishment of a system of just and democratic laws and most importantly the education of the Hawaiian people who learned much besides religion.

They were taught reading and writing in Hawaiian and English trained in agriculture and mechanics, studied the practical arts in the high school above Lāhainā; and finally learned to understand constitutional government, diplomacy and finance.

As a practicing physician, Rev. Baldwin treated and helped save the people of Maui, Molokai and Lāna‘i.

A series of epidemics swept through the Hawaiian Islands, whooping cough and measles, soon after followed by waves of dysentery and influenza; then, in 1853, a terrible smallpox epidemic.

Although precise counts are not known, there were thousands of smallpox deaths on O‘ahu; Baldwin is credited with keeping the toll to only a few hundred on Maui.

Dwight Baldwin was patriarch of a family that founded some of the largest businesses in the islands. His son, Henry Perrine Baldwin (1842–1911) and Samuel Thomas Alexander (1836–1904; also son of a missionary) met in Lāhainā, Maui.

They grew up together, became close friends and went on to develop a sugar-growing partnership that spanned generations and left an indelible mark on Hawai‘i – Alexander & Baldwin (one of Hawai‘i’s Big Five companies.)

In addition, sons Henry Perrine Baldwin and David Dwight Baldwin laid the foundation for what is now known as Maui Land & Pineapple Company, Inc in the late 1800s through the acquisition of land and formation of associated companies.

In 1870 Dwight and Charlotte moved to Honolulu as their health deteriorated and lived with their daughter Harriet (called “Hattie”). Charlotte died October 2, 1873, and Dwight died on January 3, 1886; they are buried at the Kawaiahaʻo Church cemetery.

Lāhainā Restoration Foundation oversees and maintains 11 major historic structures in Lāhainā and provides tours of the Baldwin House. Hours of Operation: Open Daily from 10 am – 4 pm ($5 Kama‘āina admission); Candlelit Tours Fridays 6 pm – 8:30 pm ($6 Kama‘āina admission)

Follow Peter T Young on Facebook

Follow Peter T Young on Google+

Follow Peter T Young on LinkedIn

Follow Peter T Young on Blogger

Baldwin-House (Lahaina Restoration Foundation)

Dwight Baldwin (1798–1886) was a physician and missionary on Maui

Baldwin House during reconstruction of 1966

Baldwin House-LOC-058628pv

Baldwin House-LOC-058629pv

Baldwin House-LOC-058632pv

Maui-Lahaina-Baldwin-House

Maui-Lahaina-Baldwin_House

Maui-Lahaina-Baldwin-House

Baldwin_House (Lahaina Restoration Foundation)

May 12, 2019 by Peter T Young Leave a Comment

Pā‘aiea Pond

It is said there once was a very large fishpond extending from Ka‘elehuluhulu, adjoining the region of Mahai‘ula (now part of Ke Kahakai State Park,) running south past Ka-Lae-O-Keāhole to as far south as Wawaloli on the boundary of ‘O‘oma (the beach park within the Natural Energy Laboratory,) in North Kona on the Big Island.

This is the present area of Kona International Airport.

This fishpond, known as Pā‘aiea, was reportedly three-miles long and a mile-and- a-half wide; it was the large fishpond of Kamehameha.

The pond was so large that fishermen going to Kailua and further South, often took a short cut by taking their canoes into the pond and going across, thus saving time against the strong sea breeze and current from Keāhole.

There was a famous saying about this fishpond: O na hoku o ka lani, o Pā‘aiea ko lalo – The stars are above, Pā‘aiea below.

The reason for this saying was because of its exceptionally large size. Within the wide waters of this pond were numerous little islets that were compared to the stars in the heavens.

“Pā‘aiea was a great pond almost like the ponds of Wainanalii and Kiholo. In the olden days, when the great ruling chiefs were living, and when these fish ponds were full of the riches of Awa, Anae, and Ahole, along with all sorts of fish which swam within.”

“During that time, Konohiki were stationed, and he was the guard of the pond that watched over the pond and all things, as here we are talking about Pā‘aiea Pond which was destroyed by lava and became pahoehoe lava which remains today”.

“In the correct and trues story of this pond, its boundaries began from Kaelehuluhulu on the north and on the south was at the place called Wawaloli, and the distance from one end to the other was 3 miles or more, and that was the length of this pond …”

“… and today within these boundaries, there are a number of pools [lua wai loko] remaining during this time that the writer is speaking before the readers of the Hoku.”

“The great Overseer [Konohiki] who cared for this pond was Kepaalani, and everything fell under him: the storehouses [hale papaa] where poi and fish were stored, the halau for the fishing canoes, the nets and all thing, and from him the fishermen and the retainers of the court would obtain their sustenance.”

“And at this time when the pond was destroyed by lava, Kamehameha was residing in Hilo for the purpose of waging war, and this war was called Kaipalaoa …”

“… during this war, Namakehaikalani died and was offered atop the Heiau of Piihonua in Hilo; and this was Kamehameha’s final war, and his enemies lived quietly without uprising once again. “

“This was the time between 1798 until 1801, and it is said that this is when lava destroyed this pond that was full of riches, and turned it into a land of pahoehoe lava which remains to this day.” (Hoku o Hawaii, 2/5/1914)

Pā‘aiea Pond was reportedly destroyed by the 1801 eruption and lava flow from Hualālai. Two parts to a story relate to the cause of its destruction.

The first suggests that one day an old woman appeared at the large canoe shed of Kepa‘alani (the konohiki or overseer of the pond.)

Another man, Kapulau, asked: “Malahini?” (newcomer)

She replied “I am a Kama‘āina, not exactly a total stranger, but I do not often come down here to the seashore. Living in the restful uplands, and hearing that there was plenty of fish down at the beach, I hastened down to see if the fishermen would give me a bit of palu.”

The konohiki replied, “”No! You cannot have fish, palu, shrimps or anything. It all belongs to the Chief, and only the Chief can give them to you.”

“Well! That is all. I now return to the uplands without even a grain of salt.” The old woman stood up and turned around to go.

When she came to Kapulau’s house, she was urged to remain and have something to eat. She consented and sat down. When she had finished her meal, Kapulau gave her a fish.

The old woman stood up, and before starting to go, she gave these instructions to her host: “Tonight, you and your wife put up a lepa (kapa cloth on end of a stick, as used to mark a taboo area) back of your house and here on your fence.” They followed her instructions.

In the second part of the story, this same old woman soon afterwards appears at a village called Manuahi which was on the Western slope of Hualālai, and where two girls who figure in this story, lived; they were roasting bread-fruit.

The name of one of these girls was Pahinahina and the name of the other was Kolomu‘o. As soon as the old woman saw then she inquired: “For whom are you roasting your bread-fruit?”

Kolomu‘o answered: “I am roasting my bread-fruit for La‘i. That is my God and the God of my parents.”

Then the old woman turned and asked Pahinahina, the other girl, “and for whom, pray, are you roasting your breadfruit?” “For Pele,” Pahinahina replies.

Then they ate the breadfruit.

Then the old woman asked Pahinahina: “Where is your house?” Pahinahina told her they shared a house, but the families lived on respective end of it. The old women then told her, “When your parents come home, you tell them to put up a lepa on the end of your part of the house.” They complied.

That night, the people living at the beach saw an eruption on Mountain of Hualālai and as they saw the lava flow they realized that the old woman whose request for fish, palu and shrimps had been refused, could have been no other than the Goddess Pele.

The lava came and destroyed the great fishpond of Pā‘aiea, dried its water and filled and covered it with black rocks.

However, two places were spared.

There remained only that very small portion of the fishpond, close to Ho‘ona (within the Natural Energy Laboratory property at Keāhole Point.)

Also, the area where Pahinahina and her family lived was left untouched, and this open space bears the name of Pahinahina to this day (it is below the old headquarters at Hu‘ehu‘e Ranch).

It is said that because of this event that the lands of Manuahi came to be called Ka-ulu-pulehu (the roasted breadfruit (‘ū is short for ‘ulu,)) and this has been shortened to Ka‘ūpūlehu.

Follow Peter T Young on Facebook

Follow Peter T Young on Google+

Follow Peter T Young on LinkedIn

Follow Peter T Young on Blogger

Paaiea-Akahipuu-Keahole-Point-Map-Emerson-Reg1449-1888-

May 11, 2019 by Peter T Young Leave a Comment

“The Queen’s Retreat” (Waikīkī)

“In 1868, the year of her 30th birthday and the sixth anniversary of her marriage to John (Dominis), Lili‘uokalani inherited valuable property in Waikiki”. (Star Bulletin)

“The Queen’s Retreat” was in the district of Hamohamo (“rub gently,”) it consisted of two homes – one, called Paoakalani (“the royal perfume,”) was her principal home in Waikīkī.

The other was Ke‘alohilani (“the royal brightness,”) located opposite Kūhiō Beach, which she referred to in her memoirs as “my pretty seaside cottage.”

“In contrast to stately Washington Place, the one-story Ke‘alohilani was open on two sides with a large and inviting living room ‘filled with all things Hawaiian,’ where Lili‘uokalani and her ohana could gather in joy and hospitality”.

“Next to a satin pillow, embroidered in heavy thread proclaiming ‘There Is No Place Like Home,’ stood feathered kahilis. … A feather cape, a knitted afghan, a dog’s tooth necklace, a gold-plated bracelet …”

“… all intermingled in the home Lili‘uokalani came to love so dearly. ‘I danced around the rooms. It was my own!’” (Lili‘uokalani; Hawaii Bar Assn)

Here, she retreated to relax and informally entertain family, friends and on occasion, visiting royalty. She also spent much of her time composing her songs and translating Hawaiian stories into English.

Her home served as a comforting getaway from the pressures of business at ʻIolani Palace, several miles away.

“Hamohamo is justly considered to be the most life-giving and healthy district in the whole extent of the island of Oʻahu; there is something unexplainable and peculiar in the atmosphere of that place, which seldom fails to bring back the glow of health to the patient, no matter from what disease suffering.”

The Queen “derived much amusement, as well as pleasure: for as the sun shines on the evil and the good, and the rain falls on the just and the unjust, I have not felt called upon to limit the enjoyment of my beach and shade-trees to any party in politics …”

“While in exile it has ever been a pleasant thought to me that my people, in spite of differences of opinions, are enjoying together the free use of my seashore home.” (Lili‘uokalani)

In setting up the Lili‘uokalani trust, “Assisted by her attorneys, Lili‘uokalani conveyed all her real property to three trustees (brother-in-law Archibald S Cleghorn, business agent Curtis P Iaukea, and attorney William O Smith) on December 2, 1909. She retained the right to use Washington Place and Ke‘alohilani as her residences”. (Hawaii Bar Assn)

After the Queen’s death, Ke‘alohilani, as well as the pier and beach fronting the area (including the fisheries,) was transferred to Prince Kūhiō.

The Prince and his wife, Princess Elizabeth Kahanu, temporarily lived in Queen Lili‘uokalani’s Waikīkī cottage, Ke‘alohilani, for about a year.

They razed it and constructed a new home, which they called Pualeilani (“heavenly flower lei” or “flower from wreath of heaven.”)

After Prince Kūhiō died at Pualeilani on Jan. 7, 1922, the property was given to the city; by 1938 the name of the pier, as well as the beach area fronting it, became known as Kūhiō Beach.

The surf break in front of this is still known as Queen’s, because this was facing the Queen’s home.

Kuekaunahi stream used to run through the property; this small stream paralleled Kapahulu Avenue and crossed Waikīkī Beach at the intersection of Kalākaua and Kapahulu Avenue.

The stream was eventually enclosed in a culvert and at the shore its waters were channeled into the ocean through the Kapahulu Groin.

Follow Peter T Young on Facebook

Follow Peter T Young on Google+

Follow Peter T Young on LinkedIn

Follow Peter T Young on Blogger