Images of Old Hawaiʻi

by Peter T Young Leave a Comment

Honuaʻula

The moku (district) of Honuaʻula includes the Southeastern portion of the island of Maui from the coastal bay of Keawakapu (modern day South Kihei area) to the rocky shoreline of Kanaloa point, seven miles south of Keoneʻoʻio (La Perouse) Bay.

The moku of Honuaʻula extends inland to what is now the southeastern face of Haleakala National Park and includes the upland regions of Ulupalakua and Kanaio. It also includes the Island of Kahoʻolawe a few miles away across the ʻAlalakeiki channel (the “rain shadow” of Maui’s Haleakalā, a “cloud bridge” connects Kahoʻolawe to the slopes of Haleakalā.)

The upper areas were in sandalwood and koa forests. Prior to European contact, early Hawaiians farmed sweet potatoes, dry land taro and harvested wood, birds and pigs from these forested areas.

Researchers believe that in the era from AD 1300 to 1800 native forests in southeast Maui areas like Honuaʻula began much lower- around the 2,300 to 2,800 foot elevation. These views are based upon analysis of bird and snail remains, common species represented in studies of Honuaʻula’s neighboring moku (district) of Kahikinui.

The areas below the west and south slopes of Haleakalā (Kula, Honuaʻula, Kahikinui and Kaupo) in old Hawaiian times were typically planted in sweet potato. The leeward flanks of Haleakalā were not as favorable for dry or upland taro. However, some upland taro was grown, up to an altitude of 3,000 feet.

The district was one frequented by droughts and famines. Hawaiians supported themselves by cultivating in the uplands, and fishing, with some lowlands agriculture when rains fell. They also traded woven goods and other items for kalo from Na Wai ʻEhā (Waikapū, Wailuku, Waiʻehu and Waiheʻe.)  (Maly)

Archaeologists have proposed that early Polynesian settlement voyages between Kahiki (the ancestral homelands of the Hawaiian gods and people) – Kahikinui, the district neighboring Honua‘ula to the south, is named because from afar on the ocean, it resembled a larger form of Kahiki, the ancestral homeland.  (Maly)

Honuaʻula (literally, Red-land or earth) is comprised of twenty traditional ahupuaʻa.  Honuaʻula was a legal-judicial district throughout the nineteen century. In modern times, Honuaʻula has been joined with portions of the traditional moku of Kula, Hamakuapoko and Hamakualoa to form Maui County’s Makawao land management district.  (de Naie)

The Honuaʻula lands are tied to the legend of the great voyaging chief, Moʻikeha, who sailed to Kahiki (Tahiti) after the devastation of his homelands in Waipiʻo Valley on the island of Hawaiʻi. One of Moʻikeha’s voyaging companions, a chief named Honuaʻula, is said to have given the Maui district its name when he asked to be put ashore there.  (Fornander)

“Where the wind dies upon the kula (plains) is the sub-region of Makena and Kula, where the mists are seen creeping along the plain. This is a land famous with the Chiefs from the distant past.”  (From the tale of Ka-miki, Maly, de Naie)

Because of its proximity to Hawaiʻi Island, favorable wind conditions, long coastline with sandy beaches and several sheltered bays, it is likely that the Honuaʻula district received voyagers from these early excursions. Perhaps this is why it was described in the ancient (AD 1200-1300) name chant of Ka-miki as being “a land famous with the Chiefs from the distant past.“

 “In ancient times, the land was covered with people. From the summits of the mountains to the shore are to be found the remains of their cultivated fields and the sites of their houses.”  (Kamakau, de Naie)

Honuaʻula’s earliest history is tied to the importance of Puʻu Olaʻi (“Red Hill” and “Miller’s Hill”.) Puʻu Olaʻi has its origin in the legendary battle between the volcano goddess Pele and the local moʻo (supernatural lizard) goddess Puʻuoinaina.

Puʻu Olaʻi, a 360-foot cinder cone forms a point and separates Oneloa “Makena” Beach from Oneuli “Black Sand” Beach. A portion of Puʻu Olaʻi further divides Makena Beach into ‘Big Beach’ and ‘Little Beach.’

Honuaʻula is also home to a number of traditional Hawaiian fishponds, most adapted from natural wetlands along the shore. Three of these are shown in old maps in the Honuaʻula, and several more were shown just to the south of Puʻu Olaʻi.

Based upon this cultural view, the earliest population levels of Honuaʻula would have been linked to availability of food from the sea and the land and fresh water resources, as well as the influence of spiritual forces and familial ties.

The presence of trade resources such as dried sea salt, volcanic glass and canoe building materials as well as safe landing areas and favorable currents would all be part of the mix of conditions to determine the extent of population.

In 1789, Simon Metcalf (captaining the Eleanora) and his son Thomas Metcalf (captaining the Fair American) were traders; their plan was to meet and spend winter in the Hawaiian Islands.  After a confrontation with a local chief on Hawaiʻi Island, Simon Metcalf then sailed to Maui and anchored the Eleanora off shore, probably at Makena Bay.

Someone stole one of Metcalfe’s small boats and killed a watchman. Captain Metcalfe fired his cannons into the village, and captured a few Hawaiians who told him the boat was taken by people from the village of Olowalu.

He sailed to Olowalu but found that boat had been broken up, enraged, Metcalfe indicated he wanted to trade with them; instead, he opened fire, about one hundred Hawaiians were killed, and many others wounded.  Hawaiians referred to the slaughter as Kalolopahu, or spilled brains; it is also called the Olowalu Massacre.

From 1800 to the 1840s (in the period prior to the Māhele ʻĀina), the land here was managed for members of the Kamehameha household and supporting high chiefs by  konohiki—lesser chiefs appointed by Kamehameha III and Ulumäheihei Hoapili. (Maly)

Up to the early 1840s, land use, access, and subsistence activities remained as it had from ancient times. But by the middle 1840s, land use transitioned from traditional subsistence agriculture to business interests, focused on ranching and plantations (the latter occurring in the cooler uplands).

Modern agricultural began on the slopes of Haleakalā in 1845 when Linton L Torbert, an active member of the Royal Hawaiian Agricultural Society, farmed potatoes and corn, primarily to supply island merchant ships and California’s ’gold rush’ era.  He later planted sugar.  (The 2,300-acres had first been leased from King Kamehameha III in 1841.)

On January 23, 1856, “Kapena Ki” (Captain James Makee) purchased at auction Torbert’s plantation.  He sold his Nuʻuanu residence. (He was active in Oʻahu business and, later, was the Kapiʻolani Park Association’s first president (they even named the large island in the Park’s waterways after him.))

The Stone Meeting House at Keawakapu (also called Honuaʻula or Makena Church) was completed in 1858.  In 1944, the church known as the Stone House, Honuaʻula, Keawekapu, Makena and Kaʻeo was renamed Keawalaʻi – the name it retains today.  (Lots of information here from ‘Project Kaʻeo’ (de Naie, Donham) and He Mo‘olelo ‘Āina No Ka‘eo (Maly))

© 2022 Hoʻokuleana LLC

by Peter T Young 1 Comment

Kaʻahumanu’s Coffin

While on a trip to the continent, Queen Kamāmalu (age 22) died on July 8, 1824; King Kamehameha II (Liholiho, age 27) died six days later on July 14, 1824.  (Prior to his death he asked to return and be buried in Hawai‘i.)

Upon their arrival in Hawai‘i, in consultation between the Kuhina Nui (former Queen Kaʻahumanu) and other high chiefs, and telling them about Westminster Abbey and the underground burial crypts they had seen there, it was decided to build a mausoleum building.

In 1825, Pohukaina (translated as “Pohu-ka-ʻāina” (the land is quiet and calm)) was constructed on what is now the grounds of ʻIolani Palace to house the remains of Kamehameha II (Liholiho) and Queen Kamāmalu.

The mausoleum was a small 18 x 24-foot Western style structure made of white-washed coral blocks with a thatched roof; it had no windows.   Kamehameha II and Queen Kamāmalu were buried on August 23, 1825.

About this same time, April 25, 1825, Richard Charlton arrived in the Islands to serve as the first British consul. He had been in London during Kamehameha II’s visit in 1824.

Nearly 10-years later, in 1832, Kaʻahumanu died; her death took place at ten minutes past 3 o’clock on the morning of June 5, “after an illness of about 3 weeks in which she exhibited her unabated attachment to the Christian teachers and reliance on Christ, her Saviour.”  (Hiram Bingham)

The Kaʻahumanu services were performed by Bingham.  After the sermon in Hawaiian, he addressed the foreigners present and the mission family.  After the close of the services, the procession was again formed and walked to Pohukaina, where the body was deposited, with the remains of others in the Royal family.  (The Friend, June 1932)

The above helps set the stage for subsequent events that happened there.

Nearly 10-years later, in 1840, Charlton made a claim for several parcels of land in Honolulu.   At the time the lease was made, Kaʻahumanu was Kuhina Nui and only she and the king could make such grants.  The land was Kaʻahumanu’s in the first place, and Kalanimoku certainly could not give it away.  (Hawaiʻi State Archives)  The dispute dragged on for years.

This, and other grievances purported by Charlton and the British community in Hawai‘i, led to the landing of George Paulet on February 11, 1843.

He noted in a letter to the King, “I have the honor to notify you that Her Britannic Majesty’s ship Carysfort, under my command, will be prepared to make an immediate attack upon this town at 4 pm tomorrow (Saturday) in the event of the demands now forwarded by me to the King of these islands not being complied with by this time.”

On February 25, the King acceded to his demands.  Under the terms of the new government the King and his advisers continued to administer the affairs of the Hawaiian population.

It soon became clear that Paulet had no intention of limiting his rule to the affairs of foreigners.  New taxes were imposed, liquor laws were relaxed.   Paulet refused to restore the old laws.  After raising multiple objections to the actions by Paulet, Judd resigned from the commission on May 11.  (Daws)

Fearing that Paulet would seize some of the archives and other national records, Gerrit P Judd took them from the government house, and secretly placed them in the royal tomb at Pohukaina.  He used the mausoleum as his office.

By candlelight, using the coffin of Kaʻahumanu for a table, Judd prepared appeals to London and Washington to free Hawaiʻi from the illegal rule of Paulet.

Dispatches were sent off in canoes from distant points of the island; and once, when the king’s signature was required, he came down in a schooner and landed at Waikīkī, read and signed the prepared documents, and was on his way back across the channel, while Paulet was dining and having a pleasant time with his friends.  (Laura F Judd)

For about five months the islands were under the rule of the British commission set up by Lord George Paulet.  Queen Victoria, on learning these activities, immediately sent an envoy to the islands to restore sovereignty to its rightful rulers.  Finally, Admiral Richard Thomas arrived in the Islands on July 26, 1843 to restore the kingdom to Kamehameha III.

Then, on July 31, 1843, Thomas declared the end of the Provisional Cession and recognizes Kamehameha III as King of the Hawaiian Islands and the Islands to be independent and sovereign; the Hawaiian flag was raised.  This event is referred to as Ka La Hoʻihoʻi Ea, Sovereignty Restoration Day, and it is celebrated each year in the approximate site of the 1843 ceremonies, Thomas Square.

Nearly 20-years later, Pohukaina was the final resting place for the Hawaiʻi’s Kings and Queens, and important chiefs of the kingdom.  Reportedly, in 1858, Kamehameha IV brought over the ancestral remains of other Aliʻi – coffins and even earlier grave material – out of their original burial caves, and they are buried in Pohukaina.

In 1865, the remains of 21-Ali‘i were removed from Pohukaina and transferred in a torchlight procession at night to Mauna ‘Ala, a new Royal Mausoleum in Nu‘uanu Valley.  In a speech delivered on the occasion of the laying of the Cornerstone of The Royal Palace (ʻIolani Palace,) Honolulu, in 1879, JH Kapena, Minister of Foreign Relations, said:

“Doubtless the memory is yet green of that never-to-be-forgotten night when the remains of the departed chiefs were removed to the Royal Mausoleum in the valley.”

“Perhaps the world had never witnessed a procession more weird and solemn than that which conveyed the bodies of the chiefs through our streets, accompanied on each side by thousands of people until the mausoleum was reached, the entire scene and procession being lighted by large kukui torches, while the midnight darkness brought in striking relief the coffins on their biers.”

“Earth has not seen a more solemn procession what when, in the darkness of the night, the bodies of these chieftains were carried through the streets”.  (Hawaiian Gazette, January 14, 1880)

In order that the location of Pohukaina not be forgotten, a mound was raised to mark the spot.  After being overgrown for many years, the Hawaiian Historical Society passed a resolution in 1930 requesting Governor Lawrence Judd to memorialize the site with the construction of a metal fence enclosure and a plaque.

© 2022 Hoʻokuleana LLC

by Peter T Young Leave a Comment

Room 120

Amasa Leland Stanford was born and grew up in New York; he was a lawyer.  Stanford married Jane Eliza Lathrop on September 30, 1850; they first lived in Port Washington, Wisconsin, then New York, and then they moved West after the gold rush, like many of his wealthy contemporaries.

Stanford made his fortune in the railroads; he co-founded and was president of the Central Pacific Railroad (it formed part of the “First Transcontinental Railroad” in North America; It is now part of the Union Pacific Railroad.) He served as California Governor and US Senator.

In 1868, the Stanfords had their only child, a son, Leland DeWitt Stanford (later known as Leland Stanford Jr.)  In 1876, Stanford purchased the Rancho San Francisquito for a country home and began the development of his famous Palo Alto Stock Farm.

Tragically, in 1884, while travelling in Italy, young Leland died of typhoid fever (2-months before his 16th birthday.)

Within weeks of his death, the Stanfords decided that, because they no longer could do anything for their own child, “the children of California shall be our children.” They quickly set out to find a lasting legacy to memorialize their beloved son.

Ultimately, they decided to establish two institutions in Leland Jr’s name.  The ‘Leland Stanford Junior University’ was founded in 1885; on October 1, 1891, it opened its doors with 15 faculty and more than 400 students (David Starr Jordan served as president.)  The Leland Stanford Junior Museum opened in 1894.

They were built on the 8,000-acre Palo Alto Farm; a provision in the school’s founding grant stipulated that the land could never be sold.  The campus still carries the nickname ‘the Farm,’ it is more commonly called, ‘Stanford.’

The university was coeducational, in a time when most were all-male; non-denominational, when most were associated with a religious organization; and avowedly practical.

The Founding Grant states the university’s objective is “to qualify its students for personal success, and direct usefulness in life” and its purpose “to promote the public welfare by exercising an influence in behalf of humanity and civilization.”

On June 21, 1893, Leland Stanford died at his Palo Alto home at the age of 69.  For a decade following her husband’s death, Jane Stanford was the sole trustee of the University; she doted on the fledgling institution with “the commanding meddlesome love which an unbridled maternal instinct thrusts upon an only child.”  (Wolfe)

Jane involved herself in Stanford’s daily management, corresponding with Jordan on every operational matter. When she disapproved of a faculty member, she told Jordan to oust him. And when she began to second-guess some of Jordan’s decisions, she found a faculty confidant, German professor Julius Goebel, to keep a paper trail on him.  (Wolfe)

On June 1, 1903, Jane granted control of the university’s endowment and management to the Board of Trustees, although she remained a member of the board and continued to be involved in its operation.

By 1904, it appears that Mrs Stanford had lost her toleration for Jordan. In June, Goebel had reported in a letter to her that Jordan’s favoritism and political patronage were endangering faculty recruitment. In a letter to trustee Horace Davis, who was another in her inner circle, Goebel wrote that she had reached the point of “final remedy … the removal of the President.”  (Wolfe)

Then a small story appeared in a couple out-of-town papers, reporting on a January 14, 1905 incident, “… private detectives are working on an alleged attempt to murder Mrs Jane Stanford … in her home here, by placing poison in mineral water.”

“The contents vomited from the stomach and found in the water were analyzed and showed sufficient poison to kill a dozen people.”  (Spokane Press, February 18, 1905.)

Of the incident, Mrs Stanford said: “How dreadful if I had died that time. People might have thought I committed suicide.”  (The San Francisco Call, March 7, 1905)  Following the incident, she planned a trip.

“If I am not to stay in my San Francisco home, and as the wet season is coming on, rendering it inadvisable for me to go to my country residence, I prefer to go to Honolulu, as it is warmer there.” (Jane Stanford; San Francisco Call, March 7, 1905)

“Mrs Stanford arrived in Honolulu … accompanied by her maid and her secretary (Bertha Berner,) and went at once to the Moana, announcing that she had come here to rest for a few weeks.”

“She seemed, however, very cheerful and received the many friends who called on her in that spirit, although to one at least of the more intimate ones she threw aside her cheerfulness and spoke of the fears that beset her (the prior poisoning attempt.)”

“Mrs Stanford went on a drive to the Pali, and down into Koʻolau, where the party had a picnic dinner. Mrs Stanford ate very heartily, and seemed to enjoy every moment of the drive. The party returned to the Moana hotel, and at dinner time Mrs Stanford went into the dining room.”

“She did not remain more than three minutes, but made no complaint of feeling ill. In fact, she said that she felt remarkably well. … Leaving the dining room, Mrs Stanford sat on the lanai talking very cheerfully until bed, time. At a little after ten o’clock … she went to her room on the second floor of the hotel, and retired.”  (Pacific Commercial Advertiser, March 1, 1905)

“After Mrs. Stanford retired on February 28 I was aroused from my sleep by hearing my name called. I recognized Mrs Stanford’s voice calling out: “Bertha – May – l am so sick.’“

“We rushed out and found her clinging to the frame of her door. Mrs Stanford said: ‘Bertha, run for a doctor.’  Mrs Stanford walked two steps and then said: ‘Bertha, I am so sick.’“  (Bertha Berner; San Francisco Call, March 7, 1905)

Doctors were called; but Jane Lathrop Stanford died in room 120 of the Moana Hotel on February 28, 1905.  (The room numbering system has changed at the Moana Hotel; her room is still used in the hotel pool.)

After a 3-day Coroner inquisition, a unanimous verdict in less than two minutes was returned, “The Coroner’s jury to-night returned a verdict that Mrs Jane L Stanford died from … strychnine poisoning, the poison having been introduced into a bottle of bicarbonate of soda with felonious intent by some person or persons to the jury unknown.”  (San Francisco Call, March 10, 1905)

Dr Robert WP Cutter wrote a book, ‘The Mysterious Death of Jane Stanford,’ wherein he implies that Stanford’s President at the time, David Starr Jordan, was involved in a cover-up of the circumstances surrounding Mrs Stanford’s death.

Immediately following her death, Jordan was en route to Honolulu.  Jordan and Timothy Hopkins, Stanford Trustee, stated, “In our judgment, after careful consideration of all facts brought to our knowledge, we are fully convinced that Mrs Stanford’s death was not due to strychnine poisoning nor to intentional wrong doing on the part of any one.”  (Pacific Commercial Advertiser, March 16, 1905)

“We think it probable that her death was due to a combination of conditions and circumstances.  Among these we may note in connection with her advanced age, the unaccustomed exertion, a surfeit of unsuitable food and the unusual exposure on the picnic party of the day in question.” (Pacific Commercial Advertiser, March 16, 1905)

Jordan also said, “Dr Humphris (the hotel Doctor) and his associates don’t know what they are talking about.”  (Evening Bulletin, March 15, 1905) And later said, “Mrs. Stanford died a natural death in Honolulu”.  (Hawaiian Gazette, January 2, 1906)

However, Honolulu papers suggested a bribe, “Hopkins interviewed the physicians and told them that if things were satisfactory, their bills would be paid at once.”

“In different interviews it was plainly shown that it would be satisfactory … if the physicians could arrange to revise their findings and agree that poison had nothing to do with the tragedy, and, in that event the amount of the bills would not be questioned, but it happened that not one of the medical men could or would change what he had said In the first place.”  (Hawaiian Star, August 23, 1905)

The Stanford website, in telling the life story of Jane Stanford notes, while “Trace amounts of strychnine were found in her body and in her bottle of bicarbonate … Her cause of death was never conclusively determined.”  (Lots of information here from Stanford.)

© 2022 Hoʻokuleana LLC

by Peter T Young Leave a Comment

Island Summits

He ‘Ohu Ke Aloha; ‘A‘ohe Kuahiwi Kau ‘Ole
Love is like mist; there is no mountaintop that it does not settle upon

“… as the sun shining in his strength dissipated the clouds, we had a more impressive view of the stupendous pyramidal Mauna Kea, having a base of some thirty miles, and a height of nearly three miles.  Its several terminal peaks rise so near each other, as scarcely to be distinguished at a distance.”

“These, resting on the shoulders of this vast Atlas of the Pacific, prove their great elevation by having their bases environed with ice, and their summits covered with snow, in this tropical region, and heighten the grandeur and beauty of the scene, by exhibiting in miniature, a northern winter, in contrast with the perpetual summer of the temperate and torrid zones below the snow and ice.”

“The shores along this coast appeared very bold, rising almost perpendicularly, several hundred feet, being furrowed with many ravines and streams. From these bluffs, the country rises gradually, for a few miles, presenting a grassy appearance, with a sprinkling of trees and shrubs.”

“Then, midway from the sea to the summit of the mountain, appeared a dark forest, principally of the koa and ʻōhia, forming a sort of belt, some ten miles in breadth-the temperate zone of the mountain.”  (Bingham at first sight of the Islands, 1820)

And when you think about high elevation places in the Hawaiian islands, of course you have to talk about that basic dichotomy between the lower elevation places where people live.

And in old times, the lower elevations would have been called the Wao Kanaka. Wao being a word that means “zone” and “Kanaka” being a person. So the Wao Kanaka is a zone in which people belong.

When you rise above that zone, you enter into a realm in which all of the living things there are not there because of human activity. They flourish as the result of the activity of the gods, or the Akua. And so that zone is called the Wao Akua. And the transition from Wao Kanaka to Wao Akua is not taken lightly.  (Gon)

The Islands’ peaks are considered the piko (summit or center of the land) and are considered sacred.  The places upon which clouds nestle are considered wao akua, the realm of the gods.  Clouds cover the actions of the gods while they walk the earth. The higher the piko, the closer to heaven, and the greater the success of prayers. (Maly)

Let’s look at Hawaiʻi’s peaks, the highest point on each Island as we move down the Island chain.

Niʻihau – Pānīʻau (1,281-feet)

Ni‘ihau was formed from a single shield volcano approximately 4.89-million years ago, making it slightly younger in age than Kaua‘i. It is approximately 70-square miles or 44,800-acres.  It’s about 17-miles west of Kauaʻi.

Pānīʻau, the island’s highest point, is 1,281-feet; approximately 78% of the island is below 500-feet in elevation.   Located inside Kauai’s rain shadow, Ni‘ihau receives only about 20 to 40-inches of rain per year.  Ni‘ihau has no perennial streams.  (DLNR)

Kauai – Kawaikini (5,243-feet)

Geologically, Kauai is the oldest of the main inhabited islands in the chain. It is also the northwestern-most island, with Oʻahu separated by the Kaʻieʻie Channel, which is about 70-miles long. In centuries past, Kauai’s isolation from the other islands kept it safe from outside invasion and unwarranted conflict.

Near the summit (Kawaikini) is Waiʻaleʻale; in 1920 it passed Cherrapunji, a village in the Khasi hills of India, as the wettest spot on Earth (recording a yearly average of 476-inches of rain.)

Oʻahu – Kaʻala (4,025-feet)

The Waiʻanae Mountains, formed by volcanic eruptions nearly four-million years ago, have seen centuries of wind and rain, cutting huge valleys and sharp ridges into the extinct volcano.  Mount Kaʻala, the highest peak on the island of Oʻahu, rises to 4,025-feet.

Today, only a small remnant of the mountain’s original flat summit remains, surrounded by cliffs and narrow ridges. It’s often hidden by clouds.

Molokai – Kamakou (4,961-feet)

The island was formed by two volcanoes, East and West, emerging about 1.5-2-million years ago.  The cliffs on the north-eastern part of the island are the result of subsidence and the “Wailua Slump” (a giant submarine landslide – about 25-miles long that tumbled about 120-miles offshore – about 1.4-million years ago.)

Kamakou is part of the extinct East Molokai shield volcano, which comprises the east side of the island.   It and much of the surrounding area is part of the East Maui Watershed partnership and the Kamakou Preserve.  A boardwalk covers part of the rainforest and bog to protect the hundreds of native plants, birds, insects and other species there.

Lānai – Lānaihale (3,337-feet)

The island of Lānai was made by a single shield volcano between 1- and 1.5-million years ago, forming a classic example of a Hawaiian shield volcano with a gently sloping profile.  (SOEST)  The island of Lānai is about 13-miles long and 13-miles wide; with an overall land area of approximately 90,000-acres, it is the sixth largest of the eight major Hawaiian Islands.

“At the very summit of the island, which is generally shrouded in mist, we came upon what Gibson (an early (1861) Mormon missionary to the islands) called his lake – a little shallow pond, about the size of a dining table.  In the driest times there was always water here, and one of the regular summer duties of the Chinese cook was to take a pack mule and a couple of kegs and go up to the lake for water.”  (Lydgate, Thrum)

Maui – Haleakalā (10,023-feet)

Haleakalā was thought to have been known to the ancient Hawaiians by any one of five names: “Haleakalā,” “Haleokalā,” “Heleakalā,” “Aheleakalā” and “Halekalā.” (Hawaiʻi National Park Superintendent Monthly Report, December 1939)

Haleakalā is best known in stories related of the demi-god Māui; he is best known for his tricks and supernatural powers. In Hawaiʻi, he is best known for snaring the sun, lifting the sky, discovering the secrets of fire, fishing up the islands and so forth.  (Fredericksen)

Kahoʻolawe – Lua Makika (1,477-feet)

Kahoʻolawe is the smallest of the eight Main Hawaiian Islands, 11-miles long and 7-miles wide (approximately 28,800-acres;) it is seven miles southwest of Maui.  The highest point on Kahoʻolawe is the crater of Lua Makika at the summit of Puʻu Moaulanui, which is about 1,477 feet above sea level.

Located in the “rain shadow” of Maui’s Haleakalā, rainfall has been in short supply on Kahoʻolawe.  However, nineteenth century forestry reports mentioned a “dense forest” at the top of Kahoʻolawe.  Historically, a “cloud bridge” connected the island to the slopes of Haleakalā.  The Naulu winds brought the Naulu rains that are associated with Kahoʻolawe (a heavy mist and shower of fine rain that would cover the island.)

Hawaiʻi – Mauna Kea (13,796-feet)

Nani Wale ʻO Mauna Kea, Kuahiwi Kūhaʻo I Ka Mālie (Beautiful is Mauna Kea, standing alone in the calm) expresses the feeling that Mauna Kea is a source of awe and inspiration for the Hawaiian people. The mountain is a respected elder, a spiritual connection to one’s gods.   (Maly)

A significant pattern archaeologists note in their investigations is the virtual absence of archaeological sites at the very top of the mountain. McCoy states that the “top of the mountain was clearly a sacred precinct that must, moreover, have been under a kapu and accessible to only the highest chiefs or priests.”  (Maly)

ʻĀina mauna, or mountain lands, reflects a term used affectionately by elder Hawaiians to describe the upper regions of all mountain lands surrounding and including Mauna Kea.  (Maly)

© 2022 Hoʻokuleana LLC

by Peter T Young 1 Comment

Hanauma Bay

About 4-million years ago, the Waianae volcano started the formation of the island of Oʻahu. About 2.5-million years ago, the Koʻolau volcano erupted on the ocean floor, and continued to grow in elevation until about 1.7-million years ago.

More than 30 separate eruptions flowed out over the eroded landscape and onto the fringing reef about half a million years ago with a series of volcanic vents opened along the southeast shoreline of O‘ahu forming now-identifiable features including Diamond Head, Punchbowl and Hanauma Bay.

It’s not clear how the bay got its name, but there are several varying explanations.  In place names, hana refers to a bay or valley. Uma can have multiple meanings:

1) Uma can refer to a curve, as in the natural geological formation of the crescent shape of the bay.

2) Another meaning refers to the sport of hand-wrestling, uma, where opponents knelt with elbows on the ground and right hands locked together and tried to force the other down. Hanauma Bay was known as a place where ali‘i would gather to play uma, as well as other recreational activities.

“Queen Kaahumanu came by canoe and went to Hanauma where Paki was the konohiki over the realms of the [legendary] chiefesses Ihiihilauakea and Kauanonoula. These were the hula dancers, Mrs. Alapai, Mr. Hewahewa, and Mr. Ahukai, who gathered for the love of and to entertain royalty.”

“The men played the game of uma. One man gripped the hand of the other and pushed to get it down. Women joined in and a whole month was spent there. That was why the place was called Hanauma, a noted place.” (Reportedly in Hoku o Hawaii, February 11, 1930

3) The stern of a canoe is also known by the term uma. Traditional Hawaiian navigators would ride a strong current across the Ka‘iwi Channel from Ilio Point on Moloka‘i to Hanauma Bay with relatively little effort.

Thus, three suggested meanings for Hanauma Bay are: curved bay, hand-wrestling bay and canoe stern bay.

In 1928, the City and County of Honolulu established Koko Head Regional Park – the land encompassing Koko Head, Hanauma Bay and Koko Crater – by purchasing it from Bishop Estate. A deed restriction limited its use to public parks and rights of way.

In the 1930s the road along Hanauma Bay’s corner of Oahu was paved and a few other amenities provided that made it easier to visit the beach and reef. After closure during World War II, the Bay area reopened and became even more visitor friendly after blasting in the reef for a transoceanic cable provided room for swimming.

In 1956, the City sold the Hawaiian Telephone Company an easement through the bay for the first leg of a new trans-Pacific undersea telephone cable. A 200-foot wide channel was blasted through Hanauma Bay for the installation of the first trans-Pacific telephone cable reaching from Hawaiʻi to California.

Hanauma Bay became Hawaiʻi’s first Marine Life Conservation District (MLCD,) in 1967.  Established to conserve and replenish marine resources, MLCDs provide fish and other marine life with a protected area in which they can grow and reproduce.  While state laws restrict the taking of all marine life within the Hanauma Bay MLCD, snorkeling, diving, underwater photography and other similar passive activities are allowed.

More changes in the 1970s by the City cleared more area in the reef for swimming, made an additional parking lot, and shipped in white sand from the North Shore, leaving Hanauma Bay increasingly more attractive for daytime use.

By 1990 overuse of the beach and surrounding area was a real problem, with visitors walking on the reef, swarming the surrounding areas, and parking on the grass and on the sides of the road.

A few years later, in 1998, an admission fee was charged, further reducing the number of visitors. The city charges non-residents (now $7.50 per person) to enter the bay; Hawaiʻi residents get in free. Parking costs $1. Then in August 2002, the Marine Education Center was opened at the entrance to the bay.

Through a mandatory video and displays, all visitors to the park learn about reefs, the nature preserve and its rules, and how to protect the marine life.  The UH Sea Grant Hanauma Bay Education Program is an excellent model and example for effective on-site resource education and protection.

Through these programs, the marine life is protected and park visitors (whether residents or tourists) are provided guidelines for appropriate behavior in the marine environment.  The benefit goes beyond Hanauma, people can apply what they learn every time they enter the ocean.

© 2022 Hoʻokuleana LLC