Diamond Head | Page 2 | Images of Old Hawaiʻi

February 4, 2022 by Peter T Young Leave a Comment

Built in About an Hour

The Hawaiian Islands were formed as the Pacific Plate moved westward over a geologic hot spot. Oʻahu is dominated by two large shield volcanoes, Waiʻanae and Koʻolau that range in age from two to four-million years old.

The younger volcanic craters are all less than 500,000 years old. They formed after Oʻahu had moved well off the hot spot and the main shield volcanoes had gone dormant for at least two-million years.

Scientists say Lēʻahi (Diamond Head) (one of these later eruptions) is a tuff cone, formed by hydromagmatic activity. Tuff is a volcanic rock made up of a mixture of volcanic rock and mineral fragments. Wherever there are explosive volcanic eruptions you can expect to find tuff. (SOEST)

A hundred years ago, Hawaiʻi missionary Reverend Sereno Bishop noted Diamond Head was made in less than an hour’s time and is “composed not of lava, like the main mountain mass inland, but of this soft brown rock called tuff.” (Bishop, Commercial Advertiser, July 15, 1901)

Others noted, “the duration of eruption of Diamond Head was of the order of five hours. The eruption may have been intermittent with interruptions sufficient to extend the whole period of activity to as much as five days, but probably not more.” (Wentworth, Bishop Museum, 1926)

“Volcanic eruptions may be distinguished into two classes, the effusive and the explosive. In the former the molten rock is poured out and covers the mountain slopes with great floods.”

“If you look up at the sides of yonder ravines (on the Koʻolau mountains,) which the rainstorms of many hundred thousands of years have worn out of the original dome-shaped mountain, you will see the back edges of the ancient lava streams lying in layers.”

“The tuff cones are entirely different, and are produced by very brief and sudden explosive eruptions. The tuff was violently shot high aloft into the air in the form of superheated mud. This hot mud cooled and thickened by the expansion of its water and its partial escape as steam before reaching the ground.”

“It hardened and cemented as it fell, though still liquid enough to form in thin layers or laminations as we see it lying around us at the base of the hill. … The tuff-fountain escaping from its confinement, at once expanded and spread out like a vast tree.”

“Here at Diamond Head, which is one mile in diameter, the bulk of the mud spread out half a mile in all directions before ending its fall. Thus a very exact circular ring was piled up of one mile in diameter. There was, however, another influence, that of a violent easterly-wind which deflected the entire fountain westward”.

“The wind also acted with especial force upon the highest part of the fountain, flinging and piling it up on the western side of the crater in a lofty cone. A large part of that cone has been weathered away by the impact of rainstorms upon the soft rock; but it still stands in a peak some 200 feet higher than the main run.”

“The vent or point of issue of the tuff-fountain must have been at the lowest point of the interior, where lies the present pond of water.” (Bishop, Commercial Advertiser, July 15, 1901) (The same series of eruptions produced Punchbowl and Koko Head Crater.)

Somewhat more than half of the craters of southeast Oahu are arranged in linear groups, those dominated by the craters Tantalus, Diamond Head, and Koko Crater. In the Diamond Head group is the main Diamond Head vent, Kaimuki crater and Mauʻumae crater.

(A cinder cone is a volcanic cone built almost entirely of loose volcanic fragments called cinders or pumice that accumulate around and downwind from a vent.)

(Cinders are glassy and contain numerous gas bubbles “frozen” into place as magma exploded into the air and then cooled quickly.) (USGS)

November 6, 2021 by Peter T Young 1 Comment

Portlock

Recent work that I have been involved with in the Portlock area on O‘ahu, reminded me of the namesake for the place, explorer and fur trader Nathaniel Portlock.

Nathaniel Portlock was born in about 1748 in Norfolk, Virginia, where his grandfather had emigrated, probably from the English south-west, around 1685. Nathaniel’s father died in 1752, leaving his wife Rebecca (formerly Ballard, who had previously been a widow with a daughter from a previous marriage).

Nathaniel’s father’s will left his property, and stay and board, to “my Daughter in Law Nancey Ballard a Negro … said children [Paul and Nathaniel] [and] their mother”.

After Portlock’s father’s death, his mother Rebecca quickly remarried a third time to a Richard Scott, who became guardian to her three surviving Portlock children and had others with her.

At about the age of 24, Nathaniel Portlock entered the British Royal Navy and was one of the loyal colonists of America, known as the “American Loyalists;” he later left that country on the close of the War of Independence.

(It is not clear what relationship a certain John Portlock had with Nathaniel; but John was born in 1765 in Shenandoah Co., Virginia and in 1781 volunteered to serve in the Virginia Regiment and fought and was “slightly wounded’ in the American Revolutionary War. It is an interesting situation if they are related.)

On March 30, 1776, he served as master’s mate on Captain James Cook’s third Pacific voyage aboard the Discovery. Portlock was transferred to the Resolution, also on the expedition, in August 1779.

Cook’s third and final voyage (1776-1779) of discovery was an attempt to locate a North-West Passage, an ice-free sea route which linked the Atlantic to the Pacific Ocean. Cook commanded the Resolution while Charles Clerke commanded Discovery. (State Library, New South Wales)

“Cook had chosen his subordinates well or had been lucky. The officers of the third voyage were a remarkably intelligent group of men.” (Captain Cook Society)

“All the great remaining voyages of the eighteenth century drew on Cook’s officers. Bligh, Portlock, Vancouver, Colnett, Riou, and Hergest all got their commands and served with great distinction. These men then passed on their skills to a second generation of men such as Flinders and Broughton.” (Mackay, Captain Cook Society)

Nathaniel Portlock and George Dixon, observed the commercial benefits that the development of the fur trade in the region could bring. In 1785, a group of London merchants formed the “King George’s Sound Co” (also known as Richard Cadman Etches and Company).

They proposed to carrying on the fur trade from the western coast of America to China, bringing home cargoes of tea from Canton for the East India Company. They bought two boats; Portlock and Dixon were selected to sail them (Dixon also previously sailed with Cook to Hawai‘i) and they set off on an expedition to North America to establish a foothold for fur trappers.

Portlock commanded the 1785-1788 expedition from the ship King George, while Dixon captained the Queen Charlotte. The purpose of the expedition was to investigate the potential of the Alaskan fur trade and to resume Cook’s search for a Northwest Passage through the continent.

The pair left England on August 29, 1785, and took nearly a year to reach Alaska, rounding Cape Horn and touching at Hawaiʻi on the way, first arriving off the coast of Kaʻū, May 24, 1786.

These were the first English ships to reach Hawai‘i following Captain Cook’s first arrival there in 1778. During the course of their 3-year expedition, they made three trips to Hawaiʻi.

A favorite anchorage on Oʻahu for Portlock was at Maunalua Bay (which Portlock named King George’s Bay). He named the Waikiki area (Diamond Head to Honolulu) Queen Charlotte’s Bay.

The East point of the Maunalua Bay (Koko Head) Portlock named Point Dick, “in honour of Sir John Dick, the first patron of this voyage,”) and the West point (Diamond Head) that Portlock named “Point Rose, after George Rose Esq. secretary of the treasury, the second worthy patron of our undertaking.” (Portlock)

Portlock also mentioned what is probably Kuapā Pond that he described as, “a little salt water river that has a communication with King George’s Bay.”

Portlock wrote about the early challenges of getting fresh drinking water in the region as they “found that we could not water at this place without an infinite deal of trouble …”

“… besides the danger of losing our casks, getting the boats dashed to pieces against the rocks, and the inconvenience of carrying our casks so far amongst a multitude of Indians, which would make it necessary to have an armed force on shore.”

“Towards evening the surgeon returned on board with the convalescents, and informed me, that the inhabitants had behaved in a very quiet inoffensive manner, though they were rather incommoded by the multitudes which curiosity brought about them.”

“By this time all our water from the ground tier was got to hand, and the cables coiled down. The inhabitants now brought us water in such plenty, that by noon on the 4th all our empty casks were filled”.

He noted, “As good water in any quantity may be procured at this island with the greatest facility for small nails and buttons, it undoubtedly must be the safest and most expeditious method any person can adopt who may chance to touch here, to barter for their water in the manner we did.” (Portlock)

“No chiefs of consequence paid us a visit as yet: the inferior chiefs indeed came on board without any scruple, and some of them slept with us every night. Amongst rest I had a daily visit from an old priest, who always brought by way of present, a small pig, and a branch of the cocoa-nut·tree.” (Portlock)

Maunalua was thought to be well-populated in ancient times. Maunalua was known for its offshore fishing resources, a large fishpond, and sweet potato cultivation. Taro was farmed in wet areas, sweet potato was grown in the drier regions and a series of fishing villages lined the coast. (McElroy) Part of that area now carries the Portlock name.

November 15, 2019 by Peter T Young Leave a Comment

Papaʻenaʻena Heiau

Hawaiʻi’s iconic landmark, Lēʻahi (Diamond Head) overlooks Waikīkī. Papaʻenaʻena heiau once stood on its western slope, overlooking the Waikīkī coastline. It was referred to by some early writers as “Lēʻahi heiau.”

“It consisted of a mana (supernatural or divine power) house approximately 50 feet long; an oven house (hale umu); a drum house; a waiea or spiritual house; an anuʻu or tower; a lele (altar) and twelve large images. The heiau was bordered by a rectangular wooden fence approximately six to eight feet tall with an eight-foot wide base, which narrowed to three feet at its apex.” (Ireland)

It is likely that the heiau was built in 1783 by Kahekili, the mōʻī (ruler) of Maui, as part of a victory celebration following Kahekili conquest of Oʻahu.

Surfing was one of the principal attractions for Waikīkī to both the chiefs and commoners who resided there. “Here at the ‘surfing heiau’ of Papaʻenaʻena, a terraced structure … is where surfers came to offer their sacrifices in order to obtain mana and knowledge of the surf.” (Kanahele)

When surf was ‘up,’ Kahuna at Papaʻenaʻena heiau reportedly flew a kite at the heiau as a signal to the people of the wave conditions. (Kanahele)

An ancient chant tells of Papaʻenaʻena and surfing:

There at Kalahuewehe is the big surf created by Papaʻenaʻena.
Arise, of ye surf of Kalahuewehe, arise! …
The kahuna of Papaʻenaʻena flies his moon kite
To proclaim the suitability of the sea for surfing.
The eager lookout on yonder highland
Anxiously scans the skies for this signal,
And relays the good news by runners;
Farmers, woodsmen, bird catchers all,
Leave their tasks and fetching their surf boards
Hurry to the beach at Waikiki.
Soon the sea is filled with natives
Sporting in the billowy surf;
Trick riding, zigging and zagging, amidst the foam,
Shouting words of defiance against the angry surf
To topple the rider if it can …. (Kanahele)

Papaʻenaʻena heiau was also a luakini heiau; human sacrifices were made at the terraced stone structure. The heiau was probably used for sacrificial or sacred purposes for 35 years.

Some historians believe that when Kamehameha I conquered ‘Oahu in 1795 at the Battle of Nuʻuanu, Kamehameha I used Papaʻenaʻena heiau to offer a sacrifice of his slain rival, Kalanikūpule, to his war god Kūkaʻilimoku.

After Kamehameha’s troops were overcome with dysentery in 1804, that stopped his attempt to conquer Kauaʻi, Kamehameha repaired Papaʻenaʻena heiau and offered in sacrifice 400 pigs, numerous coconuts and bananas and three kapu violators.

The heiau was also used for one (possibly its last) sacrifice. Kanihonui was killed and placed on the Papaʻenaʻena alter.

Kamehameha learned that Queen Kaʻahumanu had an affair with Kanihonui. He was a handsome 19-year old. Reportedly, Kaʻahumanu had seduced the boy while she was intoxicated; in addition, the boy was the son of Kamehameha’s half-sister – and, Kamehameha and Kaʻahumanu raised him.

George W. Bates, in 1854, describes a heiau at the foot of Lēʻahi (believed to be Papaʻenaʻena) as: “Just beyond Waikiki stand the remains of an ancient heiau, or pagan temple. It is a huge structure, nearly quadrangular, and is composed merely of a heavy wall of loose lava stones, resembling the sort of inclosure commonly called a ‘cattlepen.’”

“This heiau was placed at the very foot of Diamond crater, and can be seen at some distance from the sea. Its dimensions externally are 130 by 70 feet. The walls I found to be from six to eight feet high, eight feet thick at the base, and four at the top.”

“On climbing the broken wall near the ocean, and by carefully looking over the interior, I discovered the remains of three altars located at the western extremity, and closely resembling parallelograms. I searched for the remains of human victims once immolated on these altars, but found none; for they had returned to their primitive dust, or been carried away by curious visitors.”

Later (at about 1856,) Queen Emma ordered her workers to take rocks from Papaʻenaʻena heiau to build a stone wall around her property at Waikīkī.

During the Māhele the site was transferred to the future King Lunalilo. After the king’s death, this site was sold to James Campbell, in 1883. Later, Walter F. Dillingham bought the land from Campbell.

With the help of famed Chicago architect, David Adler, the Dillinghams built a home similar to the Villa La Pietra they admired in Tuscany while on their honeymoon – they named their new home La Pietra – meaning The Gem or The Rock.

After Walter’s death, La Pietra was sold to Hawaii School for Girls, who relocated their school there (1969.) The former Papaʻenaʻena heiau site is now the home for La Pietra – Hawaii School for Girls, an independent, college preparatory school for girls, grades 6 through 12.

When Papaʻenaʻena heiau stood on Diamond Head, it overlooked what is today First Break, the beginning of Kalahuewehe, a surfing spot famous for hundreds of years.

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Reconstruction-illustration-Papaenaena_Heiau-(NPS)

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Waikiki-Kaneloa-(Before Kapiolani_Park)-Lyons-Reg0306 (1876) (portion)-noting_Papaenaena

August 15, 2019 by Peter T Young 1 Comment

Camp McKinley

The Spanish-American War was a conflict in 1898 between Spain and the United States, effectively the result of American intervention in the ongoing Cuban War of Independence.

William McKinley was president of the United States, and the causal event was the explosion of the battleship USS Maine in Havana Harbor, Cuba on February 15, 1898.

So, what does that have to do with Hawai‘i?

Well, back then, Spain had interests in the Pacific, particularly in the Guam and Philippines. Although the main issue was Cuban independence, the ten-week war was fought in both the Caribbean and the Pacific.

Likewise, US foreign policy advocated the taking of the Caribbean Islands and the Philippine Islands for bases to protect US commerce.

Meanwhile, Hawai’i, had gained strategic importance because of its geographical position in the Pacific. Honolulu served as a stopover point for the forces heading to the Philippines.

On August 12, 1898, the United States ratified the Hawaiʻi treaty of annexation. At the time, there was no assigned garrison here until August 15, 1898, when the 1st New York Volunteer Infantry regiment and the 3rd Battalion, 2nd US Volunteer Engineers landed in Honolulu for garrison duty.

The two commands were initially camped alongside each other as though they were one regiment in the large infield of the one-mile race track at Kapi‘olani Park. The initial camp in the infield at the race track was unnamed.

As more members of the regiment arrived, the camp was moved about three or four hundred yards from the race track to an area called ‘Irwin Tract.’ The Irwin Tract camp was named “Camp McKinley,” in honor of the president.

The site “was near the only ocean-bathing beach on the Island and the reported site of a proposed Sanitarium selected by the resident physicians in the immediate vicinity of the best residential quarter of the Island. In addition it had shade in the park, a drill and parade ground on the racecourse, city water, and was accessible.”

The troops used the bathing facilities at the Sans Souci Resort which was located on the beach at the southeast corner of the park.

Camp Otis was a short-lived camp of Philippine expeditionary troops who arrived on the troop ship ‘Arizona’ on August 27, 1898 and were left in Honolulu when the ship went on to Manila.

The soldiers camped inside the racetrack at Kapi‘olani Park. The camp was later moved east within the racetrack to a point “nearly opposite Camp McKinley.” The camp was named after Major General Elwell S. Otis, US Volunteers, the commanding officer in the Philippines in 1898-99.

Camp Otis was abandoned about November 7, 1898 when the ‘Arizona’ returned and the troops departed for Manila.

Owing to the prevalence of malarial and typhoid fever, they moved the regiment to a camp to Wai‘alae, on the north side of Diamond Head, about three miles from “Camp McKinley.”

They temporarily occupied the Paul Isenberg estate which stretched from Kapahulu Avenue to Kāhala Beach. A letter from one soldier camped there noted, “The tents are pitched on the sandy beach at Waialie (sic)…”

The 2nd Engineers ultimately built barracks and other buildings for the new Camp McKinley just north of Kapi‘olani Park, between Leahi and Kana‘ina avenues (it is now covered by businesses along Kapahulu Avenue and residences in the area.)

Local hospitals were used for the sick soldiers until Independence Park Hospital was established on August 15, 1898. The Red Cross also established a hospital for soldiers in the Child Garden Building on Beretania Street in June, 1898.

The Independence Park Hospital was located in a dance pavilion at Independence Park, southeast of the corner of Sheridan and King Streets.

In October, 1898, concern over conditions at Independence Park Hospital and the large number of sick soldiers required that additional hospital space be obtained. The Independence Park Hospital was closed in January, 1899.

The Nu‘uanu Valley Military Hospital (also known as “Buena Vista Hospital”) was located at the former John Paty home (known as Buena Vista) on the east side of Nu‘uanu Avenue at Wyllie Street. (That site is now covered by the Nu‘uanu-Pali Highway interchange, just north of the Community Church of Honolulu.)

Camp McKinley remained in existence until Fort Shafter was opened in late June, 1907. The garrison was either artillery or coast artillery troops during this period.

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Camp_McKinley_Kapiolani_Park-1898

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Camp McKinley was set up in Kapi’olani Park, at the base of Diamond Head-NY_Volunteers-1898

Buena Vista Hospital, Honolulu, late 1898, looking east (US Army Museum)

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July 18, 2019 by Peter T Young 1 Comment

Lēʻahi

Lēʻahi, also known as Diamond Head, is a nearly circular crater of approximately two-thirds of a mile in diameter.

Diamond Head is different things to different people:
• Homes of Hawai‘i’s Kings, Queens and Royal Families were in its shadow
• It’s an internationally-recognized visitor industry icon
• It’s the backdrop to the famous Waikīkī Beach
• It served an integral role in the island military defenses
• It is present home and command center for State Civil Defense
• It’s an easy walk to the summit for spectacular views of the ocean and coastline
• It is a backdrop to a transformation of social, political and religious events

Diamond Head was given its name by British sailors who found natural calcite crystals on the slopes of the mountain and mistook them for diamonds. Hawaiians called the volcanic cone Lēʻahi, Laeʻahi or Lae-ahi. Translations include: “brow of the ʻahi” and “cape of fire.”

In the legend of Pele and Hi‘iaka, Hi‘iaka is said to have compared Diamond Head to the brow of the ‘ahi: Me he i‘a la ka Lae o Ahi; E kalali au ae nei i ke kai – Like a fish is the Brow-of-the-ahi Resting high above the sea.

Other names for Diamond Head include Point Rose (given to the geologic feature in 1786 by Captain Nathaniel Portlock in honor of the secretary of the British treasury), Diamond Hill and Conical Mountain.

Geologically speaking, Diamond Head is a dormant volcanic tuff cone, with a variable-height rim surrounding the recessed interior area; the eruption of Diamond Head took place well over 150,000-years ago.

The highest point (at 761-feet) on the southwest rim of Diamond Head is known as Lēʻahi Summit (most of the rim is between 400-500-feet.) The crater is on the southern coastline of Oʻahu, approximately one-and-a-half miles south of the Koʻolau range.

From at least the 15th century, chiefly residences lined the shore of Waikīkī, and cultivated fields spread across the Waikīkī plain to the foot of the crater and inland to the Ko‘olau valleys. There were several heiau in Waikīkī, of which several were located around Diamond Head.

One of Kamehameha’s main heiau (also suggested as a surfing heiau,) Papaʻenaʻena (also called Lēʻahi Heiau,) was situated at the base of the southern slopes.

Other heiau in the vicinity include Kupalaha Heiau, which may have been connected with Papaʻenaʻena, Pahu-a-Maui Heiau on the crater’s eastern cliffs overlooking the ocean (the site of the present Diamond Head lighthouse), Kapua Heiau near the present Kapiʻolani Park, and Ahi Heiau on the peak of Diamond Head.

In the early years of the 19th century, people tended gardens in the crater and one visitor described finding “an abundance of melons and watermelons growing wild, upon which we feasted”.

In 1831, the botanist, Dr. FJF Meyen, noted the crater contained a small pool of water “which was completely covered with plants”. (The crater pond was filled-in by military bulldozing; now, there is a seasonally-moist wetland where standing water can occasionally be seen.)

Some have suggested there is little likelihood for archaeological sites of pre-contact Hawaiian or early post-contact origin in the crater. The archival research suggests that the only Hawaiian activity that might have taken place in the crater was dryland farming (dating to 1822.)

In the Great Māhele division of lands between the king and his high chiefs, Diamond Head, which lies within the ¬ʻili of Kapahulu in the ahupua¬ʻa of Waikīkī, was awarded to William C. Lunalilo, the future king of Hawaiʻi (1873-1874).

In the early 1860s, Mark Twain commented, “On the seventh day out we saw a dim vast bulk standing up out of the wastes of the Pacific and knew that that spectral promontory was Diamond Head, a piece of this world which I had not seen before for twenty-nine years.”

“So we were nearing Honolulu, the capital city of the Sandwich Islands – those islands which to me were Paradise; a Paradise which I had been longing all those years to see again. Not any other thing in the world could have stirred me as the sight of that great rock did.”

In 1884, the Kapahulu portion of Lunalilo’s Māhele award was subdivided by the Lunalilo Estate. Diamond Head was transferred from the estate to the Hawaiian Government.

The summit of Lēʻahi affords an excellent and unobstructed view of the ocean from Koko Head in the east, to beyond the ʻEwa Plain to Wai‘anae in the west. The utility of Diamond Head did not go unnoticed by the U.S. Army.

In 1906, the US government acquired the 729-acres of Lunalilo’s property from the Hawaiian Government, as well as other adjacent lands (including Black Point), to create Fort Ruger Military Reservation, the easternmost of the coastal defense forts.

From 1963 to 2001, the FAA had its air traffic control facilities in Diamond Head crater, which guided Hawai‘i-bound aircraft from 250 miles outside the Islands to within 20 miles of their intended airport.

Diamond Head State Monument was first officially established under an Executive Order by Hawaiʻi’s Governor Quinn in 1962; nearly 500-acres of land now make up the Monument.

This early designation covered about 145-acres in a horseshoe configuration preserving the famous profile and the south and west exterior slopes from the crater rim down to Diamond Head Road. Subsequently, Executive Orders have added additional lands to the Monument.

The interior of the crater had been closed to the public from 1906 until 1968. (Remember the Sunshine Festivals back then?) In 1976, DLNR’s Division of State Parks became the agency responsible for the planning and management of the Monument – it is now open every day.

Two major tunnels (Kāhala Tunnel and Kapahulu Tunnel) provide pedestrian and vehicular access into the crater.

Two separate trail systems (interior and exterior) address different needs and purposes. The exterior trail system has a dual function as a jogging and bicycle path traversing the mauka end of the Monument and along the existing trail on the lower ʻEwa-makai slopes. The interior trail system leads to the summit of Lē¬ʻahi (1.6-mile round trip.)

Diamond Head is open daily 6 am to 6 pm, every day of the year including holidays, with entrance Fees of $5.00 per car or $1 per person for pedestrians (the money goes to State Parks.) Mountain Biking is not allowed on this trail. No dogs allowed in Diamond Head State Monument.

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