Images of Old Hawaiʻi

by Peter T Young Leave a Comment

Wai O Keanalele

“Wai o ke ola! Wai, waiwai nui! Wai, nā mea a pau, ka wai, waiwai no kēlā!”  (Water is life! Water is of great value! Water, the water is that which is of value for all things!) (Joe Rosa; Maly)

Water was so valuable to Hawaiians that they used the word “wai” to indicate wealth. Thus, to signify abundance and prosperity, Hawaiians would say waiwai.

“Kekaha wai ‘ole na Kona” (“waterless Kekaha of the Kona district”) speaks of Kekaha, the portion of North Kona extending north of Kailua Bay from Honokōhau to ʻAnaehoʻomalu.  It is described as “a dry, sun-baked land.”)

Kamakau notes during the 1770s, “Kekaha and the lands of that section” were held by descendants of the Nahulu line, Kameʻeiamoku (living at Kaʻūpūlehu) and Kamanawa (at Kīholo,) the twin half-brothers of Keʻeaumoku, the Hawai‘i island chief.

It is the home of Kamanawa, at Kīholo, and its fresh water resources that we look at today.

Situated within the ahupuaʻa of Puʻuwaʻawaʻa, this area has ancient to relatively recent (1801 Hualālai eruption and the 1859 Pu‘u Anahulu eruption.)

Kīholo (lit. the Fishhook) refers to the legend which describes how in 1859 the goddess Pele, hungry for the ‘awa and mullet, or ʻanae, which grew there in the great fishpond constructed by Kamehameha I, sent down a destructive lava flow, grasping at the fish she desired.  (DLNR)

This place name may have been selected as a word descriptive of the coastline along that part of the island where the east-west coast meets the north-south coast and forms a bend similar to the angle between the point and the shank of a large fishhook.

There is no confirmation for this theory, except for our knowledge that Hawaiian place names have a strong tendency to be descriptive.  (Kelly)

While only a handful of houses are here today, in ancient times, there was a village that with many more that called Kiholo home.

“This village exhibits another monument of the genius of Tamehameha (Kamehameha I.) A small bay, perhaps half a mile across, runs inland for a considerable distance. From one side to the other of this bay, Tamehameha built a strong stone wall, six feet high in some places, and twenty feet wide, by which he had an excellent fish-pond that is not less than two miles in circumference.”

“There were several arches in the wall, which were guarded by strong stakes driven into the ground so far apart as to admit the water of the sea; yet sufficiently close to prevent the fish from escaping. It was well stocked with fish, and water-fowl were seen swimming on its surface.” (Ellis, 1823)

Where it was feasible, sometimes in small embayments, and other times directly on the coastal reefs, Hawaiians built walled ponds (loko kuapā) by building a stone wall, either in a large semicircle – from the land out onto the reef and, circling around, back again to the land—or to connect the headlands of a bay, they enclosed portions of the coastal waters, often covering many acres.

These ponds provided sanctuaries for many types of herbivorous fish. One or more sluice gates (mākāhā) built into the wall of a pond allowed clean, nutritious ocean water and very young fish to enter the pond. This was the type of fishpond that was reported to have been built at Kīholo by early visitors to the area.  (Kelly)

While Ellis credits Kamehameha with building Ka Loko o Kīholo (The Pond of Kīholo,) it is more likely that the fishpond was built in the fifteenth to the early part of the seventh centuries and that Kamehameha later repaired and rebuilt it.  (Kelly)

It was in operation well after that.  “Took the road from Kapalaoa to Kailua on foot. Passed the great fish pond at Kīholo, one of the artificial wonders of Hawaiʻi; an immense work! A prodigious wall run through a portion of the ocean, a channel for the water etc. Half of Hawaii worked on it in the days of Kamehameha.”  (Lorenzo Lyons, August, 8, 1843; Maly)

Fishing and fish from the pond provided much of the food for the villagers.  In addition, due to the limited rainfall and no surface streams, they also planted sweet potatoes, at least seasonally (probably just before the winter rains were expected, whatever soil was available was piled in heaps and nourished with leaves and other vegetable matter.)  (Kelly)

Kīholo and other ponds (ie Pā‘aiea (once where the Kona Airport is situated)) would have supplied food for Kamehameha’s warriors when they sailed off in the great canoe fleet to conquer the chiefs on the Islands of Maui, Moloka‘i and O‘ahu in 1794 and 1795. (Kelly)

“The natives of this district (also produced) large quantities of salt, by evaporating sea water. We saw a number of their pans, in the disposition of which they display great ingenuity. They have generally one large pond near the sea, into which the water flows by a channel cut through the rocks, or is carried thither by the natives in large calabashes.”  (Ellis, 1823)

“After remaining there some time, it is conducted into a number of smaller pans about six or eight inches in depth, which are made with great care, and frequently lined with large evergreen leaves, in order to prevent absorption. Along the narrow banks or partitions between the different pans, we saw a number of large evergreen leaves placed.”

“They were tied up at each end, so as to resemble a shallow dish, and filled with sea water, in which the crystals of salt were abundant. … it has ever been an essential article with the Sandwich Islanders, who eat it very freely with their food, and use large quantities in preserving their fish.”  (Ellis, 1823)

“Salt was one of the necessaries and was a condiment used with fish and meat, also as a relish with fresh food. Salt was manufactured only in certain places. The women brought sea water in calabashes or conducted it in ditches to natural holes, hollows, and shallow ponds (kaheka) on the sea coast, where it soon became strong brine from evaporation. Thence it was transferred to another hollow, or shallow vat, where crystallization into salt was completed.”  (Malo)

The 1850s saw several outbreaks of lava from Mauna Loa: in August 1851; in February 1852 (it came within a few hundred yards of Hilo;) and in August 1855, when it flowed for 16-months.

Then, in 1859, activity shifted to the northwestern side of the mountain. A flow started on January 23rd at an elevation of 10,500 feet; it came down to the sea on the northwest coast in two branches, at a point just north of Kīholo. On January 31st the stream had reached the sea, more than thirty-three miles in a direct line from its source – the first eruption in historic times from a high altitude to accomplish the extraordinary feat.  (Bryan, 1915)

The 1859 flow basically destroyed Kīholo and transformed it from a former residence of chiefs to a sparsely populated fishing village.  In the early 20th century, Kīholo became the port for Puʻuwaʻawaʻa Ranch, some 10 miles inland near Puʻuanahulu. Cattle were shipped from Kīholo to Honolulu until 1958. The construction of Queen Kaʻahumanu Highway in 1975 ended Kīholo’s former isolation.  (Kona Historical Society)

What about the water?

Today, evidence remains of the fresh groundwater flow through subterranean lava tubes and chambers out into the bay.   There is a series of caves in Puʻuwaʻawaʻa that was formed from lava tubes. The ceilings of lava tubes often collapsed in some places and were left intact in others, forming caves with relatively easy access through the collapsed areas.

Such caves were used for shelters by Hawaiians, perhaps during the summer months when they came to gather salt or to fish. The place name Keanalele (the discontinuous cave) is descriptive of caves found just inland of the coast in the ahupua‘a of Pu‘uwa‘awa‘a between Kīholo and Luahinewai.

Some of the caves contain fresh or brackish water, particularly those located toward the makai (seaward) end of the cave series. Caves that contained water were precious to the inhabitants of the area, even if the water in them was slightly brackish.  (Kelly)  One of these is identified as Wai O Keanalele, with three feet of almost fresh water..

On January 25, 2002 the Board of Land and Natural Resources transferred responsibility for State-managed lands within the ahupua‘a of Pu‘uwa‘awa‘a and Pu‘u Anahulu from its Land Division to the Divisions of Forestry and Wildlife (DOFAW) and State Parks.

The portion that was made the responsibility of the Division of State Parks was designated the Kīholo State Park Reserve.  The Kīholo State Park Reserve is comprised of 4,362 acres and includes an 8-mile long wild coastline along the Kona Coast of the Island of Hawai‘i (bounded by Queen Kaʻahumanu Highway on the east, the Pu‘uwa‘awa‘a/Kaʻupulehu district boundary on the south, the shoreline on the west and the Pu‘u Anahulu/ʻAnaehoʻomalu ahupua‘a boundary on the north.)

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by Peter T Young 1 Comment

Nāhuku

Nāhuku (the protuberances) is a lava cave, or more commonly called a lava tube.

Lava tubes are natural conduits through which lava travels beneath the surface of a lava flow. Tubes form by the crusting over of lava channels and pāhoehoe flows.  When the supply of lava stops at the end of an eruption or lava is diverted elsewhere, lava in the tube system drains downslope and leaves partially empty conduits beneath the ground.  (USGS)

One of the most photographed lava tubes is Nāhuku in the Hawaiʻi Volcanoes National Park.  It was found in 1913 by Lorrin Andrews Thurston (July 31, 1858 – May 11, 1931,) a local newspaper publisher, a lawyer, politician and businessman.

Thurston was born and raised in the Kingdom of Hawaiʻi, grandson of the first Christian missionaries to Hawaiʻi. He played a prominent role in the overthrow of the Hawaiian Kingdom that replaced Queen Liliʻuokalani with the Republic of Hawaiʻi.

But this story is about a cave in Volcano, not politics.

Thurston first visited Kīlauea in 1879 at the age of 21 with Louis von Tempsky.  Thurston wrote that “we hired horses in Hilo and rode to the volcano, from about eight o’clock in the morning to five in the afternoon.”  (NPS)

Ten years later Thurston’s first mark upon the Volcano landscape appeared. In 1889, using his position as Minister of the Interior, he oversaw the construction of an improved carriage road from Hilo to Volcano.

The road was completed in 1894 allowing four-horse stages to transport visitors from Hilo to Volcano in seven hours. This feat would greatly increase the number of people able to view the volcano at Kīlauea.  (NPS)

The cave/lava tube he later found is also known as Keanakakina (Cave of Thurston – keana meaning cave and kakina the Hawaiian name for Thurston.)

“On Aug. 2nd a large party headed by LA Thurston explored the lava tube in the twin Craters recently discovered by Lorrin Thurston, Jr. Two ladders lashed together gave comparatively easy access to the tube and the whole party, including several ladies, climbed up.”

“No other human beings had been in the tube, as was evidenced by the perfect condition of the numerous stalactites and stalagmites. Dr. Jaggar estimated the length of the tube as slightly over 1900 feet. It runs northeasterly from the crater and at the end pinches down until the floor and roof come together…”  (Thayer, Kempe)

Thurston and George Lycurgus (Uncle George) were instrumental in getting the volcano recognized as Hawaiʻi Volcanoes National Park.  Starting in 1906, the two were working to have the Mauna Loa and Kilauea Volcanoes area so designated.  In 1912, geologist Thomas Augustus Jaggar arrived to investigate and joined their effort.

Jaggar had tried to lead several expeditions to the top of Mauna Loa in 1914 but was unsuccessful due to the elevation (13,678 feet) and the harsh conditions: rough lava, violent winds, noxious fumes, shifting weather, extreme temperatures and a lack of shelter, water and food.  (Takara)

On August 1, 1916, President Woodrow Wilson signed the country’s 13th National Park into existence – Hawaiʻi National Park.  At first, the park consisted of only the summits of Kīlauea and Mauna Loa on Hawaiʻi and Haleakalā on Maui.

Eventually, Kīlauea Caldera was added to the park, followed by the forests of Mauna Loa, the Kaʻū Desert, the rain forest of Olaʻa and the Kalapana archaeological area of the Puna/Kaʻū Historic District.

On, July 1, 1961, Hawaiʻi National Park’s units were separated and re-designated as Haleakalā National Park and Hawaii Volcanoes National Park.

OK, back to Nāhuku.

This 500-year old, 600-foot long (with ceilings between 10 and 30-feet) lava tube is accessed via a short trail down, through and around back to the starting point (overall, it’s about 1/3-mile and takes about 20-30-minutes.)  (The lava tube available for viewing is about 600-feet, the actual tube is approximately 1,500-feet.)

It is one of the very few readily-accessible lava caves/tubes for folks to see in Hawaiʻi.  The cave has two openings used as an entrance/exit for the trail. The primary entrance is reached via a bridge.  The cave/tube is lit with electric lights and has a flat rock floor.

The main entrance of the cave is near the top of the side wall of a closed depression. Its location is close to the margin of the Kilauea Iki section of the present-day Kilauea caldera-crater complex. This closed depression has the Hawaiian name Kaluaiki.  (Halliday)  The other entrance is a ceiling hole, caused by roof collapse much after the cave had cooled.  (Kempe)

Hawaiʻi Volcanoes National Park is worth seeing, and a stop at Nāhuku (Thurston Lava Tube) is worth making, even if you have seen it a million times before.  Enjoy this and other day hikes in the Park.

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by Peter T Young Leave a Comment

Worst Possible Place For A Forced Landing In The Islands

While there is no good place to crash land an airplane, in 1941 the crew of the Army’s B-18 Bolo (serial number 36-446, constructors number 1747) found what was described as the “worst place.”

Prior to September 18, 1947 (the time the US Air Force was formed,) military aviation was conducted by the Army or Navy.

But let’s step back a bit.

In 1935, a design competition and “fly-off” was held to select a replacement for the Martin B-10/12 the standard bomber then in service with the United States Army Air Corps (USAAC.)

Douglas developed the B-18 “Bolo” to replace the Martin B-10; the new model was based on the Douglas DC-2 commercial transport.  The B-18 prototype competed with the Martin 146 (an improved B-10) and the four-engine Boeing 299, forerunner of the B-17 Flying Fortress, at the Air Corps bombing trials at Wright Field in 1935.

Although many Air Corps officers judged the Boeing design superior, the Army General Staff preferred the less costly Bolo; contracts were awarded for 82-planes, the order was increased to 132 by June of 1936.

Although designated a reconnaissance and bomber aircraft, the Douglas B-18 flew other important missions.  Hickam B-18s towed targets for gunnery practice by the coast artillery ground troops.   The targets were attached to steel cables and reeled several hundred feet aft of the aircraft.   (Trojan)

Though equipped with inadequate defensive armament and underpowered, the Bolo remained the Air Corps’ primary bomber into 1941. Thirty-three B-18s were based in Hawaiʻi with the 5th Bombardment Group and 11th Bombardment Group.

One of those Hawaiʻi B-18 Bolos, piloted by Boyd Hubbard Jr, took off from Hickam Field at 7 pm February 25, 1941 for a routine inter-island night instrument-navigation training flight.  Three other B-18s trained with them that night.

Their flight path took them over the Island of Hawaiʻi.  While flying on instruments at 10,000-feet, Hubbard’s B-18 suffered a main bearing failure in the left engine.  Hubbard headed to Suiter Field, the Army’s auxiliary field (it is now known as Upolū Point Airport.)

Although all possible fuel and cargo was jettisoned, the aircraft was too heavily loaded to maintain altitude on one engine.  As the aircraft descended the other engine began sputtering.  The crew believed they were over the ocean at the time in heavy fog during the dark night.

Hubbard made a last split-second correction prior to the crash. As he later described it, the mountain just loomed up before him in the darkness and he just reacted. He pulled back hard on the wheel and the aircraft stalled and belly flopped into the thick underbrush.

The undergrowth was so dense the plane settled into it and did not slide forward very far.  The crew felt the plane hit the tops of some trees and skid for about 75 yards before coming to rest at about the 3500-foot elevation in a gulch on the side of the Kohala mountain.  (Trojan)

Lee Webster, a Flight Engineer on one of the other B-18s in the group, reportedly gave this account of the accident, “I was just becoming accustomed to the eerie feeling of night flying by the time we started our second leg of the triangle toward a point somewhere off the northern tip of the island and to this point radio contact led us to believe we were in good shape.”

“Suddenly that was shattered by a report from one of the other planes having engine problems and then soon after a report of engine failure and that they were losing altitude. We immediately broke off our mission to accompany the disabled aircraft into Hilo airport, but to make matters worse we flew into some very bad weather. After what seemed a short period of time we lost radio contact with them and when attempts to locate the lost plane became futile we returned to Hickam Field.”  (Trojan)

The next morning at dawn a search was launched from Hickam Field using 24 bombers.  The wreck was soon spotted and an airdrop from Army planes provided the downed crew with blankets, food and hot coffee.

At dawn the following day (Thursday, February 27,) a rescue team departed from Suiter Field (Upolū.)  Members of the rescue party included Fred C Koelling (leader,) Ronald May, Leslie Hannah, Melvin Johnson and Hiroshi Nakamura.  (Pacific Wrecks)

They took the Kohala Ditch Trail on horseback for 2 ½-hours, then had to cut a new trail on foot for 8-miles through marshland and heavy brush for another 4-hours before nearing the crash site.

Firing pistols into the air to attract the downed fliers’ attention; the air crew responded with a burst of bullets and shot flares into the air; after 12-hours, they reached the downed plane.  (Veronico)

Remarkably, only minor injuries were sustained by Hubbard and the crew (crew members were Co-Pilot 2nd Lt Francis R Thompson; Engineer SSgt Joseph S. Paulhamus; Radioman Pvt William Cohn; Crewman Pvt Fred C Seeger and Crewman Pvt Robert R Stevens.)

Airmen from Hickam later described the site as the “Worst possible place for a forced landing in the Islands.”  (Trojan)

Hubbard continued on with a distinguished career in the Army, retiring as Brigadier General and earning Legion of Merit with oak leaf cluster; Distinguished Flying Cross with oak leaf cluster; Bronze Star Medal and numerous other medals, badges and citations.  (He retired March 1, 1966; he died February 15, 1982.)

The plane sat since on the side of Kohala mountain, just west of Waimanu Valley.  While various internet reports suggest Pacific Aviation Museum acquired the plane and has plans to restore and display it, the Curator of the Museum noted to me that “the plane is not ours”.  It continues to sit on the slopes of Kohala in Hāmākua.

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Marine Dam

Marines and Sailors trained for what has been referred to as the toughest marine offensive of WWII. 1,300 miles northeast of Guadalcanal, the Japanese had constructed a centralized stronghold force in a 20-island group called Tarawa in the Gilbert Islands.

RADM Shibasaki, the Japanese commander there, proclaimed, “a million men cannot take Tarawa in a hundred years.”   Ultimately, the objective took 9,000 marines only four days (November 20 to November 23, 1943) – but not without a staggering 37% casualties.  US victories at Tarawa, New Guinea and the Solomon Islands marked a turning point in the war.

The Marines would reconstitute at Camp Tarawa at Waimea, on the Island of Hawaiʻi.  Originally an Army camp named Camp Waimea (when the population in town was about 400,) it became the largest Marine training facility in the Pacific following the battle of Tarawa.  

Pyramid tent cities and streets of long convoys of jeeps, trucks, half-tracks, tanks, artillery and amphibious ducks made up the formidable, but top secret, Camp Tarawa; over 50,000 servicemen trained there between 1942 and 1945.

A lasting legacy of the military presence in Waimea was an addition in the community’s drinking water system – “Marine Dam” – it’s still in use and is located above Waimea Town near the lower edge of the forest.

Marine Dam is a diversion dam in Waikoloa Stream at the 3,460-foot elevation, built during World War II by the US Engineering Department to supply water for the military encampment of several thousand Marines in Waimea.

Built in 1943, the 5-foot high dam captured stream water into a 12-inch lightweight steel clamp-on pipeline. In 1966, the steel pipeline was replaced by a more durable 18-inch ductile iron pipe.  A still basin and a cleanout were also added.

Today, the Marine Dam serves its original function and is a major source of drinking water for the South Kohala Water System, which provides drinking water as far east as Paʻauilo and west to the Waiemi subdivision on Kawaihae Road.

Hawai‘i County Department of Water Supply (DWS) relies on the streams of Kohala Mountain for its primary source of water.

The primary sources for the Waimea Water System are the mountain supplies from Waikoloa Stream and the Kohākōhau Stream diversion. The surface water sources are supplemented by the Parker Ranch groundwater well.  Surface water is treated at the Waimea Water Treatment Plant and blended with groundwater before distribution.

Raw water from the streams is stored in 4 reservoirs with a total capacity of over 150 million gallons (MG) and is treated in the DWS filtration plant. This system provides about 2-million gallons per day (mgd) (the system has a potential capacity of 4-mgd.)

There are three 50-million-gallon reservoirs in the Waimea system, although one of them is out of commission as a result of damage from the 2006 Kiholo Bay earthquake.  Two were initially damaged, but one has since been repaired.

The dam seems to also have helped native species; two Koloa ducks were observed on October 30, 1968 in a small pool of Waikoloa Stream approximately 400 yards above the Marine Dam, Kohala Watershed, and expressed the opinion that this was the “first sighting of wild Koloa on Hawaiʻi in more than 20 years”.

The work of the dam did not go unnoticed.  In 1997, the American Water Works Association designated the Marine Dam as an “American Water Landmark” (the only award for a neighbor island facility.)  Three other Water Landmark awards were issued to Kalihi Pump Station (1981,) Hālawa Shaft (1994) and the Beretania Pumping Station (1995.)

To receive a landmark status, the facility must be at least 50 years old and of significant value to the community.

DWS is permitted by the State’s Water Commission to take 1.427-mgd total from its diversions at the Marine Dam and Kohākōhau Dam, which is approximately 33% of the median daily discharge of Waikoloa and Kohākōhau streams combined.

The average or “mean” annual daily flow at Waikoloa stream is 9.12 cubic feet per second (cfs) (5.89 (mgd;)) however, this mean flow likely occurs only 20-30% of the time.

The median daily discharge for Waikoloa stream is 4.3 cfs (2.78 mgd.)  On a more typical day, streamflow is within the 70-75% range (meaning the percentage of time discharge equaled or exceeded this amount), or between 2.5-2.8 cfs (1.62-1.81 mgd.)  (MKSWCD)

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Ana Huna

Native Hawaiians believe ʻiwi (the bones) to be the primary physical embodiment of a person. Following death, ʻiwi are considered sacred, for within the bones reside the person’s mana (spiritual essence.) Mana was greatly valued, and native Hawaiians spent their lives maintaining and enhancing their mana. (Halealoha Ayau)

For native Hawaiians, it was important for the bones of a deceased person to complete their journey and return to the ground to impart their mana.

From island to island, community to community and family to family, there were many different ways to prepare bodies for burial. Each method was appropriate for the individual and his or her status.  Burial locations were one of the most secretive traditions in a culture over a thousand years old. (DLNR)

Sometimes the bones of the dead were dug up out of the burial grounds to be used for arrows for rat shooting and for fishhooks, and the bones and bodies of the newly buried were dug up for food and bait for sharks.

For this reason, surviving family members sought places of concealment for the bones of their grandparents, parents, children, chiefs and relatives. They searched for deep pits (lua meki) in the mountains, and for hiding pits (lua huna) and hiding caves (ana huna) along the deep ravines and sheer cliffs frequented by koa‘e birds.  (Kamakau; Kumu Pono)

For some, including the high aliʻi, often their ʻiwi were placed in secret burial caves (ana huna.)

A few of the notable areas burial areas with secret burial caves include, ʻIao Valley, Pohukaina, Pali Kapu o Keōua and the reported cave burial of Kahekili and Kamehameha at Kaloko.

ʻIao Valley (Maui)

For centuries, high chiefs and navigators from across the archipelago were buried in secret, difficult-to-access sites in the steep valley walls of ʻIao on Maui.

‘Iao Valley became a “hallowed burying place for ancient chiefs” and is the first place mentioned in the historical legends as a place for the secret burials of high chiefs.

Because this was sacred ground, commoners were not permitted to enter the valley, except for the Makahiki festival.  Some suggest the last burial was in 1736, with the burial of King Kekaulike.

Pohukaina (Oʻahu)

“There is only one famous hiding cave, ana huna on Oʻahu. It is Pohukaina… This is a burial cave for chiefs, and much wealth was hidden away there with the chiefs of old … Within this cave are pools of water, streams, creeks, and decorations by the hand of man (hana kinohinohiʻia), and in some places there is level land.”  (Kamakau)

Pohukaina involves an underground burial cave system that connects with various places around O‘ahu and is most notable as the royal burial cave at Kualoa. The opening in the Honolulu area is in the vicinity of the Kauikeaouli (Kamehameha III) residence (the grounds of ʻIolani Palace,) where also many of the notable chiefs resided.  (Kamakau; Kumu Pono)

The opening on the windward side on Kalaeoka‘o‘io faces toward Ka‘a‘awa is believed to be in the pali of Kanehoalani, between Kualoa and Ka‘a‘awa, and the second opening is at the spring Ka‘ahu‘ula-punawai.

On the Kona side of the island the cave had three other openings, one at Hailikulamanu – near the lower side of the cave of Koleana in Moanalua—another in Kalihi, and another in Pu‘iwa. There was an opening at Waipahu, in Ewa, and another at Kahuku in Ko‘olauloa.

The mountain peak of Konahuanui was the highest point of the ridgepole of this burial cave “house,” which sloped down toward Kahuku. Many stories tell of people going into it with kukui-nut torches in Kona and coming out at Kahuku.  (Kamakau; Kumu Pono)

Pali Kapu O Keōua (Kealakekua, Hawaiʻi Island)

Keōua (father of Kamehameha I) and Kalaniʻōpuʻu (aka Kaleiopuʻu & Kalaiopuʻu) were half-brothers, sons of Peleioholani.  During the illness of Keōua, at his residence in Hilo, a messenger was sent to Kaʻū to notify Kalaniʻōpuʻu of his brother’s illness; he immediately started for Hilo.

Keōua said to Kalaniʻōpuʻu, “Brother, I cannot live long, for our uncle Alapaʻinui has an evil disposition and is praying me to death. My only request to you is to take my young son Kamehameha and keep him with you, for some day he will become famous and will add luster to our lineage; do not neglect him.”

Kalaniʻōpuʻu sent for their kahuna; as soon as the kahuna saw Keōua he advised Kalaniʻōpuʻu to return home, as it was impossible for his brother to live.  (He died shortly thereafter; his remains were transported to Kona.)

On arriving at Kailua great preparations were being made for the mourning ceremonies. Wailing, removing the teeth, shaving the head, etc, took place. After these ceremonies Kalaniʻōpuʻu headed for Kaʻawaloa to await the remains of his brother Keōua from Hilo.

On their arrival they were deposited in a cave three-fourths of the way up the pali, whence it was called “Ka Pali Kapu O Keōua (at Kealakekua Bay.”)  (Diary of George Hueu Davis, the Son of Isaac Davis; Henriques)

Later, in 1829, Kapiʻolani “and Kaʻahumanu removed the bones of (Kapiʻolani’s) father, and more than a score of other deified kings and princes of the Hawaiian race, from their sacred deposit, – may be the “House of Keave” at Honounou, – placing them out of the way, in one of the caves high in the precipice at the head of the bay where she resided.”  (Anderson, 1864)

(A little side note on Pali Kapu O Keōua … while I was at DLNR, the 2006 Kohala earthquakes exposed a previously unknown burial cave on the side of the Kealakekua cliff.  Because we had concerns about keeping the cave secret, I asked FEMA to document this new cave in a separate, non-public report, aside from the general (public) earthquake damage report.  They agreed; the cave was subsequently sealed.)

Kaloko (Kona, Hawaiʻi Island)

An early traditional reference to the area in the late eighteenth century mentions the burial of Kahekili, the ruler of Maui, in a hidden cave at Kaloko. However, the most significant burial ceremony traditionally reported to have taken place there is that of Kamehameha, although there is no firm proof of this.  (NPS)

Following his death, Kamehameha’s bones were supposedly transported by canoe from Kailua to Kaloko, where the bearers of the royal remains met the man in charge of the secret burial cave, and together they placed the bones in the same depository used for Kahekili.

“Kaloko (pond) is another famous burial area; it is in Kekaha, Hawaii. (In a cave that opens into the side of the pond) were laid Kahekili, the ruler of Maui, his sister Kalola, and her daughter, Kekuʻiapoiwa Liliha, the grandmother of Kamehameha III. … This is the burial cave, ana huna, where Kameʻeiamoku and Hoapili hid the bones of Kamehameha I so that they would never be found.”  (Kamakau; NPS)

In 1887 King Kalākaua designated a man named Kapalu, who had guided him to a burial cave at Kaloko in which he supposedly beheld Kamehameha’s bones, as overseer and keeper of the “Royal Burial Ground” at Kaloko.

A year later Kalākaua wrote that he ordered Kapalu to retrieve the bones, which the king took to Honolulu and deposited in the Royal Mausoleum in Nuʻuanu Valley.  (Barrère; NPS)  (Questions remain as to where Kamehameha was buried.)

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