Kilauea | Page 2 | Images of Old Hawaiʻi

April 11, 2023 by Peter T Young Leave a Comment

Whose Footprints Are These?

Geologic evidence suggests that the modern caldera of Kīlauea formed shortly before 1500 AD. Repeated small collapses may have affected parts of the caldera floor, possibly as late as 1790. For over 300-400 years, the caldera was below the water table.

Kilauea can be an explosive volcano; several phreatic eruptions have occurred in the past 1,200 years. (Phreatic eruptions, also called phreatic explosions, occur when magma heats ground or surface water.)

The extreme temperature of the magma (from 932 to 2,138 °F) causes near-instantaneous evaporation to steam, resulting in an explosion of steam, water, ash and rock – the 1980 eruption of Mount St. Helens was a phreatic eruption.

The 1924 eruption at Halemaʻumaʻu documents and illustrates the explosive nature of Kilauea. However, the 1924 explosions were small by geologic standards and by the standards of some past Kilauea explosions.

The hazards of larger explosions, such as those that took place multiple times between about AD 1500 and 1790, are far worse than those associated with the 1924 series. (USGS)

There were explosions in 1790, the most lethal known eruption of any volcano in the present United States. The 1790 explosions, however, simply culminated (or at least occurred near the end of) a 300-year period of frequent explosions, some quite powerful. (USGS)

Keonehelelei is the name given by Hawaiians to the explosive eruption of Kilauea in 1790. It is probably so named “the falling sands” because the eruption involved an explosion of hot gas, ash and sand that rained down across the Kaʻu Desert. The character of the eruption was likely distinct enough to warrant a special name. (Moniz-Nakamura)

At the time, Kaʻū Chief Keōuakūʻahuʻula (Keōua) was the only remaining rival of Kamehameha the Great for control of the Island of Hawaiʻi; Keōua ruled half of Hāmākua and all of Puna and Kaʻū Districts. They were passing through the Kilauea area at the time of the eruption. The 1790 explosion led to the death of one-third of the warrior party of Keōua. (Moniz-Nakamura)

Camped in Hilo, Keōua learned of an invasion of his home district of Kaʻū by warriors of Kamehameha. To reach Kaʻū from Hilo, Keōua had a choice of two routes one was the usually traveled coastal route, at sea level, but it was longer, hot, shadeless and without potable water for long distances. (NPS)

The other route was shorter, but passed over the summit and through the lee of Kilauea volcano, an area sacred to, and the home of, the Hawaiian volcano goddess Pele. Keōua chose the volcano route, perhaps because it was shorter and quicker, with water available frequently. (NPS)

In 1919, Ruy Finch, a geologist at the Hawaiian Volcano Observatory discovered human footprints fossilized in the Kaʻū desert ash. Soon, this area of the desert became known as “Footprints.”

Barefoot walkers left thousands of footprints in wet volcanic ash within a few miles southwest of Kīlauea’s summit.

Many historians and Hawaiians believe the footprints were made by Keōua and his warriors. Keōua was known to be in the area at the time, and previous thought suggested this part of the desert did not have pre-contact use, so it was narrowed down to them.

Scientists later investigated – one approach was to look deeper at the evidence.

Forensic studies indicate that the length of a human foot is about 15% of an individual’s height. A man’s foot may be slightly more that 15%, a woman’s slightly less, but it is possible to estimate the height to a couple of inches. (USGS)

They measured 405-footprints to determine how tall the walkers were. The average calculated height is only 4-feet 11-inches, and few footprints were made by people 5-feet 9-inches or more tall. Early Europeans described Hawaiian warriors as tall; one missionary estimated an average height of 5-feet 10-inches. Many now believe that most of the footprints were made by women and children, not by men, much less warriors. (USGS)

Meanwhile, Keōua’s party was camped on the upwind side of Kīlauea’s summit – perhaps on Steaming Flat – waiting for Pele’s anger to subside. They saw the sky clear after the ash eruption and began walking southwestward between today’s Volcano Observatory and Nāmakanipaio. (USGS)

Suddenly, the most powerful part of the eruption began, developing a high column and sending surges at hurricane velocities across the path of the doomed group. Later, survivors and rescuers made no footprints in the once wet ash, which had dried. (USGS)

Then, archaeologists looked for other evidence to help identify who the footprints may have belonged to. Contrary to general thought that the area was not used by the Hawaiians, archaeological investigations discovered structures, trails and historic artifacts in the area. (Moniz-Nakamura)

Most of the features were along the edge of the Keʻāmoku lava flow. Several of the trails converge south of the flow, suggesting a major transportation network. The structures are likely temporary, used as people were traversing through the desert on their way to/from Kaʻū and Hilo. (Moniz-Nakamura)

The sheer number of temporary shelters along the Keʻāmoku flow, as well as the trail systems and quarry sites, strongly suggest that this area was frequently used by Hawaiians travelling to and through the area – before and after the 1790 eruption. (Moniz-Nakamura)

If the footprints aren’t Keōua’s warriors, then how did one-third of his warriors die?

Several suggestions have been made: suffocation due to ash; lava, stones, ash and other volcanic material; or strong winds produced by the eruption, asphyxiation and burning killed them. (Moniz-Nakamura)

A more recent suggestion is that a “hot base surge, composed primarily of superheated steam … (traveling at) hurricane velocity” was the cause of death. The wind velocity prevented the people from running away; they probably huddled together, then “hot gases seared their lungs.” (Moniz-Nakamura)

Some now suggest that, if these observations and ideas are correct, the footprints were made in 1790, but not by members of Keōua’s group. (USGS)

A reconstruction of events suggests that wet ash, containing small pellets, fell early in the eruption, blown southwestward into areas where family groups, mainly women and children, were chipping glass from old pāhoehoe. They probably sought shelter while the ash was falling. Once the air cleared, they slogged across the muddy ash, leaving footprints in the 1-inch thick deposit. (USGS)

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 Kilauea and Mauna Loa on Hawaiʻi and Haleakalā on Maui.

Eventually, Kilauea 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.

In 1961, Hawaiʻi National Park’s units were separated and re-designated as Haleakalā National Park and Hawaii Volcanoes National Park.) (Lots of good information here is from USGS, NPS and Jade Moniz-Nakamura.)

January 13, 2023 by Peter T Young Leave a Comment

1960 Kapoho Eruption

The eruption in Kilauea Iki had ended on December 21, but the shallow reservoir beneath the summit of Kilauea volcano was gorged with magma. Rather than removing pressure, the eruption had, for all intents and purposes, created more.

The end of 1959 was an uneasy time for the staff at the Hawaiian Volcano Observatory. During the last week of the year, a swarm of earthquakes started in Pāhoa (more than 1,000 earthquakes were recorded by the Pāhoa station on January 12.)

The 1960 Kapoho eruption and its predecessor, the 1959 summit eruption in Kilauea Iki Crater, together formed a summit-flank sequence. The Kapoho eruption caused havoc in lower Puna, an idyllic rural community until the lava fountains and flows covered farm land and villages.

The size and frequency of the earthquakes increased; at 8 am, January 13, the ground was severely cracked along the fault through Kapoho town. Movement along the fault was literally pulling the town apart.

The ground was constantly shaking. The roughly 300-residents undertook voluntary evacuation, which was completed by early evening. At 7:35 pm, January 13, 1960, a red glow above Kapoho confirmed the start of the eruption.

Within half an hour, fountaining was nearly continuous along a nearly ½ – mile long fissure. After a couple hours, the activity focused with central fountains – for the next 11-hours powerful steam blasts roared from the vents.

The resulting fallout coated everything with a thin film of fine, wet, glassy ash. Salt crystals formed as the water evaporated; they testified to the brackish nature of the groundwater.

By noon on January 14, the steam blasts had ended and lava fountaining was confined to many sources along a 650-foot long section of the fissure. An ʻaʻa flow, 18-feet thick and nearly 1,000-feet wide reached the ocean – a bench formed 300-feet beyond the old shoreline.

In an attempt to save Warm Springs, bulldozers pushed a rock dike; shortly after, lava overtopped it and filled the pool.

Kapoho, a bit uphill of the fissure, was near all this activity but had not been touched by lava. Pumice and lava were wreaking havoc on nearby homes and farms (papaya, coconut, orchid and coffee groves.)

ʻAʻa continued to enter the ocean; it was also spreading southward. Bulldozers worked in forming a barrier to protect Kapoho, Kapoho School, an area of expensive homes and real estate at Kapoho Beach Lots. By January 20, lava had reached the barrier and overtopped it on January 23; a second barrier was shoved aside on January 27.

A third barrier held the flow, but lava then moved underground, beneath the end of the barrier, emerging near Kapoho School. The buildings began to burn at 10 am and the school was lost shortly after noon.

The barrier itself remained intact, and it survived until February 5, when it was finally overtopped and almost totally buried by lava that eventually covered the Kapoho cemetery. More coastal houses were lost.

Despite notable developments in the vent area, Kapoho village remained virtually intact except for a blanket of pumice and ash that covered everything.

For seven hours on the afternoon of January 27, the heaviest pumice fall of the entire eruption rained down on the area during strong kona winds.

However, it was the lava flow that would doom the town.

Late that night, the rapidly moving ʻaʻa flow moved through the streets, overwhelmed building after building. By midnight January 27, most of Kapoho had been destroyed; a couple days later (January 30) the town was gone.

The eruption ended slowly. Dribbles of lava continued to enter the sea north of Cape Kumukahi as late as February 13. High fountains continued until February 15, when lava was spraying upward from the main vent area to heights of 600-feet. It gradually subsided and on the morning of February 19, the eruption stopped.

Volcanologists concluded that the Kapoho eruption was tied to events at Kilauea’s distant summit. On January 17, four days after the Kapoho eruption had started, the summit began to subside (deflate, by analogy with a balloon) as magma was leaving the storage reservoir and heading down the east rift zone to the Kapoho area.

The eruption was the first during the modern era of volcano monitoring at Hawaiʻi Volcanoes Observatory. As a result, probably more fundamental ideas were reached from it than from any other single eruption in Hawaiʻi.

The main lesson, and really the only one that bears repeating over and over again, is clear. What happened then will happen again. That lesson should never be lost. (All information here is from USGS.)

October 5, 2022 by Peter T Young Leave a Comment

Hawaiian Volcano Research Association

“Keep and publish careful records, invite the whole world of science to co-operate, and interest the business man.” (Jaggar, 1913)

In contemplating the formation of a volcano observatory in Hawai‘i, Thomas Jaggar enlisted support from the Chamber of Commerce and the leading citizens of Honolulu.

In 1909, subscriptions were started by personal interview through the agency of Mr. Thurston and volunteer solicitors, after a lecture on volcanoes by Professor Jaggar, delivered at the University Club of Honolulu. A generous response came from a number of organizations and individuals.

The Chamber of Commerce appointed a committee to seek subscriptions in June, 1909. These were: Charles M. Cooke, Ltd., C. H. Cooke, Acting Director; Inter-Island Steam Navigation Co., Ltd., James A. Kennedy, General Manager; Mr. W. G. Irwin; Kilauea Volcano House, Ltd., E. W. Campbell, Treasurer; Hilo Rail Road Co., Lorrin A. Thurston, General Manager; Hawaiian Promotion Committee; Mr. George Wilcox; Mr. Aug. Knudsen and the Bishop Museum.

The founding of the Volcano Observatory and the formation of the group of subscribers called the “Research Association,” were themselves evolved productions of the inspiring work of early investigators, as well as of the natural intellectual stimulus created in man by the unexplained Kilauea lake of boiling nebulous flux.

October 5, 1911, at a well-attended meeting in the University Club, Honolulu, an informal organization of the Research Association was adopted and placed in the hands of a committee consisting of L. A. Thurston, chairman; A. F. Judd, representing the trustees of the Bishop Museum; President J. W. Gilmore, representing the College of Hawaii; C. H. Cooke, treasurer of the association; J. A. Kennedy.

Mr. Thurston at this meeting pointed out that there should be no break in the collection of records at Kilauea so well started by Mr. Perret, and suggested that a committee of five be appointed with power to act, to draw up a form of organization and to solicit subscriptions to help cover daily operations.

The persons who signed the subscription list of 1909 had been interviewed and had mostly expressed themselves as willing to renew their subscriptions. He reviewed the history of the observatory movement and then suggested that a voluntary, unincorporated, local organization be formed, to secure funds to carry on volcanic research; such funds to be administered and expended by an unpaid executive committee of five to be annually elected by the association.

The meeting of October, 1911 put the money-raising in the hands of the committee of five, and the estate of CM Cooke, Ltd. became guarantor of a fund of $5,000 annually, the actual subscriptions in Hawaii at first amounting to some three-quarters of that sum.

Mr. Jaggar by personal interviews raised $2,800 additional in 1912, assisted by a new subscription blank approved July 10, 1912, by the Honolulu Chamber of Commerce. In January of that year he had raised $1,785 in Hilo through the energetic assistance of Mr. Demosthenes Lycurgus, with the approval of the Hilo Board of Trade, this money being for the Observatory building.

A few small gifts have been made for special purposes such as the motorcar and certain specimens destined for the Bishop Museum.

The subscriptions are partly for five years, but many are renewable from year to year. Their motto was Ne plus haustae aut obrutae urbes (No more shall the cities be destroyed).

President Gilmore mentioned the many unsolved problems at the volcanoes and the necessity for continuous and concerted effort to collect data. He pointed out the extensive instrumental equipment which would be necessary and agreed for the College of Hawaii to give such assistance as its rules would permit.

Mr. Judd expressed great interest on the part of the Bishop Museum and undertook to investigate thoroughly what funds could be used to this end under the trust deed of that Institution.

Mr. C. H. Cooke, president of the Bank of Hawaii, deplored the multiplicity of organizations in Honolulu and expressed the belief that it would be to the welfare of all concerned if the Massachusetts Institute of Technology (MIT) would take the scientific responsibility of the work.

Governor Frear cited two main propositions as involved in the plan of work of the proposed Volcano Research Association, one concerning the scientific value of the work and the other the advertising of the Islands to the world.

He did not know whether the government could assist but it might profitably be brought before the legislature. He thought the project would be heartily endorsed by the Hawaiian members.

Mr. T. Clive Davies expressed the hope that the scientific motive would greatly dominate the publicity idea as he feared the “blighting hand of commercialism” would seriously interfere with good research.

The net result of this meeting was to establish an association for the private subscription of money to volcano research. Through this, the Hawaiian Volcano Observatory was formed.

According to its constitution, the name of this Association shall be the Hawaiian Volcano Research Association. The objects of this Association shall be:

To encourage and promote investigation of and research concerning volcanoes and volcanic phenomena, and all matters connected therewith or incidental thereto;
To establish and maintain an observatory at the Volcano of Kilauea, with subordinate stations at other points, from which investigation and research may be conducted, and at which records may be made and kept for the information of all, subject to the rules of the Association;
To invite scientific institutions and observers to make use of the buildings, apparatus and facilities of the Association, subject to the rules of the Association, and, so far as possible, to assist such institutions and observers in carrying on their work;
To promote the publication and dissemination of knowledge concerning volcanology and allied subjects, and to accumulate literature, photographs, models, maps and specimens, relating thereto, for the information of all, subject to the rules of the Association.

Membership was open to Any person, corporation, association or institution signing an application blank, whose name may be approved by the Board of Directors and who shall pay the dues prescribed by the Constitution, shall thereby become a member of the Association. (The membership dues shall be $5.00 per annum, payable annually in advance.)

Those who contribute to the support of the Association other than or in addition to the membership dues, shall be known as ”Patrons” of the Association.

The Hawaiian Volcano Observatory (HVO), in operation from July 1, 1912, under the direction of the Department of Geology of the Massachusetts Institute of Technology, in part, received initial funding from trustees of the Estates of Edward and Caroline Whitney.

The Whitney Fund provided $25,000 to the Massachusetts Institute of Technology where the principal and interest of the fund was for the conduct of research or teaching in geophysics.

MIT cooperated with the Hawaiian Volcano Research Association by becoming its largest subscriber for the five years, through the income of the Whitney fund and other payments. The Research Association’s funding support continued for several decades.

By December 1915, with Jaggar having worked in Hawai‘i for three years, the Research Association and MIT sent him to Washington DC to appeal to Congress to take over HVO as a government institution. In addition, the governor of Hawai‘i and the Honolulu Chamber of Commerce asked him to continue to push for the establishment of a national park. (Moniz Namakura)

The US Geological Survey (USGS) has operated HVO continuously since 1947. Before then, HVO was under the administration of various Federal agencies – the US Weather Bureau, at the time part of the Department of Agriculture, from 1919 to 1924; the USGS, which first managed HVO from 1924 to 1935; and the National Park Service from 1935 to 1947.

It currently operates under the direction of the USGS Volcano Science Center, which now supports five volcano observatories covering six US areas – Hawaiʻi (HVO), Alaska and the Northern Mariana Islands (Alaska Volcano Observatory), Washington and Oregon (Cascades Volcano Observatory), California (California Volcano Observatory), and the Yellowstone region (Yellowstone Volcano Observatory). (Information here is from various documents of USGS, HVO and NPS.)

November 28, 2017 by Peter T Young Leave a Comment

Halemaʻumaʻu

“Astonishment and awe for some moments rendered us mute, and like statues, we stood fixed to the spot, with our eyes riveted on the abyss below. Immediately before us yawned an immense gulf, in the form of a crescent, about two miles in length, from north-east to south-west, nearly a mile in width, and apparently eight-hundred feet deep.”

“The bottom was covered with lava, and the south-west and northern parts of it were one vast flood of burning matter, in a state of terrific ebullition, rolling to and fro its ‘fiery surge’ and flaming billows.” (Ellis, 1823)

In 1823, Reverend William Ellis visited Kīlauea caldera on his journey around the island of Hawaiʻi. He was the first foreigner to be shown the home of Pele.

By the time Ellis arrived, more than 300-years after the summit collapses of the late 1400s, the caldera had begun to refill. He measured the chasm from the highest rim to its depths; it was over 1,000-feet deep, with a series of terraces that stepped down to a vast inner crater that occupied nearly half the caldera’s floor. (NPS)

“Sometimes I have seen what is called Halemaʻumaʻu, or South Lake, enlarged to a circuit of three miles, and raging as if filled with infernal demons”. (Halemaʻumaʻu is lit., fern house.)

“On another occasion I found the great South Lake filled to the brim, and pouring out in two deep and broad canals at nearly opposite points of the lake.”

“The lava followed these crescent fissures of fifty or more feet deep and wide until they came within half a mile of meeting under the northern wall of the crater, thus nearly enclosing an area of about two miles in length and a mile and a half in breadth.”
(Coan)

According to Hawaiian oral tradition, the Kīlauea caldera formed during an epic battle between Pele, the Hawaiian volcano deity, and her younger sister, Hiʻiakaikapoliopele (Hiʻiaka.)

Pele had sent Hiʻiaka to fetch her lover, Lohiʻau, from Kauai. Upon returning, Hiʻiaka discovered that Kawahine‘aihonua (Pele, the woman who eats the land) had broken her promise and set fire to Hiʻiaka’s beloved ‘ʻōhiʻa forests.

To avenge this transgression, Hiʻiaka made love to Lohiʻau at the summit of the volcano, in full view of her sister. Pele lashed out in anger and buried Lohiʻau beneath a flood of lava.

Driven by remorse, Hiʻiaka dug furiously to recover the body. Rocks flew as she dug the great pit. Their brother stopped Hiʻiaka from digging deeper, for doing so would surely have let in water and put out the fires of Pele. Thus the great caldera of Kīlauea was formed. (NPS)

Within the heart of Kīlauea, a great reservoir swells with magma prior to an eruption. In the late 1400s, however, large volumes of magma erupted or moved elsewhere in the volcano, emptying the magma reservoir.

Its internal support withdrawn, the top of the mountain collapsed, accompanied by explosive eruptions. Great blocks of the old summit slumped inward. The gaping depression that formed was ringed with stepped terraces descending to its floor. (NPS)

The summit caldera (‘crater’) of Kilauea is 2-1/2 miles long and 2 miles wide and its floor has an area of approximately 2,600-acres. Near its southwestern edge the caldera floor is indented by the depression Halemaʻumaʻu, the ‘Fire Pit,’ a collapsed crater about 3,200-feet wide. (NPS)

Geologic evidence suggests that the modern caldera of Kīlauea formed shortly before 1500 AD. Repeated small collapses may have affected parts of the caldera floor, possibly as late as 1790. For over 300-400 years, the caldera was below the water table.

Kīlauea is an explosive volcano; several phreatic eruptions have occurred in the past 1,200 years. (Phreatic eruptions, also called phreatic explosions, occur when magma heats ground or surface water.)

There were explosions in 1790, the most lethal known eruption of any volcano in the present US. The 1790 explosions, however, simply culminated (or at least occurred near the end of) a 300-year period of frequent explosions, some quite powerful. (USGS)

Keonehelelei is the name given by Hawaiians to the explosive eruption of Kilauea in 1790. It is probably so named “the falling sands” because the eruption involved an explosion of hot gas, ash and sand that rained down across the Kaʻū Desert. The character of the eruption was likely distinct enough to warrant a special name. (Moniz-Nakamura)

The 1790 explosion led to the death of one-third of the warrior party of Kaʻū Chief Keōuakūʻahuʻula (Keōua.) At the time Keōua was the only remaining rival of Kamehameha the Great for control of the Island of Hawaiʻi; Keōua ruled half of Hāmākua and all of Puna and Kaʻū Districts. They were passing through the Kīlauea area at the time of the eruption. (Moniz-Nakamura)

Estimates of the number of fatalities range from “about 80 warriors” (William Ellis) to about “400 people” or “800 warriors” (Stephen Desha) to “5,405 countrymen” (David Douglas, quoting an eyewitness, a Priest of Pele, in 1834.) The lower numbers are probably most realistic. The dead were warriors and family members of Keōua’s army bound for Kaʻū. (NPS)

The next subsidence of the caldera floor occurred in 1868, when large earthquakes shook the southern part of Hawaii and simultaneous eruptions occurred from Mauna Loa and Kilauea. An area about 6,200-ft wide on the central caldera floor sagged about 330-ft, and a deeper conical pit about 900 m wide and about 3,000-ft developed at its southwest end at Halemaʻumaʻu. (USGS)

The pit again filled, and by 1874 a lava shield at Halemaʻumaʻu had once again grown to about the elevation of the southern caldera rim. Minor subsidences in and around Halemaʻumaʻu occurred again in 1879, 1886, 1891, and 1894.

The subsidence of 1894 was followed by 13-years of dormancy and very subdued, episodic activity within the pit of Halemaʻumaʻu. (USGS)

Lava returned to Halemaʻumaʻu shortly after the 1924 explosions ceased, but instead of being sustained the activity was now episodic. A series of seven brief eruptions in the next 10-years reduced the depth of Halemaʻumaʻu from 390 to 150 m, and then no eruptions occurred for 18 years, from 1934 to 1952.

Sustained eruption from June to November of 1952 filled Halemaʻumaʻu with another 120 m of lava. A brief eruption in May-June 1954 added 6 m of lava in Halemaʻumaʻu and a thin lava flow on the caldera floor to the east (Macdonald, 1955) (USGS)

The eruption of Kīlauea volcano continues at two locations. In the park, the vent within Halemaʻumaʻu Crater is easily viewed from the overlook at the Jaggar Museum. The second location is the Pu’u ‘Ō’ō vent located 10 miles east of the summit, on the remote east rift zone of Kīlauea. This area is not accessible to the public.

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Overlook at Jaggar Museum-Shiinoki

Kilauea’s summit caldera-Dzurisin-1980

Kilauea Aerial

‘Kilauea_Volcano’,_oil_on_canvas_painting_by_William_Pinkney_Toler,_c._1860s

Kilauea_Summit-Halemaumau-Klemetti

Kapiolani_Defying_Pele-(HerbKane)

Halemaumau-1930

Eruption column from Halemaumau. Photo by Tai Sing Loo at 1500 on May 23, 1924 from near Volcano house or HVO-(USGS)

0820. cloud is now over 3.7 km high-three lightning bolts observed in the column-(USGS)-1924

August 3, 2017 by Peter T Young 1 Comment

Kong Lung Store

The formation of Kilauea Plantation on Kauai goes back to the 1860s when American settler Charles Titcomb bought the ahupua‘a of Kilauea from Kamehameha IV for about $3,000 and moved there from Hanalei in 1863.

He had been growing sugar in Hanalei, but gave it up and built a homestead and cattle ranch at Kilauea which grew into the town of Kilauea. He later bought the adjoining ahupua’a of Nāmāhāna.

Kilauea Plantation began in 1877 with the planting and purchasing of mill equipment. EP Adams and Robert A Macfie Jr. (son of a Liverpool sugar refiner) were majority investors. William Green and Sanford B. Dole (later governor of Hawai‘i) held minority
interests.

In 1880 the four men incorporated the Kilauea Sugar Company as a Hawai‘i corporation, just a few years after the Reciprocity
Treaty between the Hawaiian Kingdom and the U.S. created a boom in sugar plantation development. (MacLennan)

Plantation life throughout the islands was centered on a landscape of buildings that reflected the system of tight control over workers and production. Typically, beyond the fields and mill, there was a plantation store, housing, medical, recreational facilities for the workers.

Ethnic groups included Portuguese, Puerto Rican, Hawaiian, Japanese, Chinese, Filipino, and Korean workers, and haole managers and supervisors. (MacLennan)

Lung Wah Chee was among the first group of Chinese immigrants that arrived on Kauai in 1876 to work for the Kilauea Sugar Company. He was born in Cheong Kong, China, September 15, 1860.

During 1894-1895 he had a contract with the Kilauea Sugar Company to load cane into cars with his own laborers. He was also required to furnish houses and firewood for the laborers. (NPS)

In the 1890s, Lung Wan Chee (aka LC Achee) operated a general merchandise store on the site of the Parish Hall (Japanese Language School) in Kilauea.

In 1902, Kilauea Sugar Plantation Co. decided to get out of the retail business and rented Chee their building; a bill of sale dated November 4, 1903, indicates that the plantation company sold to Kong Lung and Company a partnership for the sum of $8,534.29, including ‘all … the goods, wares and merchandise, stock-in-trade, show cases, scales, and Implements, in, upon and about the store.’ (NPS)

Later, Kong Lung Store moved into a former plantation building, it was the last of the stone structures built by the Kilauea Sugar Company. It was constructed around 1941 to replace an older wooden frame building at the same site.

The building measures 117-feet by 67-feet and is constructed of field stone up to the lower portion of the gable. The upper section is built of wood and has five ventilating jalousie windows at each end.

The store and the lanai are on a concrete slab. The front elevation is of five bays. The two end bays step forward, while the central three are an Inset lanai. The lanai has three stone piers which help to support the roof. Entrance to the store is through two screen doors.

The 1941 and later Kong Lung Store contained general merchandise, a barbershop, butcher shop, and post office. During the war, there was a lunch counter/diner to serve the many soldiers in the vicinity. Wages for store employees were about $40/month.

Workers for the store were said to have awoken at 2 am to work in the store. Then, at 5 am, they would go to work in the fields. Merchandise for the store arrived in the cane cars returning from Kahili Bay after delivering cane to freighters.

The raw sugar which was processed and bagged into 125 pounds at the mill was shipped to Honolulu by way of Kahili bay (or Kilauea Bay). The train hauled the sugar to Kahili then it was transferred on small boat then onto the Freighter which was anchored out in the bay.

The supplies for the Sugar Co and merchandise for Kong Lung Co. which was the only store in Kilauea at that time, came back by way of the empty cane cars. (Gushiken)

“Customers in the supermarket were plantation people. Groceries and dry goods, general hardware is what we went into. In those days, people were working six days a week, nine and ten hours a day. They would have no time for shopping. We had a delivery service then. No frozen goods.”

“The Sugar Plantation had its own dairy, between the store and the lighthouse. The slaughter was done there too. We had raw milk, no pasteurized. Everyone had their own vegetables, and rice was grown down in Kahili and Kalihiwai Valley and all the families made their own bread, raised their own chickens and pigs.” (Chow Lung, NOS)

The Store was managed by Kwai Chew ‘Chow’ Lung (son of the founder) and a partner. In 1955 they bought the building from the plantation and operated the business until 1979 when the property was sold to Tim King and Kelsy Maddox-Bell.

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