Images of Old Hawaiʻi

by Peter T Young Leave a Comment

For the Birds

“The spread of civilization and the utilization of wild lands, added to the destruction of animals for food, adornment, clothing, and sport, threaten the very existence of many species of native birds and mammals.”

“The necessity of regulating the killing of game was perceived early in our colonial history, and even the need of caring for our insectivorous birds found recognition about 1850.”

“Only in comparatively recent years, however, has the importance been recognized of protecting the large class of birds which, although they do not destroy insects or other creatures inimical to agricultural interests, are nevertheless worthy of preservation because of their beauty, grace, and harmlessness.”

“If such birds add nothing to our material wealth, they beautify the world and greatly increase the joy of living.”

“Though by no means the first to recognize the importance of protecting its wild life, the United States has taken a leading place among the nations of the world in this respect”

“One of the most efficient of the conservation measures adopted by the Government is the setting apart here and there of islands and sterile tracts of land, worthless for other purposes, upon which our native wild birds and mammals may live and perpetuate their kind for the pleasure and profit of our own and future generations.” (Yearbook of the US Dept of Agriculture, 1911)

“The National bird reservations under the care of the Department of Agriculture already number 51 and play a very important part in the preservation of our wild game and birds.”

“One of the most unique and interesting of these is the Hawaiian Islands Bird Reservation in the mid-Pacific, which, at certain seasons of the year, harbors millions of sea fowls that repair thither to establish rookeries and rear their young.”

“The following is the executive order setting apart this refuge:”

Executive Order No. 1019. It is hereby ordered that the following islets and reefs, namely: Cure Island, Pearl and Hermes Reef, Lysianski or Pell Island, Laysan Island, Mary Reef, Dowsetts Reef, Gardiner Island, Two Brothers Reef, French Frigate Shoal, Necker Island, Frost Shoal and Bird Island …”

“… situated in the Pacific Ocean at and near the extreme western extension of the Hawaiian Archipelago between latitudes 23° and 29° north, and longitudes 160° and 180° west from Greenwich, and located within the area segregated by the broken lines …”

“… are hereby reserved and set apart, subject to valid existing rights, for the use of the Department of Agriculture as a preserve and breeding ground for native birds.”

“It is unlawful for any person to hunt, trap, capture, wilfully disturb, or kill any bird of any kind whatever, or take the eggs of such birds within the limits of this reservation except under such rules and regulations as may be prescribed from time to time by the Secretary of Agriculture.”

“Warning is expressly given to all persons not to commit any of the acts herein enumerated and which are prohibited by law. This reservation to be known as the Hawaiian Islands Reservation.”  Signed by Teddy Roosevelt, February 3, 1909.

The names have changed, a bit, but the place remains the same.

“This refuge consists of a dozen or more islands, reefs, and shoals that stretch westward from the archipelago proper for a distance of upwards of 1,500 miles toward Japan. The average distance between them is something like 100 miles.”

“Some of them, like Necker, Bird Island, and French Frigate Shoal, are masses of volcanic rock thrust up out of the ocean and so steep and rugged as generally to be inaccessible to anything without wings.”

“Others are little more than diminutive sand spits, snatched from the grasp of ocean by the aid of coral animals. Still others are larger, and a few, like Laysan, being covered with sandy soil, are clothed with a more or less flourishing growth of shrubs, vines, and grasses.”  (Yearbook of the US Dept of Agriculture, 1911)

“As the islands are part of our National possessions and have been set apart as a bird reserve, the care and the protection of their avian inhabitants would seem clearly to devolve upon the Federal Government. It is true that their remoteness and inaccessibility render it difficult to guard them properly.”

“An effort, however, will be made to secure from Congress sufficient funds to provide for the services of a warden for Laysan and for an assistant. It is hoped also to secure a small power boat of adequate size to enable trips to be made between Laysan and the other islands and Honolulu.”

“These measures, if supplemented by an occasional visit from one of the Government cutters during the height of the breeding season, will insure the continued safety of the nesting colonies. From a variety of causes sea birds are being reduced in numbers almost everywhere, chiefly as the result of plumage hunting and of the growing scarcity of breeding sites.”

“Hence these island bird colonies, one of the wonders of the world, will become of increasing importance with each succeeding year. They should be regarded as a National heritage, and the birds be adequately protected, not only for the sake of our own citizens, but for those of other countries whose people go down to the sea in ships.”

“Otherwise these birds will suffer the fate that overtook those on Marcus Island, also one of our possessions, where, as reported by Bryan, in six years a colony of albatrosses almost as large as that of Laysan was reduced to less than a score of birds through the unchecked activities of feather hunters.” (Yearbook of the US Dept of Agriculture, 1911)

Unlike all other islands and atolls in the Northwestern Hawaiian Islands, Kure Atoll is the only land area owned by the state of Hawaiʻi – all of the other Northwestern Islands are owned by the US government.

While I was at DLNR, we created Refuge rules that established “a marine refuge in the Northwestern Hawaiian Islands for the long-term conservation and protection of the unique coral reef ecosystems and the related marine resources and species, to ensure their conservation and natural character for present and future generations.“ 

This started a process where several others followed with similar protective measures.  The BLNR unanimously adopted the State’s Refuge rules, President George W Bush declared it a Marine National Monument and UNESCO designated it a World Heritage Site. 

To me, this action reflects the responsibility we share to provide future generations a chance to see what it looks like in a place in the world where you don’t take something.

One of the issues about the rules, and in protecting the place, relates to access.  Due to the sensitivity of the area, permits are limited – so, rather than taking the people to the place, there are tools now in place to bring the place to the people.

© 2022 Ho‘okuleana LLC

by Peter T Young 1 Comment

Wahiawā

During ancient times, various land divisions were used to divide and identify areas of control. Islands were divided into moku (districts;) moku were divided into ahupuaʻa. A common feature in each ahupuaʻa was water, typically in the form of a stream or spring.

The Island of Oʻahu has six Moku: Kona, Koʻolaupoko, Koʻolauloa, Waialua, Waiʻanae and ʻEwa. The Waiʻanae ahupuaʻa, within the moku has an un-typical shape – it is sometimes referred to in two parts: Waiʻanae Kai, on its western side, runs from the ocean to the Waiʻanae Mountains (like a typical ahupuaʻa – this portion of Waiʻanae runs from the mountain to the sea.)

From there, however, the section referred to as Waiʻanae Uka continues across Oʻahu’s central plain and extends up into the Koʻolau Mountains – extending approximately 15-miles from the Waianae Mountains to the Koʻolau Mountains and ends up overlooking the windward coastline. (Each section is within the same ahupuaʻa.)

Wahiawā, situated in Waiʻanae Uka, was from very ancient times, identified with the ruling aliʻi of Oʻahu. The name breaks down to Wahi (place), a (belonging to), wa (noise.) (Handy)

Perhaps the name goes back to the time when Hiʻiaka was in this general area and could see waves dashing against the coast afar off and hear the ocean’s ceaseless roar… (Handy)

The chiefs of Līhuʻe, Wahiawā, and Halemano on Oʻahu were called Lo chiefs, poʻe Lo Aliʻi (”people from whom to obtain a chief”,) because they preserved their chiefly kapus…

They lived in the mountains (i kuahiwi); and if the kingdom was without a chief, there in the mountains could be found a high chief (aliʻi nui) for the kingdom. Or if a chief was without a wife, there one could be found – one from chiefly ancestors. (Kamakau)

A “sizable population” filled the Wahiawā area in traditional Hawaiian times, based on the “various areas of loʻi northwest of the present town of Wahiawā. … There were extensive terraces that drew water from Wahiawā Stream, both above and below the present town.”

“There were many small terrace areas along the sides of the valleys of all the streams of this general area. … The peculiarity of this area, apart from distance from the sea, is that it is the only extensive level area on (Oʻahu.)” (Handy)

In more modern times, at the height of the sandalwood boom, Kamehameha was buying foreign ships, including six vessels between 1816 and 1818, to transport his own wood to the Orient. (Kuykendall) According to Kamakau, Wahiawā was a prime source for the valuable wood; the largest trees were from Wahiawā.

Over the remainder of the decade, the population fluctuated. Things changed at the end of the decade. Following the overthrow of the Hawaiian monarchy, western military and agricultural interests would transform the Wahiawā landscape.

Land that had previously been leased to Oʻahu businessman James Robinson for cattle grazing was designated Wahiawā homestead land by The Land Act of 1895 (as homestead land, including water rights from the Kaukonahua Stream (not DHHL homestead, this was for general homesteading.))

Then, in 1897, Californian, Byron Clark, became the Hawaiian Republic’s commissioner of agriculture. In looking for land for him to settle on, he learned of the availability of land at Wahiawā.

Clark organized a group of other Californians (as well as others) to join him in settling the whole tract of thirteen hundred acres — which became known as the Wahiawā Colony Tract. Having formed an agricultural cooperative called the Hawaiian Fruit and Plant Company, the homesteaders began formalizing and refining the physical organization of their Wahiawā settlement.

To reach Wahiawa, the homesteaders forded the north and south forks of Kaukonahua Stream which surrounds Wahiawa, making it an island within an island. Life was hard but they cleared the land and planted their required fruit trees and crops.

They built a one-lane bridge, constructed homes, laid out roads, obtained water rights, built a store and post office, and saw to it their children were educated. In a very short time the homesteaders had a community and started the pineapple industry.

Clark found some discarded pineapple slips which he shared with Alfred W Eames and in 1900 they harvested their first crop in the community. Clark experimented in his home kitchen to can the fruit in glass jars.

Eames founded the Hawaiian Island Packing Company and built his first cannery in the Wahiawā heights area in 1902. This company was later known as Del Monte Fresh Produce (Hawaii) Inc.

Another homesteader and planter, Will P Thomas, operated under the Thomas Pineapple Company, which in 1917 following his death, became Libby McNeill & Libby of Honolulu.

Initially each settler lived in a house on his five-acre parcel in the town site and farmed his other land in the surrounding area. It was soon discovered, however, that each settler preferred to reside on his own farmstead, holding his town lot in reserve.

The homesteaders abandoned the village plan and agreed that one man, Thomas Holloway, would live on their 145-acre central lot site.

On August 27, 1902 a trust deed, referred to as the Holloway Trust, formally set aside the central town lots for the use and benefit of the Settlement Association of Wahiawā resident landowners. Within a few years, Wahiawā Town was underway.

Some of the town’s streets would be named for the early homesteaders – including Clark, Kellogg, Thomas and Eames streets (initial mapping shows California Avenue as the first, and main, road.)

Another notable change at this time was the result of a presidential order of July 20, 1899 setting aside Waianae Uka lands as the military reservation. Ten years later, in 1909, these lands would become the site of Schofield Barracks, named after Lt. General John M. Schofield.

Another homesteader to the area was James D Dole, who moved to Wahiawā in 1900 to attempt farming on 61-acres. Dole described Wahiawā at the beginning of the 20th century as “a park-like stretch of some 1,400-acres of third-class pasture land, dotted with shacks of 13 hopeful homesteaders for whom (the) general sentiment was merely pity.”

Dole founded Hawaiian Pineapple Company in 1901. He built a cannery next to his pineapple fields in Wahiawā and packed his first cans in 1903. By 1904, Wahiawā was known as “The City of Pines” and was considered the “hub” of the pineapple industry in the world.

Within a few years pineapple production at Wahiawā had increased that Dole planned a cannery at Iwilei, near the shipping facilities of Honolulu Harbor. Today his Hawaiian Pineapple Company (HAPCO) is known as Dole Food Company, Hawaii.

In order to transport the pineapple from Wahiawā to Honolulu, Dole persuaded the Oʻahu Railway & Land Company to extend its rail line to Wahiawā. The line to Wahiawā was constructed in 1906.

Another change occurred on January 23, 1906 when the Wailua Agricultural Company, later known as Waialua Sugar Company, constructed the Wahiawā Dam and Reservoir, a 2.5-billion-gallon capacity reservoir (the largest in Hawaiʻi;) it is generally known as Lake Wilson, today.

Another “story that has never been told in Hawaii” were the events of December 7, 1941 in Wahiawā. While the incident is usually called “the bombing of Pearl Harbor,” other areas on O‘ahu were also shelled. In Wahiawā two civilians died, 22 were injured, and two houses were burned down.

Sixty-seven-year-old Soon Chip Kim was sitting in a Wahiawa plantation cafeteria when the town was fired upon. The bullets went through the roof, killing Kim.

Richard Masaru Soma, 22, was waiting at a bus stop on Kamehameha Highway for a ride to go fishing with a friend when Wahiawā town was strafed by enemy fire. Soma was injured and died five days later. (Napoleon)

In addition to the two civilian casualties, 22 people were injured in Wahiawā. Dr. Merton Mack, who Purnell said was the only physician in town at the time, treated the injured at his clinic on the corner of California Avenue and Kamehameha Highway.

The enemy also suffered casualties in Wahiawa. According to Purnell, a Japanese plane, engaged in a dogfight with an American plane, was hit and crashed into the Hawaiian Electric substation on Neal Avenue, killing the pilot and co-pilot. On its way down, the plane clipped a house, setting it ablaze. The fire spread to a neighboring home, destroying both buildings.

The start of World War II further helped to accelerate developments within Wahiawā to accommodate the needs of the growing military population. Wahiawā Elementary School, which started in 1899 to educate children of farmers who were brought in from California, closed their doors in the 1940s to become the new Wahiawā General Hospital.

At the end of World War II, the facility continued to remain in operation under the leaders of the Wahiawā Hospital Association. The 72-bed acute care facility was dedicated in 1958, under the official name, Wahiawā General Hospital.

Post World War II, the old Wahiawā Hotel had been used as living quarters for area school teachers. By the 1960s, Wahiawā teachers, who had been quartered at the teachers’ cottages (as they referred to them), were forced to relocate as plans for the new Wahiawā Branch Library were underway; the library opened on July 19, 1965. (Lots of information here from Cultural Surveys and Wahiawā Historical Society.)

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by Peter T Young 1 Comment

Kaneʻaki Heiau

The ahupuaʻa of Mākaha, between Waiʻanae Ahupuaʻa to the southeast and Keaʻau Ahupua‘a to the northwest, extends from the coastline to the Waiʻanae Range

Earliest accounts describe Mākaha as a good-sized inland settlement and a smaller coastal settlement.  These accounts correlate well with a sketch drawn by Hiram Bingham in 1826 depicting only six houses along the Mākaha coastline.

Green describes Mākaha’s coastal settlement as “…restricted to a hamlet in a small grove of coconut trees on the Keaʻau side of the valley, some other scattered houses, a few coconut trees along the beach, and a brackish water pool that served as a fish pond, at the mouth of the Mākaha Stream.” (Cultural Surveys)

This stream supported traditional wetland agriculture – kalo (taro) – in pre-contact and early historic periods

Supporting this, Māhele documents note Mākaha’s primary settlement was inland where waters from Mākaha Stream could support lo‘i and kula plantings. Although there is evidence for settlement along the shore, for the most part, this was limited to scattered, isolated residents.

One of the best preserved heiau on Oʻahu is situated inland in Mākaha Valley.

It was originally built possibly as a Lono class agricultural heiau, probably around AD 1545. Unlike many other ancient religious sites, it remained intact after the Hawaiian religion was overthrown. (Apo)

Mākaha Stream, a focal point of the ahupuaʻa, gave life to the valley in both ancient and modern times. After six reconstruction phases, Kaneʻaki Heiau was transformed into the present day Luakini class structure. This final phase, imply direct reference to a paramount chief having commissioned and participated in the event, since only he/she could build such a heiau.  (WaiʻanaeHawaiianStudies)

Excavation data suggests that Kaneʻaki Heiau was in major operation for centuries, beginning in AD 1545. The last phase of construction occurred during Kamehameha’s campaign to unite the islands (1795-1810.)  (WaiʻanaeHawaiianStudies)

When the kapu system was overthrown, Kaneʻaki Heiau, unlike many other ancient religious sites, remained intact. In time, two restoration projects (one from 1969-70 and the other from 1996-97) were completed in order to retain the physical, spiritual and historical aspects of Kaneʻaki Heiau. (WaiʻanaeHawaiianStudies)

Nearby is a huge stone, “Pohaku O Kāne” (Stone of Kāne). This is one of the forms of the god Kāne, the uppermost of the four major gods, was worshipped by the many ʻohana that lived that ahupua’a. In modern times, it has come to be regarded as the guardian over the heiau and is still venerated by some people.  (WaiʻanaeHawaiianStudies)

Earlier restoration was completed in 1970.  A terrace and platform temple was first constructed on this site about 1545. It underwent six alterations, becoming ever larger and more sophisticated. (NPS)

Tradition says that in 1795 Kamehameha ordered that Kaneʻaki be transformed into a war heiau to insure his final conquest of Kauaʻi (Kaʻena Point, nearby, points directly at that island).  (NPS)

Supposedly those who started restoring the temple in the 1940s used Puʻukohola Heiau (at Kohala on the Big Island) as a model for the placement of the houses and idols. (NPS)

Bishop Museum staff supervised the restoration. There is a low terrace from which observers watched the ceremonies, the large hale mana for the priests on the upper platform alongside the smaller hale pahu, with an altar on pole legs between them.  (NPS)

Behind the altar is the god figure flanked by two prayer towers. These structures were reconstructed on the basis of postholes found in the stone platform.  (NPS)

Waiʻanae School Hawaii Studies Program suggests the following General Protocol Guidelines.

Kaneʻaki Heiau remains a significant place of culture to this very day. Therefore, it is very important to establish guidelines that will ensure the preservation of this sacred site, and to protect those that come to visit.  (WaiʻanaeHawaiianStudies)

  • Your approach to Kaneʻaki Heiau should be very respectful and treated as though you are in the house of god. You may be greeted and briefed by members of Hui Mālama O Kaneʻaki. Then you may proceed to the heiau trail. 
  • Unnecessary noise should be avoided or limited to the lower areas (parking/lawn area).Only guides may speak. 
  • Absolutely no entry allowed onto the main platforms. 
  • You must remain on the trail established by guides. Let your eyes and ears do the touching and not your hands. 
  • The following list of hoʻokupu are considered acceptable offerings: Maiʻa (Hawaiian banana), Awa, Niu, Kumu, Wauke, ʻOhe, Kalo, Ipu or Lua Ki. These offerings should be made in their natural state and not “prepared.” But no hoʻokupu, other than the personal mana you share with us today, is better than inferior offering.  (WaiʻanaeHawaiianStudies)

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by Peter T Young Leave a Comment

Growing Pains

Oʻahu is about 382,500-acres in size; the district of Puna on the island of Hawaiʻi is about 320,000-acres in size – almost same-same.

According to the 2020 census, Oʻahu has about 984,000-people and Puna has about 46,800.  That means there are less than a half-acre per person on Oʻahu and about 7-acres per person in Puna.

For some, it sounds like optimal living; and, many are moving to the Big Island to enjoy this rural lifestyle.

Open spaces with room to roam, it sounds kind of like the Wild West.  And, for some, that’s its nickname, however, not with the same context.

Wait, there’s more.

Between 1958 and 1973, more than 52,500-individual lots were created.  There are at least over 40 Puna subdivisions. Geographically, these subdivisions are sometimes as big as cities.

For example, Hawaiian Paradise Park has over 8,800 building lots and is reportedly the second largest private subdivision in the United States.  It is over 4-miles long and nearly 3½-miles wide.

Back then, they plotted out the subdivisions in cookie-cutter residential/agricultural lots across a grid, with very little space for other uses (such as parks, open space, government services, regional roads … the list goes on and on.)

To add insult to injury, most subdivision lots are accessed by private, unpaved roads. The streets generally lack sidewalks and lighting, and do not meet current County standards in terms of pavement width, vertical geometrics, drainage and other design parameters.

There are only two main roads to move the people in the district in and out – one (Route 130 – Keaau-Pahoa Road) goes into Pahoa to Kalapana; the other (Route 11 – Volcano Highway) serves the lots up in the Volcano area.

Most lots rely on individual catchment systems (captured off the roof and rainfall stored in water tanks) supplemented with private delivery trucks for drinking water.  None of the subdivisions have central sewer systems. Large sections of some subdivisions are off the power grid.

Oh, and one more thing, about 6,400 subdivision lots lie in the highest lava hazard zone and over 500 of these are exposed to additional risks from subsidence, tsunami and earthquakes.

That’s not just hazards noted on a map; thousands of these lots have been covered by lava flows or have been rendered unbuildable by shoreline subsidence over the years.

While most of these subdivisions are on agricultural-zoned lands, the actual use of developed lots is predominantly residential.

At the time these subdivisions were approved, the Puna district was sparsely populated and, with the exception of a sugar plantation and a small-scale visitor attraction at the volcano, which had not yet been developed as a national park, there was little economic activity in the area.

Shortly after the approval of the first of these subdivisions, Hawai‘i was admitted as the 50th state. That event, coinciding with jet travel, spurred increased investment in the Islands.

To prevent the excesses of land speculation, Hawai‘i adopted the first State Land Use Law in the nation in 1961.

Most of the Puna district was placed in either the Conservation District or the Agriculture District when formal boundaries were established in 1964, and this somewhat served to abate the number of subdivision applications.

However, it wasn’t until the County adopted a subdivision ordinance in 1973, setting more rigorous lot size and infrastructure standards, that large subdivisions with minimal services were effectively discouraged.

In the first decade or so following the creation of the non-conforming subdivisions, lot sales were fairly brisk, but there was little lot development.

In the 1970 Census, the recorded population of the Puna District was only 5,154-residents, most of whom lived in the older settlements of Kea‘au, Pāhoa and Volcano.

That was then, over the years the population exploded, doubling to 11,751 in 1980, then up another 10,000 by 1990 (to 20,781,) and another 11,000 by 2000 (to 31,335,) and another 14,000 by 2010 (to 45,326) to the 2020 population of about 46,800.

Population growth has worn on the minimal infrastructure, as well as people’s patience.

Today, folks in Puna are living with the lack of planning and regulatory control over the subdivision bonanza days.  But, they do benefit from lower sales prices (associated with the general lack of facilities and the huge availability.)  Some say you are getting what you pay for.

This region is finally undergoing some short and long-range planning.  And, there are attentive council members seeking to have Puna get its fair share.

Depending on your perspective, addressing the issues in this region today is either a planner’s nightmare or a planner’s dream.  This is an area where I would love to get involved – for me, challenges create opportunities.

The image notes the individual parcels within the Puna district (overlaying the Google Earth image.)  At this scale, many of the lots are not discernible – the fully gray areas indicate smaller lot residential uses, with no (or very limited) park space – where you can just see between the lines, these are 1-5 acre parcels.

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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.)

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