Puna | Images of Old Hawaiʻi

July 18, 2024 by Peter T Young Leave a Comment

Waiwelawela

Paʻu o keahi o Waiwelawela o ka lua e
Aloha na poʻe la o

The pit of Waiwelawela is encircled by fire
Greetings to the people of the upland pit

(From the chant “A popoʻi haki kaikoʻo” – it describes how Pele got established in Puna; it compares the movement of the lava to the movement of water.)

There are indications that the ancient Hawaiians made use of natural hot springs for recreation and therapy. Oral history relates that the ancient chieftain, Kumukahi, frequented hot springs in Puna to relieve his aches and pains. (Woodruff/Takahashi)

“The fame of the waters of the warm springs of the Puna districts has been great during many years. In fact, it is a legend … that when the ailments of the body overcame the aliʻi of old they betook themselves to the spring known as Waiwelawela … and there they were healed of rheumatic affections through bathing, and their systemic ills cured by drinking of the waters.”

“This legend has come down to the Hawaiians of today and even now there is a fame attached to the waters of the springs, which draws to the side of the stream scores of the native residents of nearby districts.” (Pacific Commercial Advertiser, January 28, 1902)

Waiwelawela “is a warm spring, crescent shaped, and of a vivid ultramarine in color …. The spring, named the Blue Lake, is 90-deg in temperature and 900-feet above the level of the sea. The water is wonderfully clear and, strange to relate, at this elevation, it has a regular rise and fall which is said to correspond to the tide of the ocean.” (Daily Bulletin, August 28, 1882)

The Kapoho Warm Springs was formed when the downthrown block of the Kapoho fault slipped below the water table and exposed the warm waters, probably heated by a magmatic body intruded in 1840. (USGS)

“At present no practical use is made of them, but were there a proper access a small hotel would be built and many invalids would be able to make use of these springs.” (Hawaiian Gazette, September 17, 1889)

“The famous warm spring is to be found near the residence of Mr RA Lyman (Kapoho’s largest landowner) and is one of the finest bathing places on the islands. Natives formerly flocked to the place from all over the islands believing that it was possessed of great healing powers.”

“The water is a pleasant temperature for bathing and is clear as crystal, small objects can be readily distinguished twenty feet below the surface. There is a mineral taste to the water.” (Pacific Commercial Advertiser, March 22, 1892)

“The railway now goes so close to them that it is believed if a few cottages were built, and attendance provided, many afflicted people would be glad to go there and be healed. Even those who need no physician would find at these springs a place for rest and contemplation, far from the maddening crowd.” (Pacific Commercial Advertiser, October 12, 1908)

“It is the most marvelously beautiful place in all these beautiful islands. There is not a doubt of it. The pool, at the base of a small peak that is like what Diamond Head would be if that had sugar cane growing to its very summit, lies shaded by a dense growth of ʻōhiʻa and koa and lehua trees and guava bushes, the sun glistening upon it through the leaves of these.”

“The waters, not steaming, but of perceptibly higher temperature than the air, by some strange law of refraction are shot through with dazzling gleams of a blue that is like the blue depths of the sky. Yet the rocks in the pool are not blue. They are of rather reddish cast.” (Mid-Pacific Magazine, 1912)

“The exposed basin where the spring comes to the surface is something like five by six yards, and the water rises from no one knows where and departs no one sees how. The water is warm and is very full of mineral salts.” (Pacific Commercial Advertiser, January 28, 1902)

“This spot is unquestionably one of the loveliest in all Hawaiʻi, and its charm is typical of Hawaiʻi. It is close against the face of a volcanic cliff. Here there is a shady grotto, and in this grotto a pool almost as it hewed out of the rocks for the bathing place of some giant of the forest.”

“The water is in spots 20-feet deep, but so translucent that it seems much less than 10. It holds many lights and shadows, many hues and colors, varying from the deep indigo blue to a transparent jade-green and in spots a golden brown. There are seats here and the shade is grateful.” (Honolulu Star-bulletin, September 6, 1916)

At Warm Springs, where portions of ‘Bird of Paradise’ (1951) and other motion pictures had been filmed, stone steps led to a spring-fed, naturally heated pool fringed by ferns, cattleya orchids and lau hala trees.

The grounds and a half-mile drive were landscaped with plumeria, thousands of ti plants, crotons and ginger. Picnic tables and barbecue pits dotted a smooth lawn shaded by mango trees. Slim Holt, who leased the property from Lyman, had labored for years to create this beauty, assisted by interested individuals and organizations. (Flanders)

Then, “Something was amiss.” An eruption at Kilauea had ended on December 21, 1959.

“(B)ut the shallow reservoir beneath the summit of Kilauea volcano was gorged with magma, far more than before the eruption started. Rather than removing pressure, the eruption had, for all intents and purposes, created more.”

“The uncertainty ended at 1935 January 13, (1960,) when red glow in the night sky above Kapoho announced the 1960 eruption.” (USGS)

Bulldozers erected a quarter-mile line of dikes designed to prevent the lava from reaching Warm Springs. Despite this effort, toward midnight the flow surmounted the embankments.

Barbecue pits exploded; trees, shrubbery, tables and benches burst into flame. Lava poured down stone steps in a cherry-red stream. Still water, reflecting the infernal scene, disappeared under the flow. The new cinder cone was dubbed Puʻu Laimanu. … Today, buried beneath this primeval landscape, under 50-feet of lava, lays Warm Springs. (Flanders)

“Estimates of damage from the six-day eruption of Kilauea volcano rose into the millions today. State Senator Richard F Lyman estimated damage to his land, blanketed by the lava as $2,000,000.”

“He owns 80-acres of sugar land and the Warm Springs resort area, now buried by the flow on Hawaiʻi Island. Other landowners reported 3,500-acres of farmland destroyed.” (The Spokesman, January 20, 1960)

“Waiwelawela (meaning ‘warm water’) was a warm spring pool near Kapoho which was covered in the 1960 eruption. … It is said by people of the area that Pele covered the springs because people were charging others, namely Hawaiians, for use of the warm springs. In former days these warm springs were available to everyone.” (Pukui; DOE)

January 21, 2023 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.

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 20, 2022 by Peter T Young Leave a Comment

Pāhoa

Early settlement patterns in the Islands put people on the windward sides of the islands, typically along the shoreline. However, in Puna on the Island of Hawaiʻi, much of the district’s coastal areas have thin soils and there are no good deep water harbors. The ocean along the Puna coast is often rough and windblown.

As a result, settlement patterns in Puna tend to be dispersed and without major population centers. Villages in Puna tended to be spread out over larger areas and often are inland, and away from the coast, where the soil is better for agriculture. (Escott)

This was confirmed on William Ellis’ travel around the island in the early 1800s, “Hitherto we had travelled close to the sea-shore, in order to visit the most populous villages in the districts through which we had passed. But here receiving information that we should find more inhabitants a few miles inland, than nearer the sea, we thought it best to direct our course towards the mountains.” (Ellis, 1823)

An historic trail once ran from the modern day Lili‘uokalani Gardens area in Hilo to Hāʻena along the Puna coast. The trail is often referred to as the old Puna Trail and/or Puna Road. There is an historic trail/cart road that is also called the Puna Trail (Ala Hele Puna) and/or the Old Government Road.

This path was essentially the main thoroughfare through the Puna district before the late-1800s. Pāhoa was oʻioʻina (a resting place) on the trail. (Papakilo) Then it grew to become the principal town of lower Puna.

The evolving trail (first by foot, then by horse, cart and buggy, and finally by automobile) likely incorporated segments of the traditional Hawaiian trail system often referred to as the ala loa or ala hele. (Rechtman)

The full length of the Puna Trail, or Old Government Road, might have been constructed or improved just before 1840. The alignment was mapped by the Wilkes Expedition of 1804-41. (Escott)

People who traditionally had lived along the Puna coast were moving toward Hilo and into the more fertile upland areas of Puna in order to find paid work and to produce cash crops for local markets and for export.

The focus began to shift to the center of the Puna District and the developing sugar and related industries near ʻŌlaʻa, Hilo and the volcano region.

Before the turn of the century, railroad operations began – with lines running into Hilo. A main railroad line and several feeder lines were constructed in the early-1900s from Keaʻau to locations in lower Puna District.

The major line ran from Hilo through Keaʻau to the Kapoho area. A branch line ran from the ʻŌlaʻa Sugar Mill up past present day Glenwood. A second branch line ran to Pāhoa town.

Some suggest this is how Pāhoa received its name. “Then the train was put in from Hilo to Puna. One spur went up into Pāhoa; it was like a dagger into the forest. I‘m told this is how Pāhoa got its name. (Pāhoa means dagger.)” (Edwards; Cultural Surveys)

People began to work in the inland areas to grow sugarcane. The new road, the Pāhoa branch of the railroad, sugarcane agriculture and a logging venture all combined to create Pāhoa as a population center in the region. (Rechtman)

Macadamia nuts and papaya were introduced in 1881 and 1919; at the turn of the century, large-scale coffee cultivation was attempted. Over 6,000-acres of coffee trees were owned by approximately 200-independent coffee planters.

This fledgling industry couldn‘t compete with more successful ventures located in other districts, and after a few decades the coffee industry in Puna was abandoned. (Cultural Surveys, Rechtman)

By 1901, sugar dominated the island’s industry and landscape, and Hilo was the epicenter of production and export. Railroads connected sugar mills and sugar plantations in Hilo, the Hāmākua and Puna. The railroad also connected the mills to the wharves at Hilo Bay.

Early on, one of the major export items transported by the railroad was timber. Starting in 1907, the Hawaiian Mahogany Company began cutting trees to clear land for sugarcane. The logs were brought to Pāhoa Town to be milled, then sent to Hilo Harbor and eventually shipped to the US Mainland as railroad ties for the Santa Fe Railroad.

The lumber mill facilities and the railroad line that served them were located near the center of town where the Akebono Theater is located.

In 1909, the company was renamed Pāhoa Lumber Company. In 1913, the main mill facilities were lost in a fire; it was rebuilt that year the company was renamed the Hawaiian Hardwood Company.

The company closed down in 1916 when the Santa Fe Railroad ended its contract to buy lumber. The defunct company then leased its mill facilities, buildings and railroad tracks to the expanding ʻŌlaʻa Sugar Company. (Rechtman)

Today, Pāhoa Town has a main street – the former highway route before the construction of the by-pass road – that still retains much of the original street-wall of plantation-era structures, as well as some significant stand-alone buildings.

Most of the uses are commercial or civic. The County has acquired a large tract of land within Pāhoa Town, which presents a significant opportunity for community revitalization and a possible catalyst for economic activity. (Puna CDP)

November 3, 2018 by Peter T Young 1 Comment

Kaimū

The name literally means ‘gathering [at the] sea [to watch surfing].’ This land section and village, at Kalapana, Hawaiʻi, was noted for its surf and its black sand beach. The black sand was formed by steam explosions that occurred when a lava flow entered the ocean in about 1750. (Pukui)

“Kaimu is pleasantly situated near the sea shore, on the SE side of the island, standing on a bed of lava considerably decomposed, and covered over with a light and fertile soil. It is adorned with plantations, groves of cocoa-nuts and clumps of kou trees.”

“It has a sandy beach, where canoes may land with safety; and according to the houses numbered to-day contains 725 inhabitants. Including the villages in the immediate vicinity, along the coast, the populations would probably amount to 2,000; and, if water could be procured near at hand, it would form an eligible missionary station.”

“There are several wells in the village, containing brackish water, which has passed from the sea, through the cells of the lava, undergoing a kind of filtration, and it is collected in hollows scooped out to receive it. The natives told us, that, at the distance of about a mile, there is plenty of fresh water.” (Ellis from 1823)

“The most important reason that settlement in the Kalapana area was on the coast was the availability of fresh food from the sea. Fishing was on the shore, which also hosted gathering of shellfish, crabs and limu, and from canoes.”

“Taro and breadfruit were major crops of the better watered coastal areas in the east but especially in the forested uplands. Bananas, sugar cane, and ‘awa were also grown in the uplands.” (Hawai‘i County)

“We passed a potato patch in the broken lava which exceeded anything I had seen. Not a particle of soil was anywhere to be seen, and the holes dug among the stones to receive the potatoes were some of them six feet in depth-thus securing a degree of moisture and shelter from the sun-though no more soil than at the surface.”

“There are but few people in this region. They are miserably poor, & for some time past have been almost in a state of famine. They get their living by fishing, making salt, & getting fern roots & a few potatoes in the mountains.”

“Their salt works are on the naked lava near the sea, the water of which is evaporated in little cups or vessels made of the Ki leaf & holding of course but a minute quantity of water.”

“These are laid in parallel rows over several acres, & the water poured into them a little at a time from Calabashes. The process is an extremely slow one, tho’ the salt is s[aid] to be excellent for the table. It is sold at the exceedingly low prices of 25 cts a bag, which will contain I sh’d judge ½ a bushel or more” (Chester Lyman, 1846)

“At the beach the road enters first the village of Kaimu, exclusively Hawaiian, with a large grove of cocoanut trees surrounding a fine semi-circular sand beach. Care should be exercised in bathing on account of the under tow.”

“Less than a mile further on, westwards, lies the village of Kalapana, one of the largest Hawaiian villages in the Islands. There are no white inhabitants, and only a couple of Chinese stores. Here is the headquarters for a couple of stages, which make irregular trips to Pahoa (Rate: 75 cents a passenger one way.)” (Kinney, 1913)

The district of Puna is distinguished as one of the least awarded private lands from the 1848 Māhele and Kuleana Act. Only 19 awards of private land were made in the entire district.

Of these, 16 awards were made in large tracts to 10 chiefs who lived outside of Puna, and three small parcels were granted, to commoners Baranaba, Hewahewa and Haka (Territory of Hawai`i 1929.)

The small number of land awards was not because Puna had a small population. In 1854, four years after the Kuleana awards were granted, the estimated population for Puna was 2,702 (Hawaii Mission Children’s Library 1854.)

Moreover, the 1858 tax records for Puna shows that 894 males over the age of 20 paid poll taxes in Puna ten years after the deadline for filing for land awards (Hawai‘i State Archives 1858.)

An examination of the possible reasons why almost the entire population of Puna did not enjoy the benefits of the Māhele and Kuleana Act lends an understanding of why Hawaiians living in the district remained outside of the mainstream of Hawai`i’s economic and social development.

First, Puna was isolated from the mainstream of economic, social and political developments. It is possible that the Hawaiians in Puna were not aware of the process or did not realize the significance of the new law.

Second, it is possible that the Puna Hawaiians did not have a way to raise the cash needed for the land surveys, which cost between $6 to $12. Wages at the time were normally between 12 1/2 cents and 33 cents a day.

However, there were few wage-earning jobs in Puna. Cash would have to be raised from selling extra fish or other products, which was difficult given the subsistence living of many Hawaiians.

Third, at least some Puna Hawaiians filed their land claims after the deadline. In an 1851 petition to the legislature, several Puna residents asked to be issued land grants without penalty, as they had filed their claims after February 14, 1848 (Allen 1979).

Under the Māhele, the bulk of Puna lands were designated as public lands either to the monarchy, as “Crown” lands or to the government of the Hawaiian Kingdom. (McGregor)

In March 1990, Kīlauea’s ongoing Puʻu ʻŌʻō-Kupaianaha eruption (that began on January 3, 1983) entered its most destructive period of the 20th century when lava flows turned toward Kalapana, an area cherished for its historic sites and black sand beaches.

By the end of the summer, the entire community, including a church, store, and 100 homes, were buried beneath 50-80 feet of lava.

As the lava flows advanced eastward, they took to the sea, replacing the palm-lined Kaimū Bay with a plain of lava that now extends nearly 1,000-feet beyond the original shoreline.

In late 1990, a new lava tube finally diverted lava away from Kalapana and back into the National Park. (USGS)

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