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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.)

© 2022 Hoʻokuleana LLC

Filed Under: Place Names, General Tagged With: Kilauea, Hawaii, Volcano, Warm Springs, Waiwelawela, Puna, Kapoho, Cape Kumukahi, Pahoa, Kilauea Iki

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)

© 2022 Hoʻokuleana LLC

Filed Under: General, Place Names, Economy Tagged With: Hawaii, Hawaii Island, Puna, Pahoa, Sugar, Coffee, Macadamia Nuts

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People, places, and events in Hawaiʻi’s past come alive through text and media in “Images of Old Hawaiʻi.” These posts are informal historic summaries presented for personal, non-commercial, and educational purposes.

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