Volcano | Page 6 | Images of Old Hawaiʻi

October 22, 2021 by Peter T Young Leave a Comment

Bombing the River of Fire

Like most Hawaiian eruptions, the eruptive activity was immediately preceded by a swarm of earthquakes, followed by tremor. Mauna Loa (“Long Mountain”) began erupting at 6:20 pm on November 21, 1935.

The eruption started with a curtain of fountains near North Pit within the summit caldera, Mokuʻāweoweo. The vents migrated 2-miles down the northeast rift zone.

During the six days of the main event, fissures opened up along the northeast rift zone of the mountain, fountaining lava 200- to 300-feet into the air.

On November 26, the summit eruption died and the northeast rift activity was reduced to a single vent at the 11,400-foot elevation. A small vent also opened up further below on the north flank of the mountain at the 8,600-foot elevation. (USGS)

Lava flows from Mauna Loa were generally fast-moving and voluminous. Lava moved relentlessly at a rate of five-miles each day; it pooled up between Mauna Kea and Mauna Loa at about where the Saddle Road is situated.

The ponded lava eventually began to follow the lay of the land, a natural drainage … Then, things “got interesting.” Lava was heading directly toward Hilo. (USGS)

Dr. Thomas A Jaggar Jr, the government volcanologist, estimated that the flow would reach Hilo by January 9, 1936. He suggested using dynamite to collapse lava tubes near the source of the flow in order to stop or divert it.

Explosives were first suggested as a means to divert lava flows threatening Hilo during the eruption of 1881. However, Jaggar’s plan of mule teams hiking the explosives up the mountain would take far too long – the lava flows were moving a mile a day.

Guido Giacometti, a friend of Jaggar, had suggested using US Army Air Corps bombers to precisely deliver explosives. Jaggar agreed, and the call was made.

The US Army Air Corps approved, and the mission and plans to strategically bomb Mauna Loa were set into motion. Lieutenant Colonel George Smith Patton was called on to oversee the Army operation. (He’s the same Patton who would go on to WWII fame.)

Lava tubes are cooled and hardened outer crusts of lava which provide insulation for the faster-flowing, molten rock inside. Such a conduit enables lava to move faster and farther.

The theory was bombs would destroy the lava tubes, robbing lava of an easy transport channel and exposing more of the lava to the air, slowing and cooling it further. (BBC)

On December 26, 1935, six Keystone B-3A bombers of the 23d Bomb Squadron and four Keystone LB-6A light bombers from the 72d Bomb Squadron joined the rendezvous circle in the predawn darkness off Diamond Head, and then headed to Hilo.

Jaggar briefed the crews on the methods he had in mind to divert the lava flow. He then flew over the volcano to assess the flows and select the right points for bombing.

8:30 am, December 27, 1935, the first five bombers departed on the bombing mission. (A second flight of five aircraft was planned for the afternoon.) Each plane carried two 300-pound practice bombs (for practice and sighting,) as well as two 600-pound Mk I demolition bombs (355 pounds of TNT each.)

The bombers opened formation and fell into a huge circle for a follow-the-leader dummy run over the target area. They were flying at about 12,500-feet, not far above the 8,600-foot altitude of the volcano’s flows.

As the lead pilot tipped the control column forward for his run he lowered the wheels, so that by the time he neared the clump of koa trees which served as reference point his plane would be moving only a little faster than the 65-mph landing speed.

‘OK?’ he called to his bombardier as they began their climb after passing over the flow. Standard radio-voice procedure was unneeded. … ‘OK,’ the bombardier grunted. (Johnson)

Five of the twenty bombs struck molten lava directly, most of the others impacted solidified lava along the flow channel margins; one of them turned out a dud.

“Colonel William C Capp, a pilot who bombed the lower target, reported direct hits on the channel, observing a sheet of red, molten rock that was thrown up to about 200′ elevation and that flying debris made small holes in his lower wing.”

“Bombs that impacted on solidified, vesicular pāhoehoe along the flow margin produced craters averaging 6.7-m diameters and 2.0-m depth….” (Swopes)

“Pilots observed that several bombs collapsed thin lava tube roofs, although in no case was sufficient roof material imploded into the tube to cause blockage.”

Jagger wrote that “the violent release of lava, of gas and of hydrostatic pressures at the source robbed the lower flow of its substance, and of its heat.”

The lava stopped flowing on January 2, 1936. The effectiveness of the lava bombing is disputed by some volcanologist. (USGS)

Here’s a link to a video of the Army bombing runs in 1935. (Lots of information here from Army, USGS, hawaii-gov, 4GFC, Johnson, Lockwood & Torgerson, Swopes and This Day in Aviation History.)

http://www.criticalpast.com/video/65675069574_bomb-Mauna-Loa_divert-lava_Keystone-B-3A_Keystone-LB-6A_United-States-fliers

Three Keystone B6As of 20th Bombardment Squadron, 2d Bomb Group, release their bombs on a practice mission

Plume from a test bombing of an old lava flow on Mauna Loa, performed in 1975

Lieutenant General Patton in 1935, prior to World War II

Keystone B-3A Bomber of the type used in the bombing of the volcano above Hilo in 1935

Dr. Thomas Jaggar and wife, Isabel Maydwell – 1917

Advancing lava flow, December 1935. (USGS)

May 26, 2019 by Peter T Young 3 Comments

Uncle George

George Lycurgus (1858–1960) was a Greek American businessman who played an influential role in the early visitor industry of Hawaiʻi.

He was instrumental in the development of the Hawaiian Volcano Observatory and Hawaiʻi Volcanoes National Park.

In 1893, Lycurgus leased a small guest house on Waikīkī Beach. He expanded it and renamed it the “Sans Souci” (French for “without care” and named after the palace of Frederick the Great in Germany.)

It became one of the first Waikīkī beach resorts (that end of Waikīkī is still called “Sans-Souci Beach.”) Among its guests was Robert Louis Stevenson.

Stevenson wrote in the guest book: “If anyone desires such old-fashioned things as lovely scenery, quiet, pure air, clean sea water, good food, and heavenly sunsets hung out before their eyes over the Pacific and the distant hills of Waianae, I recommend him cordially to the Sans Souci.”

“In 1893 Sans Souci was a rambling hostelry, nestled among the coconut and palm trees of Waikiki Beach. The guests occupied small bungalows, thatched-roof affairs about ten by twelve, the bed being the principal article of furniture.”

“It was in one of these bungalows that Stevenson had established himself, propped up with pillows on the bed in his shirt-sleeves.” Scribner’s Magazine, August, 1926.

By 1898, the Spanish American War had increased American interest in the Pacific. Hawaiʻi was annexed as a territory of the United States and Lycurgus applied for American citizenship.

He opened a restaurant called the Union Grill in Honolulu in 1901. He later invested in a logging venture in 1907 and also bought the Hilo Hotel in 1908.

In 1903, when he returned to Greece to visit his mother, he met and married Athena Geracimos from Sparta. She was probably the first Greek woman in Hawaiʻi.

In December 1904, George and his nephew (Demosthenes Lycurgus) became principal stockholders of the Volcano House Company and took over the management of the Volcano House hotel on the Big Island of Hawaiʻi.

His nephew always introduced him as “Uncle George” to the guests, which earned him his new nickname.

He worked with Lorrin Thurston and others for ten years, starting in 1906, to have the volcano area made into Hawaiʻi Volcanoes National Park.

In January 1912, geologist Thomas Jaggar arrived to investigate the volcano. A building for scientific instruments was built in a small building next to the hotel. Jaggar stayed in Volcano for the next 28 years.

In 1921, George Lycurgus sold the Volcano House to the Inter-Island Steam Navigation Company and moved to Hilo. During the Great Depression the company was going bankrupt and Lycurgus bought it back.

A fire destroyed the hotel in 1940, ironically from a kitchen oil burner, not volcanic activity. Only a few artifacts, such as a koa wood piano, were saved.

At the age of 81, he traveled to Washington, DC to have the construction of the new park headquarters building farther back from the lip of the crater.

That allowed him, in 1941, to build a more modern hotel at the former Hawaiian Volcano Observatory site. He reopened the new Volcano House (designed by notable architect Charles William Dickey.)

After another eruption in 1952, at the age of 93, he arranged a publicity stunt involving riding a horse to the rim of the erupting vent and tossing in his ceremonial bottle of gin. (The offering of gin became a regular at Volcano after that.)

Uncle George died in 1960 at the age of 101.

The National Park recently announced that Hawaiʻi Volcanoes Lodge Company has been selected to operate the Volcano House Hotel, Nāmakanipaio cabins and campground and other commercial services within Hawaiʻi Volcanoes National Park. The facility is scheduled to reopen in late-2012.

Volcano has been a special place for me.

As a kid, our family often visited Volcano and regularly stayed at the Volcano House. I remember seeing and meeting Uncle George while he was sitting before the continuously-burning fireplace at the Volcano House.

Decades later, I purposefully went to Volcano to plan the formation of my first business; the initial planning was on cocktail napkins at the Volcano House bar (the business succeeded.)

Today, the Young siblings own a house at Volcano our mother built; I used to visit there once a month, but now get back to it less frequently.

The Volcano Art Center Gallery is located in the 1877 Volcano House Hotel (now adjacent to the Volcano Visitor Center) under a cooperative agreement with the National Park Service.

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Uncle George Lycurgus

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Uncle_George_Lycurgus-1958

Sans_Souci_Hotel_Ad-1893

San Souci Beach Area – large house (Mitchell) is where Natatorium is now located-1886

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December 10, 2018 by Peter T Young Leave a Comment

Punalu‘u Hotel

The railroad from Punaluʻu to the village of Keaiwa (where the Pāhala Sugar Mill was located) was reported in June 1878 to be “the first railroad in these islands”. Railroads continued to operate in Kaʻū until the 1940s but the Pāhala – Punaluʻu railroad was discontinued in 1929. (Cultural Surveys)

Starting in the late-1800s, to get people and goods around the Islands, folks would catch steamer ships; competitors Wilder Steamship Co (1872) and Inter-Island Steam Navigation Co (1883) ran different routes, rather than engage in head to head competition.

For Inter-Island’s routes, vessels left Honolulu stopping at Lāhainā and Māʻalaea Bay on Maui and then proceeding directly to Kailua-Kona.

From Kailua, the steamer went south stopping at the Kona ports of Nāpoʻopoʻo on Kealakekua Bay, Hoʻokena, Hoʻopuloa, rounding South Point, touching at the Kaʻū port of Honuʻapo and finally arriving at Punaluʻu, Kaʻū, the terminus of the route. (From Punaluʻu, five mile railroad took passengers to Pāhala and then coaches hauled the visitors to the volcano from the Kaʻū side.)

The Punaluʻu Harbor and Landing served the communities of Punaluʻu and Nīnole and the sugar plantation at Pāhala and was considered the “port town for the district in 1880.” (Orr) By the mid-1880s Punaluʻu had storehouses, a restaurant, a store, and numerous homes constructed of lumber. (Cultural Surveys)

“The Interisland steamer W G Hall, 380 tons burthen, leaves Honolulu alternate Tuesdays and Fridays, at 10 A. M. She is one of the best sea boats plying in our waters, and tourists will find her accomodations and table equal to any, while her officers and stewards are ever on the alert to supply all their wants.”

“(T)he steamer at once proceeds to Punalu‘u, the terminus of the sea route. This is usually reached about 6 P. M. The passengers are landed in boats and will proceed to the Punalu‘u hotel, where they will find themselves comfortably taken care of.” (Whitney)

Peter Lee owned and operated the Punalu‘u hotel. He popularized the Punalu‘u-Pahala route to Kilauea. He built a 24-mile wagon road from Pahala to Kilauea, following by seven years the construction of a hotel at Punalu‘u, which then became a third takeoff point. (NPS)

“The hotel is clean, the table good, and the proprietor will be found very obliging and ready to afford any information required.” (Whitney)

Later, Lorrin Thurston became more interested in the Volcano … and the Volcano House and the Punalu‘u hotel, “In June 1890, I again visited Kilauea, and became so interested in it that I applied to Samuel G. Wilder, then head of Wilderʼs Steamship Co., who held leases of the Volcano House and site; I purchased some leases of him, and secured a new lease from the owner, the present Bishop Estate.”

“I also purchased a hotel at Punalu‘u from Peter Lee, and made him the manager of both hotels. A new company was formed; I got enough capital to remodel the Volcano House and to make additions so that it was much more commodious and attractive.”

“Formerly it had had only six bedrooms for visitors, a living room, a small dining room, a kitchen, and a room for the manager. The lumber and other materials for construction and repairs were shipped from Honolulu to Punalu‘u, whence they were hauled to Pahala by the plantation railroad, and thence to the volcano by the Hustace draying concern of Honolulu.”

The Paradise of the Pacific, noted, “Arrangements have been completed with the Wilderʼs Steamship Co. and the Inter-Island Com., so that a single round trip ticket can be obtained at the office of either Steamship Company for fifty dollars ($50) …”

“… which covers all room, meals, board and lodging at Hilo or Kau, transportation to and from the Volcano by either carriage or horse back, and board, lodging, steam sulphur baths and guide into the crater, at the Volcano.” (Maly)

“This ticket includes an absence from Honolulu, of eight days and gives five days on shore, which can be spent at any point the ticket-holder chooses, either at the Volcano, Hilo or Punalu‘u.”

“If the trip up to the volcano is made the day the steamer arrives, and return on the day she leaves, it allows four nights and three days at the volcano, or two days and two nights longer than heretofore allowed on this ticket.”

“Double route round trip tickets may also be obtained for seventy dollars ($70). This ticket includes all expenses covered by the other ticket and the holder may go by either the Hilo or Kau route and return by the other.”

“By taking this ticket an entire week may be spent at the Volcano, in a cool bracing climate, with invigorating sulphur baths at hand, and the Greatest Volcano on Earth in constant action in the front yard of the Hotel.” (Hawaiian Gazette, June 2, 1891)

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Punaluu village, Hawaii-S00084-1880

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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Kaimu-Beach-lava entering

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Young woman at Kaimu Black Sand beach, Kalapana-PP-29-10-017-1935

Two young women on Kaimu Black Sand beach, Kalapana-HAL_Promotion-PP-29-10-019

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Sunrise at Kaimu Black Sand beach, Kalapana-PP-29-10-002

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Pauline Wessel on Kaimu Black Sand beach, Kalapana-PP-29-10-023-1935

Kalapana Store-pre-lava flow

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Kalapana Store-post-lava flow

Kaimu Black Sand Beach, Kalapana

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April 24, 2018 by Peter T Young 1 Comment

Keakealani School

Peter Lee, an enterprising pioneer with an eye to the future, tried to popularize the Punalu‘u-Pahala route to Kilauea Volcano, a noted attraction, then and now.

“The wonderful volcano of Kīlauea, on the island of Hawaii, is the great attractive of visitors. It is the only crater in the world that is constantly in action, and that can be safely approached at all times to the very edge of the precipice which encloses the boiling lava.”

“To reach Kīlauea necessitates a passage of thirty hours from Honolulu in a fine steamer to Hilo or Punalu‘u, then a ride of thirty
miles in coaches takes visitors to a fine hotel, which overlooks the molten lava lake. It is a sight that will repay the effort and expense incurred ten times over, and one that will never be forgotten.” (Whitney)

In 1891, Lee built a 24-mile wagon road from Pahala to Kilauea, following by seven years the construction of a hotel at Punalu‘u. (NPS) However, the construction of the Volcano Road from Hilo had also begun.

With the completion of the Hilo to Volcano Road in 1894, four-horse stagecoaches came into the picture, reducing the travel time from Hilo from two days to six and one-half hours, and Hilo became the principal departure point for Kilauea. (NPS)

Lee later sold to the new owners of the Volcano House and then managed both hotels for them. Lee would remain as manager of the Volcano House until 1898.

Lee established a home on land near the center of the ʻŌlaʻa Summer Lots 29-Mile subdivision, which later become Volcano Village.

Noting the need for a school there, in 1914, Peter Lee donated a one-acre site on Haunani Road (named for one of his daughters) to the Territory of Hawai‘i for a “school to teach the children of the region”.

In 1915 the first school building was constructed – a classic one-room structure, along with a teacher’s cottage, small garage, and water tank. The school was named “Keakealani School” in honor of another of Lee’s daughters. (VSAC DEA)

In 1934 the growing student population called for larger facilities and the present two-room building was constructed and the teachers’ cottage and garage demolished, which left the layout we see there today.

In the late 1930s the Kennedy Family, who owned the property abutting the school site to the Hilo side, donated 2.25 acres to the Territory to increase the site to its current 3.25 acres.

In addition to the two-room building, the property consists of a grassy field with a few open-sided, temporary shelters. (VSAC DEA)

By Executive Order No. 1040 dated November 27, 1943, control of the subject property was placed in the Territorial Department of Public Instruction, now the Department of Education (DOE).

“The Hawaii Visitors Bureau won’t admit it. Mainland tourists basking in the sun at Waikiki beach won’t believe it. But kerosene and electric heaters are used to warm the tootsies of some 100 youngsters who attend classes in several public schools here in this island paradise when the mercury takes a nose dive.”

“Mrs Antonio Short, principal of KeaKealani school in the volcano area on the island of Hawaii, explained that ‘some days during the winter we keep our heaters burning all day and have frosty windows, like real Christmas weather.’”

“‘Frost ‘fell’ on our school yard twice in five years, and the temperature sometimes gets as low as 32 degrees,’ Mrs Short said. ‘Most of the youngsters even have to wear sweaters and coats until 10 am on cold days. And if it gets much worse, the youngsters will have to wear shoes all the time.’” (The Times, Shreveport, December 16, 1956)

DOE operated a public school on the site until 1973, when the students were transferred to Mountain View Elementary School. Until 2010, DOE used the facility as an outdoor education center for elementary students on the island of Hawaii.

Budgetary constraints caused DOE to terminate this program, and the facility was subsequently licensed on a year-to-year basis to Volcano School of Arts and Sciences (Volcano School), a public charter school, commencing on July 1, 2010. (DLNR)

Volcano School used the facility as its middle school campus, and received a $618,000 grant-in-aid from the 2011 Legislature to expand the facility to better accommodate its middle school program.

DOE and Volcano School subsequently executed a Lease Agreement effective as of August 1, 2012 that specifies that the premises shall be used for a charter school (consistent with the purpose of the executive order). (DLNR)

This allows the school to consolidate its grades K-4 classes, which are currently located on Old Volcano Rd., with its grades 5-8 classes so the school’s students will be together on one campus. (KHON2)

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