Images of Old Hawaiʻi

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‘We stopped, and trembled’

“Messrs (William) Ellis, (Asa) Thurston, (Artemas) Bishop and (Joseph) Goodrich made a tour round the island of Hawai‘i, examining its various districts, conversing with the natives, and preaching the gospel 130 different times.”  (History of ABCFM)

“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.”

Makoa, their guide, “objected strongly to our going thither, as we should most likely be mischievous, and offend Pele or Nahoaarii, gods of the volcano, by plucking the ohelo, (sacred berries,) digging up the sand, or throwing stones into the crater, …”

“… and then they would either rise out of the crater in volumes of smoke, send up large stones to fall upon us and kill us, or cause darkness and rain to overtake us, so that we should never find our way back.”

“We told him we did not apprehend any danger from the gods … If we were determined on going, he said, we must go by ourselves, he would go with us as far Kapapala, the last village at which we should stop, and about twenty miles on this side of it …”

“… from thence he would descend to the sea-shore, and wait till we overtook him. The governor, he said, had told him not to go there, and, if he had not, he should not venture near it, for it was a fearful place. … [W]e proceeded on our way, leaving Makoa to wait for them, and come after us as far as Kapapala, where we expected to spend the night.”

In 1823, they were the first Westerners to visit Kilauea volcano.  Ellis describes his first impressions, “After walking some distance over the sunken plain, which in several places sounded hollow under our feet, we at length came to edge of the great crater, where a spectacle, sublime and even appalling, presented itself before us“.

“‘We stopped, and trembled.’”

“Astonishment and awe for some moments rendered us mute, and, like statues, we stood fixed to the spot, with our eyes riveted on the abyss below.”

“Immediately before us yawned an immense gulf, in the form of a crescent, about two miles in length, from north-east to south-west, nearly a mile in width, and apparently 800 feet deep.”

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

“Fifty-one conical islands, of varied form and size, containing so many craters, rose either round the edge or from the surface of the burning lake.”

“Twenty-two constantly emitted columns of grey smoke, or pyramids of brilliant flame; and several of these at the same time vomited from their ignited mouths streams of lava, which tolled in blazing torrents down their black indented sides into the boiling mass below.”

“The existence of these conical craters led us to conclude, that the boiling caldron of lava before us did not form the focus of the volcano; that this mass of melted lava was comparatively shallow; and that the basin, in which it was contained was separated, by a stratum of solid matter, from the great volcano abyss, which constantly poured out its melted contents through these numerous craters into this upper reservoir.”

“We were further inclined to this opinion, from the vast columns of vapour continually ascending from the chasms in the vicinity of the sulphur banks and pools of water, for they must have been produced by other fire than that which caused the ebullition in the lava at the bottom of the great crater …”

“… and also by noticing a number of small craters, in vigorous action, situated high up the sides of the great gulf, and apparently quite detached from it.”

“The streams of lava which they emitted rolled down into the lake, and mingled with the melted mass there, which, though thrown up by different apertures, had perhaps been originally fused in one vast furnace.”

“The sides of the gulf before us, although composed, of different strata of ancient lava, were perpendicular for about 400 feet, and rose from a wide horizontal ledge of solid black lava of irregular breadth, but extending completely round.”

“Beneath this ledge the sides sloped gradually towards the burning lake, which, was, as nearly as we could judge, 300 or 400 feet lower. It was evident, that the large crater had been recently filled with liquid lava up to this black ledge, and had, by some subterranean canal, emptied itself into the sea, or upon the low land on the shore.”

“The grey, and in some places apparently calcined, sides of the great crater before us; the fissures which intersected the surface of the plain on which we were standing; the long banks of sulphur on the opposite side of the abyss; the vigorous action of the numerous small craters on its borders …”

“… the dense columns of vapour and smoke, that rose at the north and south end of the plain; together with the ridge of steep rocks by which it was surrounded, rising probably in some places 300 or 400 feet in perpendicular height, presented an immense volcanic panorama, the effect of which was greatly augmented by the constant roaring of the vast furnaces below.”

“After the first feelings of astonishment had subsided, we remained a considerable time contemplating a scene, which it is impossible to describe, and which filled us with wonder and admiration at the almost overwhelming manifestation it affords of the power of that dread Being who created the world, and who has declared that by fire he will one day destroy it.”

“We then walked along the west side of the crater, and in half an hour reached the north end.”  (All here is from William Ellis’ Narrative of a Tour Through Hawaii.)

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Charles Titcomb

Charles Titcomb was a practical Yankee of considerable ability (born in Boston, July 24, 1803), a watchmaker by trade, who had reached the Hawaiian Islands as a sailor on the bark Lyra that was wrecked in the ‘false passage’ (apparently around Maui) in 1830.  (Damon and PCA March 31, 1883) He lived/worked at various places on Kauai.

Koloa

He initially settled at Koloa, Kauai.  At the time, “Clusters of native dwellings are scattered on the plain, but the principal village is situated a mile from the beach, at a short distance from the missionary buildings.”

“Fields of sugar cane, taro, yams, and other vegetables, bespeak a more than usual attention to agriculture. The population of Koloa, which is about three thousand, is increasing rapidly by emigrations from other districts. But the principal attractions here are the estates of Messrs. Ladd & Co. and Messrs. Peck & Titcomb, American gentlemen.”

“From Ladd and Company Messrs. Peck and Titcomb subleased about 400 acres on which, from 1836 to 1840, they conducted careful experiments in raising cotton, coffee and silk.”

“Their mulberry trees throve so that one of the little hills on their land was soon called Mauna Kilika, or Silika, as it still is on old maps. …  Beset by one difficulty after another, such as drought, blight and failure of the silkworm eggs to hatch even when taken in bottles to the mountain tops for a lower temperature, silk culture was abandoned about 1840.”

“Mr. Titcomb then transferred his equipment across the island to Hanalei to begin similar attempts there. And sugar thus remained the one active commercial enterprise in Koloa.” (Damon)

Hanalei

“In the course of time other white settlers were attracted to the fertile and well-watered region of Hanalei and Waioli, among whom the first to undertake a business venture systematically was this same Charles Titcomb of Koloa.”

“While his interests were frankly commercial, and it was of course essential that his silk worms should be fed on Sunday, as on every other day, it is not true, as has sometimes been alleged, that the missionaries of Hanalei attempted to thwart his industrial efforts.”

“The refutation of this charge is made on the indisputable authority of Mr. G. N. Wilcox, who grew up in one of the two mission homes at Waioli and knows the history of Kauai as it is known to no other living person today.”

The missionaries at Hanalei, as at Koloa, rejoiced that Hawaiians had now some means of profitable labor by which they could free themselves from the restrictions of the konohiki, or overlord. And while the missionaries regretted that a certain amount of labor was necessary on the Sabbath, it came to be regarded as an inevitable accompaniment of economic change.”

“And when on, or even perhaps before, the blighting of his mulberry trees at Koloa, Mr. Titcomb started cuttings in the Hanalei river bottom, a prodigiously rapid growth was the result, even also as ratoons.”

“Mr. Jarves states that Mr. Titcomb had obtained his lease of Hanalei river lands from the king as early as 1838. A fairly good quality and quantity of silk was soon produced, the Hawaiian women proving skilful in the art of reeling the delicate threads from the tiny cocoons, and the first export was made in 1844, but profits were too slow to warrant the necessary outlay of capital.”

“Securing berries from the Kona fields of Messrs. Hall and Cummings, Mr. Titcomb gradually replaced his mulberry orchards with coffee plants, and thus opened direct competition with his immediate neighbors.”

“Another commercial venture, somewhat farther afield, was made by Mr. Wundenberg in company with Messrs. Titcomb and Widemann late in 1848, when the three gentlemen left their families on Kauai and proceeded to join the gold rush to California. The net result seems to have been chiefly in the realm of experience, for it was not long before all three had returned to their former agricultural pursuits. …”

“In 1853 [Robert Wyllie] bought the Crown lands at Hanalei which were leased by the Rhodes Coffee Plantation, and two years later Captain Rhodes sold out his financial interest in it to Mr. Wyllie.”

“After the visit of the royal personages at Hanalei in 1860, Mr. Titcomb’s plantation became known as Emmasville and Mr. Wyllie’s as Princeville Plantation, in honor of the event. And Princeville is the name which persists to this day as the title of the estate.”

“In 1862 the Princeville plantation, following Mr. Titcomb’s lead, was converted from coffee to sugar and the face of the river valley took on a materially different aspect. Mr. Wyllie added the two ahupuaas, land divisions, of Kalihikai and Kalihiwai, to his Princeville estate, and sent to Glasgow for his sugar mill.” (Damon)

“Foremost in enterprise, Mr. Titcomb was the prime mover in introducing the Tahitian variety of cane, which for so many years was the backbone of the industry.”

“The whaling captain entrusted with the importation of this new cane chanced to make port at Lahaina, whence the samples were distributed throughout the islands. Hence the name, Lahaina cane, for that staple variety which was in reality from Tahiti.”

“[T]he coffee plantation of Mr. Titcomb at Hanalei was reported, just before the drought, as in excellent order and always a model of good management and thrift.” (Damon)

Coffee was grown successfully at Hanalei during the 1840s and 1850s until a blight caused by aphids wiped out over 100,000 coffee trees.  (Soboleski, TGI)

“In 1852 Irish potatoes constituted the largest export from the islands to California, but two years later the Hawaiian planters ‘were eating potatoes from California of better quality and less price.’”

“By the process of the survival of the fittest, sugar was becoming Hawaii’s staple product. Yet even that finally proved unsuited to the cool, wet climate of Hanalei.”

“Mr. Titcomb, in the lead as usual, sold the Emmasville Plantation of over seven hundred acres to Mr. Wyllie in 1863 and moved to Kilauea, further to the eastward on the Kauai shore. Here he bought the Kilauea land grant from the king and established himself in cattle ranching.”  (Damon)

Kilauea

“He built himself a house, which until very recently was used as the Kilauea plantation hospital; and when Mr. Widemann came to Hanalei in 1864, Mr. Titcomb secured his herd of cattle from Grove Farm.”

“Capt. Dudoit and Mr. Titcomb of Hanalei also met with considerable success at Kilauea, but the former moved his family to Honolulu in 1862.”

“These two gentlemen had become discouraged with the struggles in sugar at Princeville and were attempting the somewhat drier climate to the eastward.”

“In 1877, when Titcomb sold his Kilauea ranch to English Capt. John Ross and Edward Adams for the purpose of growing sugar cane, Kilauea Sugar Plantation was founded, with Titcomb staying on to build the plantation’s first sugar mill.” (Damon)  Kilauea Plantation closed in 1971. (Soboleski, TGI)

“Having primitive works, his whole product was for many years put into syrup, during which time ‘Titcomb’s Golden Syrup’ was the choice article of our  groceries. … Titcomb was an industrious, law-abiding citizen; a neighbor to be desired, and an affectionate husband and father.” (Daily Honolulu Press, March 24, 1883)

Titcomb married Kanikele Kamalenui in 1841; they were the parents of at least 3 sons and 5 daughters.  Kanikele died January 16, 1881; Charles died March 21, 1883.

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Whose Footprints Are These?

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

On August 1, 1916, President Woodrow Wilson signed the country’s 13th national park into existence – Hawaiʻi National Park.  At first, the park consisted of only the summits of Kilauea and Mauna Loa on Hawaiʻi and Haleakalā on Maui.

Eventually, Kilauea Caldera was added to the park, followed by the forests of Mauna Loa, the Kaʻū Desert, the rain forest of Olaʻa and the Kalapana archaeological area of the Puna/Kaʻū Historic District.

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

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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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Hawaiian Volcano Research Association

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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