Images of Old Hawaiʻi

by Peter T Young Leave a Comment

Six Active Volcanoes in Hawai‘i

The Hawaiian Islands are at the southeast end of a chain of volcanoes that began to form more than 70 million years ago. Each island is made of one or more volcanoes, which first erupted on the floor of the Pacific Ocean and emerged above sea level only after countless eruptions.

Hawaiʻi sits over a ‘hot spot,’ the Hawaiian hot spot.

It’s one hot spot, but lots of volcanoes have formed over it.  The Islands are above a moving sea floor of the North Pacific Ocean (the Pacific Ocean is mostly floored by a single tectonic plate known as the “Pacific Plate.”)

The Pacific Plate is moving over the layer in the Earth known as the Asthenosphere. This movement takes it to the northwest.  As the plate moves over a fixed spot deeper in the Earth where magma (molten lava) forms, a new volcano can punch through this plate and create an island.

As the plate moves away, the volcano stops erupting and a new one is formed in its place. With time, the volcanoes keep drifting westward and getting older relative to the one active volcano that is over the hot spot.

As they age, the crust that they sit on cools and subsides. This, combined with erosion of the islands, once active volcanism stops, leads to a shrinking of the islands with age and their eventual submergence below the ocean surface.

Each island is made up of at least one primary volcano, although many islands are composites of more than one. The Big Island, for instance, is constructed of 5 major volcanoes: Kilauea, Mauna Loa, Mauna Kea, Hualālai and Kohala (the island is still growing, but is basically about 400,000-years old.)

About 40-million years ago, the Pacific Plate changed direction from north to northwest – so the Emperor Seamounts run more north-south, the Hawaiian Ridge north-westerly.

Midway Island is 27.7-million years old; Meiji Seamount the northern part of the Emperor Seamount (near the end of the Aleutian chain) is about 80-million years old.

All of these are still youngsters, when you look at the perspective, say, of the dinosaurs.  The Islands weren’t even a glimmer in anyone’s eyes when dinosaurs walked the Earth; sixty-five million years ago the last of the non-avian dinosaurs went extinct, after living on Earth for about 165-million years.  (USGS)

If all of Earth time from the very beginning of the dinosaurs to today were compressed into 365 days (1 calendar year), the dinosaurs appeared January 1 and became extinct the third week of September.

Using this same time scale, the Earth would have formed approximately 18.5-years earlier. By comparison, people have been on earth only since December 31 (New Year’s eve.)  (USGS)

While we typically think of and/or hear news reports of eruptions on Kilauea and Maunaloa, presently, the US Geological Survey (USGS) Hawaiian Volcano Observatory  (HVO) monitors the six currently active volcanoes in Hawai‘i.

The Island of Hawai‘i, with four active volcanoes, is liveliest. Between 1912 and 2012, there were nearly 50 Kīlauea eruptions, 12 Mauna Loa eruptions, and one Hualālai intrusion of magma.

Kīlauea, the youngest and most active volcano on the Island of Hawai‘i, erupted almost continuously from 1983 to 2018 at Pu‘u‘ō‘ō and other vents along the volcano’s East Rift Zone. Since then, there have been periodic eruptions in and nearby Halema‘uma‘u crater at the volcano’s summit.

In 2018, Kīlauea experienced the largest lower East Rift Zone eruption and summit collapse in at least 200 years. Several summit eruptions since December 2020 have generated lava lakes that have been slowly filling in the collapsed area, including Halema‘uma‘u crater. About 90 percent of the volcano is covered with lava flows less than 1,100 years in age.

Mauna Loa, the largest volcano on Earth, has erupted 34 times since 1843. An eruption 1984 lasted 22 days and produced lava flows which reached to within about 4.5 miles of Hilo, the largest population center on the Island of Hawai‘i.

The most recent eruption in 2022 lasted two weeks and erupted lava flows that came to within 1.7 miles of the Daniel K Inouye Highway (Saddle Road). Lava flows less than 4,000 years old cover about 90 percent of the volcano.

Hualālai, the third most active volcano on the Island of Hawai‘i, has erupted three times in the past 1,000 years and eight times in the past 1,500 years.

The most recent eruption in 1801 generated a lava flow that reached the ocean and now underlies the Kona International Airport. Lava flows less than 5,000 years old cover about 80 percent of the volcano.

Mauna Kea, the highest volcano on the Island of Hawai‘i, erupted most recently between about 6,000 and 4,500 years ago from at least seven separate summit-area vents, producing lava flows and cinder cones. Glaciers covered parts of the volcano’s summit area during the recent ice ages, the only Hawaiian volcano known to have been glaciated.

Kama‘ehuakanaloa (formerly Lō‘ihi Seamount), the only known active Hawaiian submarine volcano, erupted most recently in 1996 during an earthquake swarm of more than 4,000 events that were recorded by the HVO seismic network. The volcano’s summit is about 3,179 ft below sea level, located 22 miles southeast of the Island of Hawai‘i.

Haleakalā, the only active volcano on the Island of Maui, erupted most recently between about 600 and 400 years ago. In the past 1,000 years, at least 10 eruptions produced lava flows and tephra cones from the rift zone that crosses the volcano from southwest to east and through Haleakalā Crater. (All here is from the US Geological Survey (USGS.))

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Wahaʻula Heiau

No keia heiau oia ke kapu enaena.
(Concerning this heiau is the burning tabu.)

‘Enaena’ means ‘burning with a red hot rage.’ The heiau was so thoroughly ‘tabu,’ or ‘kapu,’ that the smoke of its fires falling upon any of the people or even upon any one of the chiefs was sufficient cause for punishment by death, with the body as a sacrifice to the gods of the temple.  (Westervelt)

Oral traditions trace the origin of Hawaiian luakini temple construction to the high priest Pā’ao, who arrived in the islands in about the thirteenth century. He introduced several changes to Hawaiian religious practices that affected temple construction, priestly ritual, and worship practices.

Prior to his coming, the prayers, sacrifices, and other ceremonial activities that the high chief and his officiating priest performed could be observed by the congregation, who periodically responded as part of the ceremony.

After Pā’ao’s arrival, temple courtyards, which were sometimes built on hillsides to add to their massiveness, were enclosed with high stone walls, preventing the masses from participating as freely in the worship ceremonies.

In addition, new gods; stronger kapu; an independent, hereditary priesthood; wooden temple images; and human sacrifices became established parts of the religious structure. Pā’ao erected the first luakini (Wahaula) at Puna, Hawaiʻi, followed by Moʻokini Heiau at Kohala. These structures signaled a new era in Hawaiian religious practices.  (NPS)

On the southeast coast of Hawaiʻi near Kalapana is one of the largest, oldest and best preserved heiau. Its walls are several feet thick and in places ten to twelve feet high. It is divided into rooms or pens, in one of which still lies the huge sacrificial stone upon which victims – sometimes human – were slain before the bodies were placed as offerings.  (Westervelt, 1915)

“At our visit to the scene we were shown the small cove, deep down the jagged bluffs of Puna’s coast line, at the southern end of Wahaʻula premises, where the bones of the slain were washed, and to this day is known as Holoinaiwi.”  (Thrum, 1904)

This heiau is now called Wahaʻula (red-mouth). In ancient times it was known as Ahaʻula (the red assembly), possibly denoting that at times the priests and their attendants wore red mantles in their processions or during some part of their sacred ceremonies.  (Westervelt)

“The Heiau of Wahaʻula is built on an ʻaʻa flow, and the ascent to it is by terraces. Upon the first terrace the female members of the royal family brought their offerings which were taken by the priests. Beyond this first terrace no female was allowed to pass.”

“Two more terraces brings one to the enclosure or temple, in the shape of a quadrangle 132 feet long, by 72 feet wide. A stone wall encloses the temple, 6 feet high and 4 feet wide. The main entrance faces the East, flanked on either side by two smaller entrances. Immediately in front of this entrance stand the remains of the old temple, which was destroyed by the ʻaʻa flow on which the present one stands.”

“Across the southern end extends a stone platform some 3 feet high built in the shape of two semi-circles connected by a straight platform. Between these semi-circles was placed the presiding deity, and on either hand were placed the offerings of fruits, etc., while immediately in front, on a small raised platform were placed the human sacrifices, which were always slain in the main entrance to the heiau.”

“Immediately in front of this altar for human sacrifices, and extending across the enclosure, stood the priests’ house. sacred to them alone. In the rear of this was the royal house, where the members of the royal family assembled during the days devoted to the sacrifices. The rest of the enclosure was paved.”  (Thrum)

“Water-worn pebbles were carried from the beach and strewn over the floor, making a smooth place for the naked feet of the temple dwellers to pass without injury from the sharp-edged lava. Rude grass huts built on terraces were the abodes of the priests and high chiefs who visited the places of sacrifice.”

“Elevated, flat-topped piles of stones were built at one end of the temple for the chief idols and the sacrifices placed before them. Simplicity of detail marked every step of temple erection.”  (Westervelt)

“(I)in the original enclosure of the heiau of Wahaʻula was a sacred grove, said to contain one or more specimens of every tree growing on the Hawaiian group, a number of which, or their descendants, had survived when he visited the place in 1869. … It was built in the quadrangular or parallelogram form which characterized all the heiaus built under and after the religious regime introduced by Pāʻao.”  (Fornander)

Beyond the heiau, on the makai side of the trail, is pointed out the footprint of Niheu, a demi-god, as well as the mark of an arrow which he shot at another demi-god who came to fight him. Further west, makai of the place where the trail turns mauka, is Kamoamoa, where the ranch driving pens are.

Here are two wells with fair water, and also a fine natural arch by the sea. Here are also a few interesting rock carvings. The most easily found of these is about a hundred yards from the paddock extension towards Kalapana, and may be located by following the line of this extension’s makai wall in an easterly direction.

The trail is straight, with a bad grade, but paved, until it has reached well up the bluff, where it passes the Pea house, the last habitation before the Crater Hotel is reached. From Pea’s it is a good eight miles to the Makaopuhi crater. The trail is narrow, passes through splendid forest, and is, though seldom used, quite easily followed.  (Kinney, 1913)

“Tradition credits a rebuilding of the temple to Imaikalani, a famous chief of Puna, and Kaʻū, in the time of Keawenui-a-umi, in the sixteenth century. It was repaired again in the time of Kalaniʻōpuʻu, about 1770, and in the time of Kamehameha I, it had its final renovation.”  (Thrum)

“This was the last heiau destroyed when the ancient tabus and ceremonial rites were overthrown by the chiefs just before the coming of Christian missionaries. At that time the grass houses of the priests were burned and in these raging flames were thrown the wooden idols back of the altars and the bamboo huts of the soothsayers and the rude images on the walls, with everything combustible which belonged to the ancient order of worship. Only the walls and rough stone floors were left in the temple.  (Westervelt)

Kīlauea’s ongoing Puʻu ʻŌʻō eruption started on January 3, 1983 when ground fissures opened up and “curtains of fire” (long thin fountains of molten lava) issued from a 3½-miles long discontinuous fissure system in the remote rainforest of the middle east rift zone of the volcano.

Since then, about 500-acres have been added to the Big Island (that volume of lava could have filled 1.5-million swimming pools. The coastal highway has been closed since 1987, as lava flows covered 8 miles to as great a depth as 80 feet. 214-homes were destroyed.

“The apprehensions uniformly entertained by the natives, of the fearful consequences of Pele’s anger, prevented their paying very frequent visits to the vicinity of her abode; and when, on their inland journeys, they had occasion to approach Kirauea, they were scrupulously attentive to every injunction of her priests, and regarded with a degree of superstitious veneration and awe the appalling spectacle which the crater and its appendages presented.”

“The violations of her sacred abode, and the insults to her power, of which we had been guilty, appeared to them, and to the natives in general, acts of temerity and sacrilege; and, notwithstanding the fact of our being foreigners, we were subsequently threatened with the vengeance of the volcanic deity, under the following circumstances.”  (Ellis, 1831)

The Wahaʻula Heiau was threatened three times in 1989 and once in 1990, but the lava flowed only up to the walls before diverting around them, but destroyed the visitor center and related facilities (built by the National Park Service in 1964, was destroyed by lava in June 1989.)  However, a subsequent 1997 flow breached the walls and covered the heiau. (star-bulletin)

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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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