Hawaii Island | Page 31 | Images of Old Hawaiʻi

July 22, 2016 by Peter T Young 1 Comment

Kuakini’s Cotton

“The pleasant village of Kailua is situated on the west side of Hawaii. It is the residence of the Governor of the Island. It is celebrated in Hawaiian history, as having been the residence for several years of Kamehameha I, and at this place he died, on the 8th of May, 1819, at the age of 66 years.”

“Here was first announced by Royal authority, that the old tabu system was at an end. It was in the quiet waters of this bay, that the brig Thaddeus anchored, April 4th, 1820, which brought the first Missionaries to the shores of Hawaii.”

“The natural features of the lofty mountain of Hualālai, and the rugged and rocky coast remain the same; but changes have been gradually going forward in the habits of the people and the appearance of the village.”

“There stands the village church with its tapering spire, almost a lac-simile of some that anciently stood in the centre of the common in many a New England village.”

“During the summer of 1844, we landed at Kailua to commence a tour of Hawaii. It was on the morning of the 1st of July, and we were kindly invited to take up our brief sojourn at the house of the Rev, Mr. Thurston who with his wife and children had been our voyaging companions on board the Clementine, from Honolulu.”

“The day of our landing happened to be the first Monday of the month, which has been so sacredly consecrated by American Missionaries and the churches of the United States, as a day of prayer for the blessing of God upon the Missionary enterprise.”

“It was pleasant to enjoy one of these sacred seasons, on the spot, so replete with incidents calculated to inspire the friend and lover of the cause with thanksgiving and gratitude. As might naturally be supposed, we had a ‘thousand’ inquiries to make of our venerable Missionary best, who bad been here watching the successive phases and changes of events for the last quarter of a century.”

“From our Journal for July 2d, we copy the following: ‘This morning it was proposed that we visit the village. Our steps were first directed to Governor Adams’ ‘factory,’ a long, and low, thatched building, now occupied as a native dwelling and store house.”

“Here the Governor undertook the manufacture of cotton cloth, and actually succeeded so far as to make several hundred yards.” (The Friend, April 15, 1845)

“Governor Kuakini indeed went so far as to manufacture a very stout kind of cloth in Kailua, Hawaii. It was proposed by the Rev. Mr. Armstrong that prizes in money and of sums which would make them worth contending for should be offered on a graduated scale for say, the three best specimens that may be exposed at the exhibition of this year.”

“It was asserted that this cotton raising is a business which will fall in with the habits of the people, and for which they have always evinced an inclination.” (Polynesian, June 11, 1859)

The cloth making experiment begun at Wailuku was continued; spinning and knitting were undertaken at one or two other stations; cotton growing was taken up by the church members at several places as a means of raising funds for new school and church buildings and to aid the missionary cause in general.

At Haiku, Maui, an American farmer commenced a small plantation, having 55 acres planted in 1838. Governor Kuakini of Hawaii. one of the most business-like of the chiefs, visited Miss Brown’s class at Wailuku in 1835 and conceived the idea of having the industry established on his island.

In 1837 the governor was reported by one of the merchants to have planted an immense cotton field at Waimea, Hawaii. In the same year he erected a stone building at Kailua, thirty by seventy feet, to be used as a factory. A foreigner in his employ made a wheel, from which as a sample the natives made about twenty others.

Wheel heads and cards were imported from the United States. Three poorly trained native women served as the first instructors for some twenty or thirty operatives, girls and women from twelve to forty years of age.

In a comparatively short time they acquired a fair proficiency in the work; by the middle of 1838 a large quantity of yarn bad been spun. Two looms were next procured and a foreigner familiar with their operation.

Members of the United States exploring squadron visited the factory in 1840, and the commander of the expedition wrote that the foreigner just mentioned ‘was engaged for several months in the establishment, during which time he had under his instruction four young men, with whom he wove several pieces of brown stripes and plaids, plain and twined cotton cloth.’

‘After this time, the natives were able to prepare and weave independently of his aid. Becoming dissatisfied, however, all left the work, together with the foreigner; but after some time they were induced to return to their work. This small establishment has ever since been kept up entirely by the natives.’ (Kuykendall)

Kuakini’s “scheme failed probably from the fact that the Governor found it cheaper to buy coarse cottons than to make them.” (The Friend, April 15, 1845)

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‘John Adams’ Kuakini, royal governor or the island of Hawai’i, circa 1823

June 26, 2016 by Peter T Young 1 Comment

Kaumana Cave

Hilo is situated on lava flows from two of the five volcanoes that form the Island of Hawaiʻi. In the northern part of Hilo near the Wailuku River (that forms the approximate boundary between Mauna Kea and Mauna Loa Volcanoes,) Mauna Loa flows overlie much older ash deposits and flows from Mauna Kea.

Twenty-seven Mauna Loa flows (pāhoehoe and ʻaʻa) have been identified in and near Hilo. The youngest flow is from the historic Mauna Loa eruption of 1880-81, and the oldest flow yet found lies near Hoaka Road, with an age of more than 24,000 years. (USGS)

The 1881 lavas reached just north of the present University of Hawaiʻi at Hilo campus. After crossing the present Komohana and Kumukoa Streets, a very narrow section crossed what is now Mohouli Street, about 300 yards above the intersection with Kapiʻolani Street.

Several hundred homes are now built on pāhoehoe lavas of the 1881 flow and can easily be recognized by their ubiquitous “rock gardens” (no soils have yet formed on this flow). Kaumana Cave was formed at this time and was a major supply conduit for the lavas that threatened Hilo. (USGS)

Lava Caves (more commonly called lava tubes) are natural conduits through which lava travels beneath the surface of a lava flow. Tubes form by the crusting over of lava channels and pāhoehoe flows.

When the supply of lava stops at the end of an eruption or lava is diverted elsewhere, lava in the tube system drains downslope and leaves partially empty conduits beneath the ground. (USGS)

Kaumana Cave is located up the hill from the downtown area on Kaumana Drive (Saddle Road,) stretching for almost two miles. When you get to the Cave you can see a concrete stair case which leads through the old skylight down to the entrance to the Cave.

The Kaumana Cave, part of a 25-mile-long lava tube, is the centerpiece of a small park maintained by the County of Hawaiʻi. Above Hilo, near the 4-mile marker along Kaumana Drive, the cave’s entrance – actually a skylight formed when part of the lava tube collapsed – is open to curious visitors who want to explore the inside.

The roof of the tube is 20 to 25 feet thick in most places and most of the rubble on the floor fell during or shortly after the eruption, when the skylight entrance fell.

The tube was initially filled with fast-moving lava then the level dropped and a long period of flow along the floor took place and from time to time slopped over to the side creating the bench-like features seen near the cave entrance. Roof blocks fell and became embedded and coated with basalt. The lava stream later emptied leaving the evacuated tube. (Hostra)

A steep staircase leads into a collapse pit. Here the cave roof collapsed and allows entry into the lava tube. From here you can enter different sections of the cave, going mauka (uphill) or makai (downhill) paths.

Going makai, a short path leads to the entrance. There are a few boulders to step carefully through, after which sections of smooth and mostly level surfaces allow a bit easier access. About 50 yards into the downhill section you reach a choke point, a little scrambling and a bit of duck-walk is necessary to get through.

After the narrow, the cave opens back up again. After another hundred yards there are a series of ledges, old crusts left by cooling lava when it half-filled the cave. To continue from here requires crawling through another very low passage. (Cooper)

“Long ʻōhiʻa tree roots hang from overhead … Sides of Cave have dribbles of lava from above forming odd stalagmitelike objects on floor. (There is a) very noticeable slope which is quite easy to travel.”

“Another junction. This one has three branches. There are two shallow rimmed lava cones filled with water. Wedge-shaped overhang is off to one side.” (1953 Loins Club; DOI)

In periods of normal rainfall, running water sometimes is audible beneath the floor of the cave. Rainfalls of 8 to 12 inches produce waterfalls spouting from cracks high on the wall of one cave section.

They form a small stream that runs on or just beneath the floor for several hundred yads before finally sinking into cracks. Its flow is augmented by several small bubbling springs at or just above floor level and part of its flow also is lost into small floor-level cracks. (Halliday)

Kaumana Cave is an example of a lava tube cave that carries floodwater for over half-a-mile. The lower end of Kaumana Cave opens into a drainage ditch several yards below the roadway of Edita Street.

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Kaumana Cave-Map-Halliday

Kaumana_Cave

May 3, 2016 by Peter T Young Leave a Comment

Kamakahonu

“The view of the king’s camp was concealed only by a narrow tongue of land, consisting of naked rocks, but when we had sailed round we were surprised at the sight of the most beautiful landscape.”

“We found ourselves in a small sandy bay of the smoothest water, protected against the waves of the sea; on the bank was a pleasant wood of palm-trees, under whose shade were built several straw houses …”

“… to the right, between the green leaves of the banana-trees, peeped two snow-white houses, built of stone after the European fashion, on which account this place has the mixed appearance of a European and Owhyee village”.

“(T)o the left, close to the water, on an artificial elevation, stood the morai (heiau) of the king, surrounded by large wooden statues of his gods, representing caricatures of the human figure.” (Kotzebue, visiting in 1816)

Several large and densely populated Royal Centers were located along the shoreline between Kailua and Hōnaunau. One such center was located along the north end of Kailua Bay at Kamakahonu.

Kamakahonu (lit. turtle eye) was possibly established as early as the sixteenth century by ʻUmi-a-Līloa. It was during the early nineteenth century that Keawe a Mahi, a kahu of Keaweaheulu presided over Kamakahonu, and upon the death of Keawe a Mahi, Kamakahonu became the residence of Kamehameha I.

During Kamehameha’s tenure at Kamakahonu several structures were erected using both traditional materials and techniques and more “modern” materials and techniques.

Kamehameha first moved into the former residence of Keawe a Mahi. He then built another house on the seaward side of that residence, that was referred to as hale nana mahina ‘ai.

This house was built high on stones and faced directly upland toward the planting fields of Kūāhewa. Like an observation post this house afforded a view of the farm lands and was also a good vantage point to see canoes coming from South Kona and from the Kailua vicinity. (Rechtman)

Much of the following is from John Papa ‘Īʻi’s book, ‘Na Hunahuna no ka Moʻolelo Hawaii’ (Fragments of Hawaiian History;) he was a member of the Kamehameha household.

‘I‘i describes that the “King erected three houses thatched with dried ti leaves,” a sleeping house (hale moe) and separate men’s (hale mua) and women’s (hale ‘āina) eating houses. The hale ‘āina belonged to Kaʻahumanu, and as ‘I‘i described:

“This house had two openings in the gable end toward the west, and close to the second opening was the door of the sleeping house. A third opening was in the end toward the upland.”

“There were three openings in the sleeping house. The one in the middle of the west end, one which served as a window on the upland side of the southwest corner, and one mauka of the window. This window lay beyond the men’s house (mua) on the south. The door mauka of the window was the one entered when coming from the men’s house.”

“The door of the men’s house closest to the sleeping house was the one used to go back and forth between these two houses. There was also a door in the end wall on the west side of this house, and two small openings in the south seaward corner, one in the upper side and one on the lower side of the corner.”

“These faced the many capes of Kona and took in the two extremities of this tranquil land and the ships at anchor. However, should the ships be more to the ocean side, only the masts were visible.”

“A fifth opening was a little on the seaward side of the northeast corner, where the upland side of the men’s house extended a little beyond the sleeping house, and it was only through this entrance that the men went in and out. It was near the door that was used to enter from the sleeping house.”

“Near the door facing westward in the mua, was the king’s eating place. On the upper side were large and small wooden containers that served as bowls and platters, together with a large poi container always filled with poi from the king’s lands.”

“The men’s eating house, the sleeping house, and the women’s eating house were at the end of a 7- to 8-foot stone wall that ran irregularly from there to the shore at the back of the hale nana mahina ‘ai. Outside of the wall was the trail for those who lived oceanward of Kamakahonu. Immediately back of the wall was the pond of Alanaio, where stood some houses.”

“Two eating houses were built for Kaheiheimālie and her daughter, Kekāuluohi, opposite the three houses thatched with ti leaves. They stood back of the kou trees growing there at Kamakahonu, both facing northwest.”

“Kaheiheimālie’s eating house had two doors, but Kekāuluohi’s had but one door. In front of her house was a bathing pool, at the upper bank of which were some small houses and that of the king.”

“A stone house was built between the three houses thatched with ti and those of these chiefesses. Its builder was either a Frenchman or a Portuguese named Aikona. He was skilled in such work…”

“When Aikona began building the end and side walls of the house at Kamakahonu he built a third wall between them and arranged stones in the center of this middle wall to from a door.”

“The walls rose together until the house, from one end to the other, was finished. When Aikona later removed the stones set up in the doorway of the center wall, the doorway looked like the fine arched bridge of Pualoalo at Peleula in Honolulu.”

“As he removed the stones, Aikona explained that had they been piled inexpertly, the whole house might have collapsed. This house was well completed.”

“In the stone house were stored the king’s valuables and those of Aikona’s. These valuables were kegs of rum and gunpowder and guns, of which the guns and powder were placed on the inside near the inner wall. “

“Later, another storehouse was built in Kamakahonu, on the north side of the hale nana mahina ‘ai. It had stone walls and was constructed like a maka halau. The upper of its two stories was for storing tapa, pa‘u, malos, fish nets, lines, and olona fiber; and all other goods went into the lower story.”

“The thatching was of sugar-cane leaves, the customary thatching on the house along that shore. Dried banana trunk sheaths were used for the inside walls and were cleverly joined from top to bottom. Banana trunk sheaths were also used in the hale nana mahina ‘ai.”

“After these houses were built, another heiau house, called Ahuʻena, was restored (ho‘ala hou). This house stood on the east side of the hale nana mahina ‘ai, separated from it by about a chain’s distance.”

“The foundation of Ahuʻena was a little more than a chain from the sand beach to the westward and from the rocky shore to the eastward. Right in front of it was a well-made pavement of stone which extended its entire length and as far out as the place where the waves broke.” (ʻĪʻi, Na Hunahuna no ka Moʻolelo Hawaiʻi’ (Fragments of Hawaiian History))

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Kamakahonu map by Rockwood based on Ii-Rechtman

kamehameha_at_kamakahonu-HerbKane

Temple_on_the_Island_of_Hawaii_by_Louis_Choris_ink,ink_wash_and_watercolor_over_pencil_1816

Map of Kailua Bay-Kekahuna-BishopMuseum

Kailua_Bay-Landing-Map-Wall-Reg2560 (1913)-Kamakahonu_site_on_left

Kailua-Bay-Kamakahonu-Ka_Hale_Pua_Ilima_Foundation-HenryEPKekahuna-BishopMuseum-SP_201853

James_Gay_Sawkins,_England,_1806-1878,_Kailua-Kona_with_Hualalai,_Hulihee_Palace_and_Church-Kamakahonu is at left_1852

Hale ʻIli Maiʻa, the Royal storehouse of King Kamehameha I, Kailua, Kona, Hawaii.

Kamakahonu-DMY

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Kamakahonu_Cove-1954 (Ahuena Heiau Inc)

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Kamakahonu DMY

Kailua Bay aerial 1960s

Kailua Bay aerial 1940s

King_Kamehameha_Hotel-(the_former_hotel)-1960s-1970s

April 24, 2016 by Peter T Young 1 Comment

ʻŌhiʻa

There is a disturbance in the forest.

The native Hawaiian ʻōhiʻa (Metrosideros polymorpha) is the most abundant tree in the Hawaiian Islands, comprising about 62 percent of the total forest area.

The name Metrosideros is derived from Greek metra, heartwood, and sideron, iron, in reference to the hard wood of the genus. Known as ‘Ōhi‘a Lehua, the species is found on all major islands and in a variety of habitats. (Friday and Herbert)

‘Ōhi‘a lehua is typically the dominant tree where it grows. Although the species is little used commercially, it is invaluable from the standpoint of watershed protection, esthetics, and as the only or major habitat for several species of forest birds, some of which are currently listed as threatened or endangered.

ʻŌhiʻa is a slow-growing, endemic evergreen species capable of reaching 75- to 90-feet in height and about 3-feet in diameter. It is highly variable in form, however, and on exposed ridges, shallow soils, or poorly drained sites it may grow as a small erect or prostrate shrub.

Its trunk may range in form from straight to twisted and crooked. Because the species can germinate on the trunks of tree ferns and put out numerous roots that reach the ground, it may also have a lower trunk consisting of compact, stilt-like roots.

The hard, dark reddish wood of ʻōhiʻa lehua was used in house and canoe construction and in making images (ki‘i), poi boards, weapons, tool handles, kapa beaters (especially the rounded hohoa beater), and as superior quality firewood.

ʻŌhiʻa lehua, though of a very nice color, cracks or ‘checks’ too easily to be useful for calabash making. The foliage served religious purposes and young leaf buds were used medicinally. The flowers and leaf buds (liko lehua) were used in making lei.

To Hawaiians of old, the gods were everywhere, not only as intangible presences but also in their myriad transformation forms (kinolau) and in sacred images (ki‘i). Most of the large images were carved from wood of the ʻōhiʻa lehua, an endemic species that is regarded as a kinolau of the gods Kane and Kū.

The materials used in large part depended on the resources available nearby and whether a hale was for aliʻi or makaʻāinana, but in either case, hardwoods were selected for the ridgepoles, posts, rafters, and thatching poles. Hardwoods grew abundantly in Hawaiian forests, in terms of both number of species and the count of hardwoods as a whole.

ʻŌhiʻa lehua grew on all the major islands and was widely used in housebuilding. Canoe decking, spreaders, and seats were commonly made of ʻōhiʻa lehua, as well as for the gunwales.

ʻŌhiʻa lehua was one of the five primary plants represented at the hula altar (ʻōhiʻa lehua, halapepe, ‘ie‘ie, maile and palapalai.) The hālau hula, a structure consecrated to the goddess Laka, was reserved for use by dancers and trainees and held a vital place in the life of an ahupua‘a.

Inside a hālau hula was an altar (kuahu), on which lay a block of wood of the endemic lama, a tree whose name translates as “light” or “lamp” and carried the figurative meaning of “enlightenment.” Swathed in yellow kapa and scented with ‘olena, this piece of wood represented Laka, goddess of hula, sister and wife of Lono.

A number of other deities were also represented on the altar by plants: ʻōhiʻa lehua for the god Kukaʻōhiʻa Laka (named for a legendary ʻōhiʻa lehua tree that had a red flower on an eastern branch and a white one on a western branch) …

… halapepe (Pleomele aurea) for the goddess Kapo; ‘ie‘ie for the demigoddess Lauka‘ie‘ie; maile representirig the four Maile sisters, legendary sponsors of hula; and palapalai fern, symbolic of Hi‘iaka, sister of the volcano goddess Pele and the benefactor of all hula dancers.

Native Hawaiians consider the tree and its forests as sacred to Pele, the volcano goddess, and to Laka, the goddess of hula. ʻŌhiʻa lehua blossoms, buds and leaves were important elements in lei of both wili and haku types.

ʻŌhiʻa is the first tree species to establish on most new lava flows. As the entire portion of eastern Hawaii Island is a volcanic area, lava flows occasionally cover areas of forested land. Thus, while some forests are covered with lava, other forested areas serve as ‘seed banks’ and help to bring growth back life to the lava-impacted area.

There is a disturbance in the forest. Rapid ʻŌhiʻa Death is posing the greatest threat to Hawai‘i’s native forests. A newly identified disease has killed large numbers of mature ʻōhiʻa trees in forests and residential areas of the Puna, Hilo and Kona Districts of Hawaiʻi Island.

Pathogenicity tests conducted by the USDA Agriculture Research Service have determined that the causal agent of the disease is the vascular wilt fungus; although a different strain, this fungus has been in Hawaiʻi as a pathogen of sweet potato for decades.

It is not yet known whether this widespread occurrence of ʻōhiʻa mortality results from an introduction of an exotic strain of the fungus or whether this constitutes a new host of an existing strain. This disease has the potential to kill ʻōhiʻa trees statewide.

The disease affects non-contiguous forest stands ranging from 1 to 100 acres. As of 2014, approximately 6,000 acres from Kalapana to Hilo on Hawaiʻi Island had been affected with stand showing greater than 50% mortality. The disease has not yet been reported on any of the other Hawaiian Islands.

Crowns of affected trees turn yellowish and subsequently brown within days to weeks; dead leaves typically remain on branches for some time. On occasion, leaves of single branches or limbs of trees turn brown before the rest of the crown of becomes brown.

Recent investigation indicates that the pathogen progresses up the stem of the tree. Trees within a given stand appear to die in a haphazard pattern; the disease does not appear to radiate out from already infected or dead trees. Within two to three years nearly 100% of trees in a stand succumb to the disease.

The fungus manifests itself as dark, nearly black, staining in the sapwood along the outer margin of trunks of affected trees. The stain is often radially distributed through the wood.

Currently, there is no effective treatment to protect ʻōhiʻa trees from becoming infected or cure trees that exhibit symptoms of the disease. To reduce the spread, people should not transport parts of affected ʻōhiʻa trees to other areas. The pathogen may remain viable for over a year in dead wood.

UH scientists are working to protect and preserve this keystone tree in Hawaiʻi’s native forest. The Seed Conservation Laboratory at UH Mānoa’s Lyon Arboretum launched a campaign to collect and bank ʻōhiʻa seeds. They will collect and preserve ʻōhiʻa seeds from all islands for future forest restoration, after the threat of Rapid ʻŌhiʻa Death has passed.

I was happy to see the proactive actions taken by the Hawai‘i Department of Agriculture; on a recent trip to the Big Island, they handed out notices to travelers on Hawaiian Air, reminding them not to take ‘ōhi‘a off the island. (Lots of information here is from Abbott and CTAHR.)

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Healthy-Impaired Ohia (UH, Lyon)

Rapid Ohia Death confirmed location (UH-CTAHR, April 13, 2016)

Rapid Ohia Death Symptons -rapid browning of tree crowns-CTAHR

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Ohia-Native_Range-FS-map

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Rapid Ohia Death-Dept-Ag-Brochure-1

Rapid Ohia Death-Dept-Ag-Brochure-2

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Tiny ohia seeds (1-2 mm) under a microscope-UH

April 17, 2016 by Peter T Young Leave a Comment

Lake Waiau

Mauna Kea falls in the senior line genealogy. (Maly)

Former Queen Emma, widow of the late Alexander Liholiho Kamehameha (IV,) and David Kalakaua were in competition for the position of monarch of Hawai’i.

Both of them needed to prove their connection to the senior line and connect back to a wahi pana (celebrated and storied places). Kalakaua went to Kanaloa-Kahoʻolawe to bathe in the waters of the ocean god Kanaloa.

Emma went to the top of Mauna Kea to bathe in the waters of Waiau. The ceremony was to cleanse in Lake Waiau at the piko of the island.

The water caught at Lake Waiau was considered pure water of the gods much like the water caught in the piko of the kalo leaf, the nodes of bamboo or the coconut and is thought of as being pure. (Maly, Mauna-a-Wakea))

Papa is a goddess of earth and the underworld and mother of gods. Wakea is god of light and of the heavens who “opens the door of the sun”. (Beckwith)

“In the genealogy of Wakea it is said that Papa gave birth to these Islands. Another account has it that this group of islands were not begotten, but really made by the hands of Wakea himself.” (Malo)

Waiau is named for the mountain goddess, Waiau (Ka piko o Waiau), and home of the moʻo (water-form) goddess Moʻo-i-nanea.

It is a place where piko of newborn children were taken to ensure long life; and from which “ka wai kapu o Kane” (the sacred water of Kane) was collected. (Maly)

Lake Waiau, located at the 13,020-foot elevation, is on the Island of Hawaii, near the summit of Mauna Kea.

The ancient Hawaiians believed that spirits traveled to and from the spirit world through Lake Waiau, which had ‘no bottom.’ (Actually, the lake has been measured in modern times at 10 feet deep.) The lake freezes over in winter. (Allen)

Lake Waiau is a ‘perched’ water body, in which water is held in a depression by an impermeable substrate of layers of silty clay, interbedded with ash layers, and it has been proposed that permafrost also underlies the lake. It has also been suggested that permafrost surrounds the lake and provides a catchment that directs water into the lake. (USGS)

In 1830, Hiram Bingham and Kauikeaouli (Kamehameha III) ascended Mauna Kea and stopped at Lake Waiau – Bingham noted, “In the morning we proceeded slowly upwards till about noon, when we came to banks of snow, and a pond of water partly covered with ice.”

“In his first contact with a snow bank, the juvenile king seemed highly delighted. He bounded and tumbled on it, grasped and handled and hastily examined pieces of it, then ran and offered a fragment of it in vain to his horse.”

“He assisted in cutting out blocks of it, which were wrapped up and sent down as curiosities to the regent and other chiefs, at Waimea, some twenty-eight miles distant.”

“These specimens of snow and ice, like what are found in the colder regions of the earth, excited their interest and gratified their curiosity, and pleased them much; not only by their novelty, but by the evidence thus given of a pleasant remembrance by the youthful king.”

“After refreshing and amusing ourselves at this cold mountain lake, we proceeded a little west of north, and soon reached the
lofty area which is surmounted by the ‘seven pillars’ which wisdom had hewed out and based upon it, or the several terminal peaks near each other, resting on what would otherwise be a somewhat irregular table land, or plain of some twelve miles circumference.” (Hiram Bingham)

Others made the ascent, “(T)hrough the sliding, weathered lava and cinders, to the pass to the right of the summit cone, and down the slope of the shoulder of the mountain wherein nestles the surprise of Mauna Kea – Lake Waiau.”

“Here, as the sun dipped behind the blue waters of the Pacific, curving up to meet it, we gazed with astonished eyes upon a tiny emerald gem, glacier made in some past time, set in a niche in the arid side of Mauna Kea.”

“We pitched our tent hurriedly by the green, cold lake, built a fire in the whipping trade wind, with its chilly bite, ate an early supper, and retired like packed sardines between our blankets. We were in an arctic zone under a tropic sky.”

“Taking our last look across the lake, we saw the image of fair Venus, streaming in white and shimmering light across the tiny, rippling waves. A thousand jewels glittered in the reflected phantom light of our neighbor planet. The next morning, ice over a half-inch thick was found in the gravel bar about the lake.” (Daingerfield, Paradise of the Pacific, December 1922; Maly)

Another noted, “At last, about 3 PM, we clambered over the rim of a low crater west of the central cones, and saw before us the famous lakelet of Waiau, near which we camped.”

“It is an oval sheet of the purist water, an acre and three quarters in extent, surrounded by an encircling ridge from 90 to 135 feet in height, except at the northwest corner, where there is an outlet, which was only two feet above the level of the lake at the time of our visit.”

“The overflow has worn out a deep ravine, which runs first to west and then to the southwest. A spring on the southern side of the mountain, called “Wai Hu”, is believed by the natives to be connected with this lake.”

“The elevation of Waiau is at least 13,050 feet, which is 600 feet higher than Fujiyama. There are few bodies of water in the world higher than this, except in Thibet or on the plateau of Pamir. No fish are found in its waters, nor do any water-fowl frequent its margins.” (Alexander, Pacific Commercial Advertiser, September 14, 1892)

“Lake Waiau … is the highest lake within the boundaries of the Pacific Ocean Basin. The southern rim of the depression containing the lake is a low segment of a cinder cone, Pu‘u Waiau, on which rests moraine of the latest period of glaciation.”

“The lake water is perched on a layer of silt and mud washed into the basin from the sides of the cone and from the glacial moraine. … The lowest point of the rim is on the western side, where the lake water occasionally overflows into the headwaters of Pohakuloa Gulch.”

“The water is derived entirely from precipitation and runoff from the edges of the basin.” (Geology and Groundwater Resources of the Island of Hawaii, Stearns & Macdonald, 1946)

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