Place Names | Page 141 | Images of Old Hawaiʻi

October 31, 2015 by Peter T Young 2 Comments

Kūlou

Hawaiian chronology counts by generations, neither by reigns nor by years. In computing long genealogies, thirty years to a generation is approximately correct. (Fornander)

When ʻUmi died he was succeeded as Mōʻī of Hawaiʻi by his oldest son, Kealiʻiokaloa; he is remembered as an unpopular king, and the only event of note connected with his reign is the arrival on the coast of Kona of some shipwrecked white people.

Arrival of the shipwrecked foreigners – white people – took place between the years 1521-1530 AD. (Fornander)

“In the time of Kealiʻiokaloa, king of Hawaii and son of ʻUmi, arrived a vessel at Hawaii. Konalihoa was the name of the vessel, and Kukanaloa was the name of the foreigner (white man) who commanded, or to whom belonged the vessel. His sister was also with him on the vessel.”

“As they were sailing along, approaching the land, the vessel struck at the pali of Keʻei and was broken to pieces by the surf, and the foreigner and his sister swam ashore and were saved, but the greater part of the crew perished perhaps; that is not well ascertained.”

“And when they arrived ashore they prostrated themselves on the beach, uncertain perhaps on account of their being strangers, and of the different kind of people whom they saw there, and being very fearful perhaps.”

“A long time they remained prostrated on the shore, and hence the place was called Kūlou, and is so called to this day. The white rock there is called Pohakukea, and the cliff above ‘Mauna-kapu,’ or Sacred Mountain, for there the Spaniards are said to have worshipped.”

“And when evening came the people of the place took them to a house and entertained them, asking them if they were acquainted with the food set before them, to which they replied that they were; and afterwards, when breadfruit, ohis and bananas were shown them, they expressed a great desire to have them.”

“The strangers cohabitated with the Hawaiians and has children with they became ancestors of some of the Hawaiian people, and also of some of the chiefs”

They were known as Lala kea, meaning white branch of the tree. To the Hawaiians the white man was termed kekea, while haole meant any foreigner, irrespective of color. (Fornander; Taylor)

In Burney’s ‘Discoveries in the South Seas,’ on October 31, 1527, three vessels left a port called Zivat Lanejo, said by Galvaom to be situated lat. 20° N. on the coast of New Spain, for the Moluccas or Spice Islands.

The vessels were called the ‘Florida,’ with fifty men, the ‘St. Iago,’ with forty-five men, and the ‘Espiritu Santo,’ with fifteen men. They carried thirty pieces of cannon and a quantity of merchandise, and they were under the command of Don Alvaro de Saavedra.

These vessels sailed in company, and when they had accomplished 1000 leagues from port, they were overtaken by a severe storm, during which they were separated. The two smaller vessels were never afterwards heard of, and Saavedra pursued the voyage alone in the ‘Florida,’ touching at the Ladrone Islands. (Fornander)

“It seems certain that a foreign vessel which was wrecked about this time on the Kona coast of Hawaii must have been one of Saavedra’s missing ships.” (Alexander; Westervelt)

From this ship a white man and woman escaped. After reaching the beach they knelt for a long time in prayer. The Hawaiians, watching them, waited until they rose, and received welcome.

The place was at once named ‘Kūlou’ (kneeling.) Through all the succeeding years the name kept the story of the wrecked white chiefs before the Hawaiian people.

The Hawaiians received their white visitors as honored guests, and permitted them to marry into noted chief-families. In the Hawaiian legends the man and woman are called brother and sister. The man was named Kukanaloa. (Westervelt)

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October 21, 2015 by Peter T Young Leave a Comment

Kaʻau

“Go hence to your father,
‘Tis there you find line and hook.
This is the hook-‘Made fast to the heavens’
‘Manaia-ka-lani’ – ‘tis called.
When the hook catches land
It brings the old seas together.
Bring hither the large Alae,
The bird of Hina.”

(Queen Liliʻuokalani, in a translation of the Kumulipo, Hawaiʻi’s creation chant, speaks of Hina’s advice to her son Maui.)

The demi-god Maui is the subject of extraordinary stories throughout Polynesia. In many of the accounts he is a mischievous trickster, stealing the secret of fire and helping his mother to dry kapa by lassoing the sun to slow its progression across the sky. (Bishop Museum)

“The most audacious terrestrial undertaking of the demigod Maui was his attempt to rearrange the Islands of the group and assemble them into one solid mass.”

“Having chosen his station at Kaʻena Point, the western extremity of Oʻahu, from which the island of Kauai is clearly visible on a bright day, he cast his wonderful hook, Mana-ia-ka-Iani, far out into the ocean that it might engage itself in the foundations of Kauai.”

“When he felt that it had taken a good hold, he gave a mighty tug at the line. A huge boulder, the Pōhaku O Kauai, fell at his feet.”

“The mystic hook, having freed itself from the entanglement, dropped into Pālolo Valley and hollowed out the crater, that is its grave.” (Manaiakalani, therefore, formed Kaʻau Crater.)

“This failure to move the whole mass of the island argues no engineering miscalculation on Māui’s part. It was due to the underhand working of spiritual forces.”

“Had Maui been more polite, more observant of spiritual etiquette, more diplomatic in his dealings with the heavenly powers, his ambitious plans would, no doubt, have met with better success.” (Emerson)

Another story of Kaʻau relates to how Helumoa at Waikiki got its name. It involves Kakuhihewa, Maʻilikukahi’s descendent six generations later, ruling chief of O‘ahu from 1640 to 1660 (Maʻilikukahi is honored as the first great Chief of O‘ahu and legends tell of his wise, firm, judicious government.)

It is said that the supernatural chicken, Kaʻauhelemoa one day flew down from his home in Kaʻau Crater in Pālolo and landed at Helumoa.

Furiously scratching into the earth, the impressive rooster then vanished. Kākuhihewa took this as an omen and planted niu (coconuts) at that very spot.

Helumoa (meaning “chicken scratch”) was the name he bestowed on that niu planting that would multiply into a grove of reportedly 10,000-coconut trees.

This is the same coconut grove that would later be called the King’s Grove, or the Royal Grove, and would be cited in numerous historical accounts for its pleasantness and lush surroundings.

Kamehameha and his warriors camped near there, when they began their conquest of O‘ahu in 1795. Later, he would return and build a Western style stone house for himself, as well as residences for his wives and retainers in an area known as Pua‘ali‘ili‘i.

Kamehameha I resided at Helumoa periodically from 1795 to 1809. He ended Waikīkī’s nearly 400-year reign as O‘ahu’s capital when he moved the royal headquarters to Honolulu (known then as Kou) in 1808 (to Pākākā.)

Here’s a little geological background on Kaʻau Crater …

The Hawaiian Islands were formed as the Pacific Plate moved westward over a geologic hot spot. Oʻahu is dominated by two large shield volcanoes, Waiʻanae and Koʻolau that range in age from two to four-million years old.

The younger volcanic craters formed after Oʻahu had moved well off the hot spot and the main shield volcanoes had gone dormant for at least two-million years.

Somewhat more than half of the craters of southeast Oʻahu are arranged in linear groups, those dominated by the craters Tantalus, Diamond Head and Koko Crater. In the Diamond Head group is the main Diamond Head vent, Kaimuki crater and Mauʻumae crater. Kaʻau is an extension of this line of craters up into the Koʻolau range.

The Koko group crater line extends for a distance of about six miles, through the Koko Crater vent and from Mānana Island to Koko Head. It includes no less than fourteen separate vents and dikes, of which most are distant from a straight line but a few yards. (Bishop Museum)

“The Kaʻau tuff and basalt flows were erupted during a high stand of the sea (probably during plus 95-foot (Kaʻena) stand of sea)” (about 1-million years ago – a ‘youthful’ volcanic outburst.) (USGS)

Rising magma encountered groundwater and generated steam explosions. Kaʻau crater was probably blasted out by the explosions. Its walls are Koʻolau basalt, overlain by tuff and mudflow debris.

Toward the end of the eruption, lava rose in Kaʻau crater, probably forming a lava lake. Slight recession of the lava in the crater at the end of the eruption left a poorly drained hollow forming a swamp that sometimes contains an open pond. (Volcanoes in the Sea)

(Kaʻau Crater is reached from the end of the Pālolo valley. The trail (muddy and wet) is a closed trail and is not open to the public – news reports note people are repeatedly rescued from there and a couple people recently died on the trail (portions of the trail involve ascending the waterfalls along the way.)

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October 16, 2015 by Peter T Young Leave a Comment

Laniākea Cave

Reverend Asa and Lucy Thurston were in the Pioneer Company of American Christian Missionaries to the Hawaiian Islands, arriving in Kailua-Kona on the Thaddeus in 1820.

“After an accurate investigation of the places adjacent, in which they thought it might be found, they chose a valley, about half a mile from the residence of the governor, and near the entrance of Raniakea, as the spot where they were most likely to meet with success.” (Ellis)

They made their home in Kailua Village, in a home the Hawaiians named Laniākea. Thurston received Laniākea, a 5.26 acre homestead parcel as a gift from Governor Kuakini.

As noted by Rev. Sereno Edwards Bishop, in his book “Reminiscences Of Old Hawaii” (1916:) “In the early (1830s,) Kailua was a large native village, of about 4,000 inhabitants rather closely packed along one hundred rods of shore, and averaging twenty rods inland.”

“It had been the chief residence of King Kamehameha, who in 1819 died there in a rudely built stone house whose walls are probably still standing on the west shore of the little bay. Nearby stood a better stone house occupied by the doughty Governor Kuakini.”

“All other buildings in Kailua were thatched, until Rev. Artemas Bishop built his two-story stone dwelling in 1831 and Rev. Asa Thurston in 1833 built his wooden two-story house at Laniākea, a quarter of a mile inland.”

“Most of the native huts were thatched with the stiff pili grass. The better ones were thatched with lau-hala (pandanus leaf) or with la-i.” (Bishop)

“Five acres were enclosed with a stone wall three feet wide and six feet high, with simply the front gate for entrance. A large thatched house was erected. Space was allowed for a yard twenty-five feet in breadth.” (Lucy Thurston)

“Thatched houses are not durable, therefore, in the course of years, we had a succession of dwellings, but this was the general arrangement. In the 12th year of the Mission, a two-storied wooden house was erected in the children’s yard, and the wall for their special enclosure removed, as the times no longer required such an accommodation.” (Lucy Thurston)

In 1823, English protestant missionary William Ellis joined forces with American protestant missionary Asa Thurston and a party of explorers to circumnavigate the island of Hawaii.

“In the course of the forenoon, two of our number visited the ruins of an old military fortification, formerly belonging to the makaʻāinana, (common people.)”

“All that at present remains, is a part of the wall, about twelve feet high, and fourteen feet thick at the bottom, built of lava, and apparently entire.”

“In the upper part of the wall are apertures resembling embrasures; but they could not have been designed for cannon, that being an engine of war, with which the natives have but recently become acquainted.”

“The part of the wall now standing, is near the mouth of Raniakea (Laniākea,) the spacious cavern … which formed a valuable appendage to the fort.” Ellis)

“The whole face of the country marked decisively its volcanic origin; and in the course of their excursion they entered several hollows in the lava, formed by its having cooled and hardened on the surface, while, in a liquid state underneath, it had continued to flow towards the sea, leaving a crust in the shape of a tunnel, or arched vault, of varied thickness and extent.

“After entering it by a small aperture, they passed on in a direction nearly parallel with the surface; sometimes along a spacious arched way, not less than twenty-five feet high and twenty wide…”

“… At other times, by a passage so narrow, that they could with difficulty press through, till they had proceeded about 1,200 feet; here their progress was arrested by a pool of water, wide, deep, and as salt as that found in the hollows of the lava within a few yards of the sea.” (Ellis)

“One may walk along it for about fifteen minutes, through a passage which often reaches a considerable height. … The cave runs into a deep subterranean pool of very cold water, and further progress can be made only by swimming through an aperture in the makai end, when one may enter an inner cave, which is said to lead to the sea.” (Kinney, 1913)

“More than thirty natives, most of them carrying torches, accompanied (Ellis’ group) in their descent; and on arriving at the water, simultaneously plunged in, extending their torches with one hand, and swimming about with the other.”

“The partially illuminated heads of the natives, splashing about in this subterranean lake; the reflection of the torch-light on its agitated surface; the frowning sides and lofty arch of the black vault, hung with lava, that had cooled in every imaginable shape …”

“… the deep gloom of the cavern beyond the water; the hollow sound of their footsteps; and the varied reverberations of their voices, produced a singular effect; and it would have required but little aid from the fancy, to have imagined a resemblance between this scene and the fabled Stygian lake of the poets.”

“The mouth of the cave is about half a mile from the sea, and the perpendicular depth to the water probably Not less than fifty or sixty feet.”

“The pool is occasionally visited by the natives, for the purpose of bathing, as its water is cool and refreshing. From its ebbing and flowing with the tide, it has probably a direct communication with the sea.” (Ellis)

When war threatened the early inhabitants of Kona, and it was not uncommon, those who could not fight took refuge in the cave, and while the battles raged overhead, the refugees sent forays up the mountain and to the sea, via the cave, to gather food and water. (laniakea)

“In this cavern, children and aged persons were placed for security during an assault or sally from the fort, and sometimes the wives of the warriors also, when they did not accompany their husbands to the battle.”

“The fortification was probably extensive, as traces of the ancient walls are discoverable in several places; but what were its original dimensions, the natives who were with us could not tell. They asserted, however, that the cavern, if not the fort also, was formerly surrounded by a strong palisade.” (Ellis)

When the Thurstons retired to Honolulu, the house and land became the property of Mokuʻaikaua Church.

In 1980, sections of the cave had collapsed and the entrance was choked with debris and the entrance near the Thurston House was disturbed by squatters.

Waste products and debris have been dumped into the cave, causing an accumulation of sediment and muck within the cave. The western entrance to the cave near Hale Halawai is blocked. Large concrete pillars within the cave apparently were place to support improvements above. (Rasmussen)

The Laniākea house fell into disrepair, and in the 1990s the Laniākea Foundation was formed to save the ruins of the cave and home site from development. (laniakea)

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October 14, 2015 by Peter T Young 3 Comments

Wahiawā Hotel

“An instance of community enterprise truly admirable is being exhibited by the Wahiawā Settlement Association in the erection of a hotel in that Salubrious village.”

“As shown in the list of building permits in this paper the other day, the building is estimated to cost $3,650, and the plans have been prepared by Emory & Webb, architects. Its location is 300 feet from the railway station.” (Star Bulletin, January 21, 1913)

Let’s look back …

In 1897, Californian, Byron Clark, became the Hawaiian Republic’s commissioner of agriculture. In looking for land for him to settle on, he learned of the availability of land at Wahiawā.

Clark organized a group of other Californians (as well as others) to join him in settling the whole tract of thirteen hundred acres — which became known as the Wahiawā Colony Tract. Having formed an agricultural cooperative called the Hawaiian Fruit and Plant Company, the homesteaders began formalizing and refining the physical organization of their Wahiawā settlement.

Initially each settler lived in a house on his five-acre parcel in the town site and farmed his other land in the surrounding area. It was soon discovered, however, that each settler preferred to reside on his own farmstead, holding his town lot in reserve. The homesteaders abandoned the village plan and agreed that one man, Thomas Holloway, would live on their 145-acre central lot site.

On August 27, 1902 a trust deed, referred to as the Holloway Trust, formally set aside the central town lots for the use and benefit of the Settlement Association of Wahiawā resident landowners.

Within a few years, Wahiawā Town was underway. Some of the town’s streets would be named for the early homesteaders – including Clark, Kellogg, Thomas and Eames streets (initial mapping shows California Avenue as the first, and main, road.)

Back to the hotel … “This hotel scheme was taken up by the association as the best way to expend a snug balance in the settlement funds, as well as to utilize the hall that had been erected for community gatherings.”

“Originally the structure was used for a schoolhouse, but ultimately the government provided a school building for itself. Besides erecting the hotel, the association is going to provide Uncle Sam with a post office building.”

“There are two buildings in the establishment as planned, the main building to be an auxiliary cottage the old assembly hall reconstructed. In the main building there will be six bedrooms, a parlor and a dining room, the last being utilizable also as a living room.”

“The remodelled cottage will have four bedrooms. A veranda ten feet wide will extend along the four sides of the main building. The bedrooms are of good size, the four on the ground floor of the main building being 12 by 13 feet. There is a gable outlook on every side of the house, each commanding beautiful scenery.”

“Each house is equipped with all needed conveniences, including linen closets. Guests will have pure water from the clouds, a large tank for rain water being provided. This is exclusively for drinking purposes as for other uses the hotel will be connected with the piped mountain water system of the settlement.” (Star Bulletin, January 21, 1913)

At the corner of Lehua Street and California Avenue stood the old Wahiawā Hotel. The “cottages,” as the hotel was referred to, was operated by Mary Johnson until World War II, when it was formally taken over by the Army for nurses’ quarters.

The start of World War II further helped to accelerate developments within Wahiawā to accommodate the needs of the growing military population. Wahiawā Elementary School on Lehua Street soon closed their doors in the 1940s to become the new Wahiawa General Hospital.

The Office of Civil Defense established a 42-bed wartime medical facility in the wood frame buildings formerly housing Wahiawā Elementary School.

At the end of World War II, the facility continued to remain in operation under the leaders of the Wahiawā Hospital Association. The 72-bed acute care facility was dedicated in 1958, under the official name, Wahiawā General Hospital. (Cultural Surveys)

Post World War II, the old Wahiawā Hotel had been used as living quarters for area school teachers. By the 1960s, Wahiawa teachers, who had been quartered at the teachers’ cottages (as they referred to them), were forced to relocate as plans for the new Wahiawa Branch Library were in the making. (Cultural Surveys)

Wahiawā Hotel was demolished in the 1960s to accommodate construction for the new Wahiawā Library. The library opened its doors on July 19, 1965. The library continues to remain in operation today. (Cultural Surveys)

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October 12, 2015 by Peter T Young Leave a Comment

Molokini

“Uluhina then was called upon,
The navel of the little one was cut,
The afterbirth of the child that was thrown
Into the folds of the rolling surf;
The froth of the heaving sea,
Then was found the loin cloth for the child.
Molokini the island
Is the navel string,
The island is a navel string.” (Fornander)

When Walinuu gave birth to Kahoolawe, Uluhina was called upon to come and cut the navel of the child Kahoolawe, and when he came and had cut the navel he took the placenta and girt it on as a loin cloth.

He then threw it into the sea and Molokini arose formed from the afterbirth of Kahoolawe and the loin cloth of Uluhina, the very name Molokini being a contraction of the words malo and Uluhina. (Fornander)

Molokini erupted about 230,000 years ago (90,000+/-;) it’s a tiny, crescent-shaped island in the ‘Alalakeiki Channel, 3-miles offshore of Haleakala volcano, East Maui.

The volcanic cone rises about 500-feet from the submarine flank of Haleakala to a summit of only 162-feet above sea level. The cone is capped by a 1770-foot crater, although the northern rim is below sea level and the crater is flooded by the sea.

Molokini is similar to cinder cones elsewhere along the southwest rift zone, except that it erupted through water. When magma erupts explosively in shallow water, the liquid water heats, expands rapidly, and changes to steam, adding to the eruptive force.

The extra force shatters the extruded lava, which exposes more hot material–and hence more steam and more force as the eruption grows. Near-shore eruptions are some of the most dangerous that Hawaiian volcanoes can produce.

Shallow marine eruptions have two consequences for the appearance of the resulting cone. The first is grain size (marine eruptions leads to finer-grained deposits;) the second is the abundance of volcanic glass (because the lava fragments are quickly cooled by water before crystals can form.)

Molokini deposits are basanite, a type of basalt with fairly low amounts of silicon and high concentrations of sodium and potassium. (USGS)

The shallow inner cove is the crater’s submerged floor. Black coral was once found in abundance in the deeper waters around Molokini, but was harvested extensively. (Harvesting is now restricted, and small colonies can be found on the islet’s back wall.)

There is no sand beach on Molokini. The cove area slopes off from the shoreline to a depth of about 100 feet before dropping off. The bottom consists of sand patches, coral and basaltic boulders

A shallow reef in less than thirty feet of water extends from the shoreline northward at the islet’s northwestern point. It is a very popular snorkeling area with tour boats packing people in.

It is part of a Marine Life Conservation District (MLCD.) The diversity of fishes and other marine life within the MLCD is among the most impressive in the state. Even humpback whales have been known to enter the cove. (DLNR-DAR)

Molokini was part of prior military training; in 2006 & 2007, a 250-pound bomb, a 105mm projectile and a 5-inch rocket were found during surface surveys by the Navy.

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