Images of Old Hawaiʻi

by Peter T Young 1 Comment

Captain Jacob Brown

Captain Jacob Brown was “a follower of the sea from his twentieth year”.

The whalers of New Bedford and the other Eastern Ports fished the Atlantic and Pacific Oceans.  They were hunting for whale products that were in high demand – whale oil was used for heating, lamps and in industrial machinery; whale bone was used in corsets, skirt hoops, umbrellas and buggy whips.

In the Pacific, rich whaling waters were discovered near Japan and soon hundreds of ships headed for the area.   The central location of the Hawaiian Islands between America and Japan brought many whaling ships to the Islands.

Whalers needed food and the islands supplied this need from its fertile lands.

William Rotch, the owner of several whaling vessels, was reportedly Nantucket’s greatest whaling merchant; he later moved to New Bedford. One of his ships was the Honqua (sometimes spelled Hoqua.)

Crew list records from the New Bedford ships’ registries show that Jacob Brown was First Mate on the Honqua on an Atlantic whale hunt from July 19, 1841 to June 29, 1843.

Then, on a September 1, 1843 to April 13, 1846 hunt into the Pacific, Brown was Captain.  He later captained another Honqua Atlantic whaling ground sail from 1846 to 1849.

It’s not clear if there were intervening sailings, but on a whale hunt in the North Pacific, Brown captained one of “seven sails of this fine fleet of 1851, the Honqua, the New Bedford, the Arabella, the America, the Armata, the Mary Mitchell, and the Henry Thompson, (that were) wrecked there, and left behind as monuments of the dangers which meet these hardy mariners in their adventurous calling.”

“The Honqua, in 1851, was totally wrecked on a sunken rock in that sea (near Cape Oliver (Sea of Ochotsk, Russia – near the Arctic Circle.”))

Brown and his wife Cordelia Hastings Brown were shipwrecked and spent four months in the Siberian snows before being rescued by a whaling ship.

All was not lost,  the rescuing Captain of the whaleship Canton, Captain James Allen Towners, purchased the salvaged  whale oil of the Honqua (1,100 bbls of oil saved, however sold at a heavily discounted price.)

From Siberia, Brown and family were eventually brought to Hawaiʻi, by way of China.

After making a trip to his home in New Bedford, Massachusetts, Captain Brown returned to Hawaiʻi a year later, his family joining him in Honolulu six years later, and remained to take a part in the development of the islands.

He retired from the sea in 1852 to assume a government position in Honolulu which placed him in charge of all government wharves and buoys at the port.

He was also captain of the towing tug “Pele.” The “Pele” was the first steam tug used in Hawaiʻi (screw tug with thirty-horse power,) called into service in 1854.

Its primary use was for towing vessels in and out of the harbor and replaced the use of men or animals to bring ships into the harbor against the prevailing northeast tradewinds.

“Prior to the launching of this vessel primitive power was used to bring the craft through the passage to an anchorage; a rope of great length was used, and it was a never-to-be-forgotten sight to see yokes of oxen, teams of horses and natives tugging at the rope. A time was consumed in making a start, but when once in motion, it was a steady walk-away.”

Richards Street was aligned as a straight path used by groups of men, and later oxen, to pull ships through the narrow channel into the harbor.

In 1856, the Pele was also used to tow barges about the harbor in connection with the Honolulu Harbor dredging operations. Pele served, with short interruptions, as the sole tug for shipping at Honolulu until after 1882.

Brown is later noted as registered owner or partner in several boats in Honolulu: Warwick, Jenny, Haunani, James Makee and CR Bishop.  These were typically used for inter-island movement of people and goods.

One of the partners was Thomas R Foster, an initial organizer of the Inter-Island Steam Navigation Company which was later incorporated on February 19, 1883.   (Brown, a friend of Foster’s, was one of the original promoters of the Inter-Island Steam Navigation Company.)  That company founded a subsidiary, Inter-Island Airways, that later changed its name to Hawaiian Airlines.

Born in 1815 to Jacob Brown and Ruth Morgan Brown, Captain Jacob Brown died on July 3, 1881 in Boston, Massachusetts, at the age of 66.  He and members of his family are buried at Oʻahu Cemetery.

He was survived by three children, Jacob F Brown (Civil Engineer and Manager of Hawaiian Abstract & Title,) Arthur M Brown (Attorney, High Sheriff in the Territory of Hawaiʻi (1898-1906,)) and Minnie H (Brown) Gilman; his oldest child, Sarah M Brown, born at sea, later died at the age of 22.

© 2022 Hoʻokuleana LLC

by Peter T Young Leave a Comment

Mākaha

The ahupuaʻa of Mākaha, between Waiʻanae Ahupuaʻa to the southeast and Keaʻau Ahupua‘a to the northwest, extends from the coastline to the Waiʻanae Range.

Pukui noted Mākaha means “fierce;” Roger C. Green suggests it relates to “fierce or savage people” once inhabiting the valley.

Green refers to “…the ʻŌlohe people, skilled wrestlers and bone-breakers, by various accounts [who] lived in Mākaha, Mākua, and Keaʻau, where they often engaged in robbery of passing travelers.”  (Cultural Surveys)

Earliest accounts describe Mākaha as a good-sized inland settlement and a smaller coastal settlement.  These accounts correlate well with a sketch drawn by Bingham in 1826 depicting only six houses along the Mākaha coastline.

Green describes Mākaha’s coastal settlement as “…restricted to a hamlet in a small grove of coconut trees on the Keaʻau side of the valley, some other scattered houses, a few coconut trees along the beach, and a brackish water pool that served as a fish pond, at the mouth of the Mākaha Stream.” (Cultural Surveys)

This stream supported traditional wetland agriculture – kalo (taro) – in pre-contact and early historic periods

Supporting this, Māhele documents note Mākaha’s primary settlement was inland where waters from Mākaha Stream could support lo‘i and kula plantings. Although there is evidence for settlement along the shore, for the most part, this was limited to scattered, isolated residents.

A “cluster” of habitation structures was concentrated near Mākaha Beach, near the Keaʻau side of Mākaha where there is also reference to a fishpond.

John Papa ʻĪʻī described a network of Leeward O‘ahu trails, which in early historic times crossed the Waiʻanae Range, allowing passage from Central O‘ahu through Pōhākea Pass and Kolekole Pass.

The old coastal trail probably followed the natural contours of the topography. With the introduction of horses, cattle and wagons in the 19th century, many of the coastal trails were widened and graded to accommodate these new introductions.  The Pu‘u Kapolei trail gave access to the Waiʻanae district from Central O‘ahu, which evolved into the present day Farrington Highway.

Kuhoʻoheihei (Abner) Pākī, father of Bernice Pauahi, was given the entire ahupuaʻa of Mākaha by Liliha after her husband, Boki, disappeared in 1829.

In 1855, after Chief Pākī died, the administrators of his estate sold the Mākaha lands to James Robinson and Co. Later, in 1862, one of the partners, Owen Jones Holt, bought out the shares of the others.

The Holt family dominated the social, economic and land-use activities in Mākaha until the end of the 19th century. During the height of the Holt family presence, from about 1887 to 1899, the Holt Ranch raised horses, cattle, pigs, goats and peacocks.

Mākaha Coffee Company bought land for coffee cultivation in the Valley, although coffee never caught on. On Holt’s death in 1862, the lands went into trust for his children.

By 1895 the OR&L rail line reached Waiʻanae.  It then rounded Kaʻena Point to Mokuleʻia, eventually extending to Kahuku.  Another line was constructed through central O‘ahu to Wahiawa.

The Holt Ranch began selling off its land in the early-1900s.

In 1908, the Waiʻanae Sugar Company moved into Mākaha and by 1923, virtually all of lower Mākaha Valley was under sugar cane cultivation.  The plantation utilized large tracks of Lualualei, Waiʻanae and Mākaha Valley.

In the 1930s, Waiʻanae Plantation sold out to American Factors Ltd (Amfac.)  They started looking for a water source to increase production of the thirsty crop.  They tunneled for water; Glover Tunnel, named for the contractor, was 4,200-feet long and had a daily water capacity of 700,000-gallons. The water made available was mainly used for the irrigation of sugar.

For a half century, Mākaha was predominantly sugarcane fields.  However, by the middle of the century, the operations were no longer profitable and the plantation started to liquidate.

In 1946, the Dillinghams announced that they were discontinuing rail service, citing decline in tonnage, rising labor costs and tsunami damage in the system. On October 17, 1946 the stockholders of American Factors (owners of the Waiʻanae Sugar Company) voted to liquidate.

Chinn Ho’s Capital Investment Corporation bought the Mākaha lands and looked to resort development in the Valley.  He envisioned a travel destination that would be the next Kaʻānapali or even Waikiki, with golf courses, condominiums and hotels.

When the Mākaha big surf break was discovered and the eventual Mākaha International Surfing Championship was underway, tourists starting coming to Waiʻanae in the 1950s, as pioneer surfers made Mākaha Beach famous.

In 1969, the Mākaha Resort was built, including Mākaha Inn and Country Club, with an 18-hole course with tennis courts, restaurant and other golf facilities was opened for local and tourist use.

Over the decades, the resort has had several starts and stops, as well as a number of transfers of ownership.

© 2023 Hoʻokuleana LLC

by Peter T Young 1 Comment

Size Matters

In expanse, Honolulu is the “largest” city in the world. Whoa … let’s take a look at what this means.

Downtown Honolulu used to be known as Kou, a district roughly encompassing the area from Nuʻuanu Avenue to Alakea Street and from Hotel Street to Queen Street (which, then, was the edge of the waterfront) – essentially the heart of the present downtown.

Honolulu Harbor, known as Kuloloia, was entered by the first foreigner, Captain William Brown of the English ship Jackall, in 1794. He named the harbor Fair Haven (some other foreign captains referred to it as Brown’s Harbor.)

The name Honolulu (with numerous variations in spelling) soon came into use. In the 1800s, the City of Honolulu was the area near the harbor which is now referred to as downtown Honolulu.

Today, some of us simply call it “Town.”

OK, so what really makes up the present day City & County of Honolulu … and how big is it?

In expanse, Honolulu is the “largest” city in the world.  We know it includes the island of Oʻahu; but that’s not all.  Let’s take a look at how and what makes up Honolulu – to get there, though, we first need to wade through some political and legal mumbo jumbo.

The State Constitution states that the area of the State includes the land, reefs and archipelagic waters:
“Hawaiʻi Constitution; Article XV – State Boundaries; Section 1.  The State of Hawaiʻi shall consist of all the islands, together with their appurtenant reefs and territorial and archipelagic waters, included in the Territory of Hawaiʻi on the date of enactment of the Admission Act, except the atoll known as Palmyra Island, together with its appurtenant reefs and territorial waters; but this State shall not be deemed to include the Midway Islands, Johnston Island, Sand Island (offshore from Johnston Island) or Kingman Reef, together with their appurtenant reefs and territorial waters.”

The Constitution also gives the legislature the authority to create Counties and other political subdivisions: “Article VIII – Local Government Creation; Section 1.  The legislature shall create counties, and may create other political subdivisions within the State, and provide for the government thereof.  Each political subdivision shall have and exercise such powers as shall be conferred under general laws.”

State law (Hawaiʻi Revised Statutes) says the archipelagic waters and smaller islands are included when describing districts: Hawaiʻi Revised Statutes – §4-3 Districts include archipelagic waters, etc.  Each of the districts includes archipelagic waters and smaller islands adjacent thereto.  (Archipelagic means an expanse of water with many scattered islands.  (Lee))

So, before we see what “Honolulu” really is, let’s look at the make-up of the State.

Hawaiʻi is geographically an archipelago. It consists of eight main islands, plus a chain of islands extending 1,100-miles to the northwest.  Johnston Atoll (Kalama), Palmyra Island and Kingman Reef to the south of Hawaiʻi were part of the Kingdom of Hawaiʻi, but the Admission Act excluded these from the geographical boundaries of the State of Hawaiʻi. (Van Dyke)

The Main Hawaiian Island group consists of the following islands:  Hawaiʻi, Maui, Oʻahu, Kauaʻi, Molokai, Lānaʻi, Niʻihau, Kahoʻolawe, Molokini, Lehua and, Kaʻula.

Papahānaumokuākea (Northwestern Hawaiian Islands) consists of all islands, atolls, reefs and shoals in the Hawaiian Archipelago northwest of Kauaʻi and Niʻihau.   All islands, atolls, reefs and shoals in the Hawaiian Archipelago, except for the Midway Islands, are included in the State of Hawaiʻi under the Admission Act, the State Constitution and the Hawaiʻi Revised Statutes.

Nine larger islands, or island groups, in the Northwestern Hawaiian Islands are: Nihoa, Necker Island, French Frigate Shoals, Gardner Pinnacles, Maro Reef, Laysan Island, Lisianski Island, Pearl and Hermes Atoll, and Kure Atoll (southeast to northwest.)

Many of these islands, or groups of islands, actually consist of many islets; for example, French Frigate Shoals contains 13 specific islets. The nine major islands, or groups of islands, range in size from Maro Reef with less than one acre to Laysan Island with 913 acres.

OK, some more political and legal mumbo jumbo.  The origin of county government within the American context is found in the Organic Act (June 14, 1900) which created the Territory of Hawaiʻi and which gave it the authority to establish municipalities.

The Territorial Legislature made a first attempt at creation of the four counties in 1903 (Act 31;) however, in 1904, the Territorial Supreme Court voided that effort on procedural grounds. The Legislature’s second attempt in 1905, “The County Act” (Act 39,) was successful, though it required an override of a veto by the Territorial Governor.  (Konishi)

The City and County of Honolulu consists of the island of Oʻahu, all other islands not included in any other county and adjacent waters thereto. (Legislative Reference Bureau)  Essentially, this means the City and County of Honolulu (“Honolulu”) covers all of Oʻahu (and its surrounding islets) plus the Northwestern Hawaiian Islands (except Midway.)

As an example of the expansive size of the archipelago, if you put the Big Island on Washington DC, Kure Atoll would be in Bismarck North Dakota.  San Francisco to New York is 2,800 to 2,900 miles; the entire Hawaiʻi chain stretches over 1,500 miles – more than halfway across the continent.  (Much of that is “Honolulu.”)

While Hawaiʻi is the world’s most-isolated, populated-place, we are about: 2,500-miles from the US mainland, Samoa & Alaska; 4,000-miles from Tokyo, New Zealand & Guam, and 5,000-miles from Australia, the Philippines & Korea.  We sometimes overlook the size of our largest City, Honolulu.

There are some things that get in the way of determining the actual “area” of Honolulu.  In part, there is disagreement on the status of the archipelagic waters (and whether it is appropriate to include these in the “area” of Honolulu) – especially in the marine expanse between Kure and Kauaʻi.

The international community has recognized the special links between coastal peoples and their adjacent waters repeatedly, and the 200-nautical-mile exclusive economic zone and the expanded 12-nautical-mile territorial sea are premised upon these links.  (Van Dyke)

Some have suggested the linkage of “historic waters” (in and around the islands, including the connecting channels in between.) The linkages are clearer within the Main Hawaiian Islands, maybe not so much to the northwest.  If not in overall area (land and connecting water,) Honolulu is clearly the largest city in expanse from Kure to Oʻahu.

© 2022 Hoʻokuleana LLC

by Peter T Young Leave a Comment

Hawaiian Woods – Hawaiian Royal Residences

Most houses at the time of Cook’s contact consisted of a framework of posts, poles and slender rods – often set on a paving or low platform foundation – lashed together with a coarse twine made of beaten and twisted bark, vines, or grassy fibers.  This was then covered with ti, pandanus or sugarcane leaves, or a thatch of pili grass or other appropriate material.

When covered with small bundles of grass laid side by side in overlapping tiers, these structures were described as resembling haystacks.  One door and frequently an additional small “air hole” provided ventilation and light, while air also passed through the thatching.  Grass or palm leaves covered the raised earth floors of these houses.

When a chief needed a house, his retainers assembled the materials and erected the structure under the direction of an individual (kahuna) expert in the art of erecting a framework and applying thatch.

Many of these more modern royal residences were named – some were named after the material they were made from.  Here are three such royal residences.

Hale Kauila (Downtown Honolulu – Queen Kīna‘u)

Hale Kauila (house built of kauila wood) once stood on the street in downtown Honolulu that still bears the name of this large council chamber or reception room (some refer to it as Kina‘u’s house.)

While the thatch is attached in the usual way, the posts are much higher than usual and have squared timber; but the most foreign touch, apart from the windows, are the cross braces at the top and between the posts and the plate (they were never used in genuine native work.)

The description by Captain du Petit-Thouars of this house (which he calls the house of the Queen Kīna‘u:) “This house, built in wood and covered with dry grasses, is placed in the middle of a fortification closed with a fence.”

“The platform on which it rests is high above the ground in the yard about 30 centimeters and it is surrounded, externally, a covered gallery which makes it more pleasant.”

“Its shape inside, is that of a rectangle lengthens; in one end, there is a flat shape by a wooden partition which does not rise to the roof.”

“This piece serves as a bedroom, in the remaining of the area, box, and at the other end, there is a portion of the high ground from 28 to 30 centimeters, which is covered with several mats: it is this kind of big couch that was placed the ladies and they are held lying on one side or stomach, or they stand to receive and to make room.”

Hale Lama (Waikīkī – King Kamehameha V)

King Kamehameha V’s Waikīkī home was built in 1866.  It was called Hale Lama.  As described by George Kanahele, the residence “was quite modest with only one bedroom, but was notable for its neo-Hawaiian architecture – a low, rectangular-shaped structure, with a high-pitched, hipped roof that was thatched and descended to the poles of the lanai that sounded three of the four exterior walls.”

“The design suited Waikiki’s climate perfectly.  The high pitched roof allowed for the upward expansion of warm air, thus cooling the inside of the house, and the wide overhanging eaves kept out both sun and rain, while inviting the serenity and beauty of the natural setting.”

“It has been mentioned that the lama wood was especially used for building houses of the gods, that is, the thatched houses within the enclosures of the heiau or luakini, and its use in building the house for King lot, Kamehameha V, gave an excuse for its reported use by an old kahuna in the King’s establishment, for a house of prayer, and I am assured by an old resident that prayers to the gods were frequently offered therein”.

After the Kamehameha V’s death in 1872, the house and property went to went to Princess Ruth who bequeathed the property to Princess Bernice Pauahi Bishop.  The Princess and her husband Charles Bishop renovated and enlarged the house with servant quarters.

Hale Kamani (Lāhainā – Princess Nahiʻenaʻena)

When Keōpūolani returned to Maui to live her final years, she had a house on the beach in Lāhainā; her daughter, Nahiʻenaʻena, lived in her own home next door – Nahiʻenaʻena called her house Hale Kamani.

It had an early and convenient addition to the common grass house in a land where the people lived so generally in the open air, was the lanai, with extensions of the rafters at the same or a slightly reduced slope.

This verandah was, generally speaking, the most comfortable part of the house.  This lanai was often detached as in the Hale Kamani and was sometimes large with walls of coconut leaves intertwined, and a nearly flat roof of similar substance which was intended to furnish shade rather than shelter from heavy rain.

At least one other Royal Residence was named after a native wood ‘Āinahau (Princess Kapi‘olani’s home in Waikīkī;) however, it was named such because it was situated in a hau grove, not that its wood was used in the structure.

© 2022 Hoʻokuleana LLC

by Peter T Young 1 Comment

Hālawa Shaft

The Hawaiian Islands are made up of one or more shield volcanoes that are composed primarily of extremely permeable, thin basaltic lava flows (within the flows are a few ash beds.)  Ordinarily, basalts are among the most permeable rocks on earth.

When rain falls on the Islands, it does one of three things: (1) wets the land surface, shallow infiltration saturates the uppermost soil layer and replaces soil moisture used by plants and then is absorbed by the vegetation and/or evaporates (evapotranspiration;) (2) runs off, eroding the land, forming valleys and gouges in the mountain slopes (and also creates some spectacular periodic waterfalls;) or (3) percolates into the ground (slowly sinks into the ground and becomes groundwater.)

The latter contributes to the groundwater recharge of the area (in the Koʻolau, it takes about 9-months for the rain, now groundwater, to seep down through cracks and permeable materials in the mountain.) Other recharge components include cloud drip (moisture condenses on the trees and leaves as clouds/fog drift through) and irrigation of an area helps add to the recharge.

Rainfall percolating through the ground may accumulate in three principal types of groundwater bodies: (1) high-level bodies perched on relatively impervious soil, ash or lava layers; (2) high-level bodies impounded within compartments formed by impermeable dikes that have intruded the lava flows; and (3) basal water bodies floating on and displacing salt water.

The principal source of fresh ground water in the Hawaiian Islands is the roughly lens-shaped basal water body floating on and displacing denser sea water.  (It varies by area, sometimes there is high-level confined water.)  Recharge of the basal water body results directly from percolating rain water or by underground leakage from perched-water bodies and bodies impounded by dikes.

The Ghyben-Herzberg principle applies to this basal water that suggests the top of fresh water above sea level should be balanced by a thickness of fresh water below sea level about 40 times as great.  That generally means, for every foot of fresh water above sea level, there is 40-feet of fresh water below it.)

Water resources were becoming a challenge in the growing Honolulu community. “From the outset it was the Board’s major problem to supply the City of Honolulu with water from sources within its own boundaries as long as that remained possible.”

“The Board’s long range plan, however, contemplated the eventual necessity of going outside the boundaries of the District of Honolulu for additional artesian water but it had been thought that the time when this would have to be done was far in the future. However, when the emergency arose it was possible to advance this phase of the program by deferring the infiltration projects.”

“Bond moneys that would have been applied to infiltration were transferred to a new project through which additional artesian water will be brought into the city from a 284-foot inclined shaft and electrically-operated underground pumping station in North Hālawa Valley.”

“War has delayed the completion of the North Hālawa project and has greatly increased its cost. Army and Navy authorities have given us splendid cooperation on this project, and, although we cannot be certain how soon all the materials and equipment required for completion of the installation will reach us, progress on its construction has been satisfactory, and it should be completed within the year 1943.”  (Report of the Board of Water Supply, Ohrt’s Report, January 28, 1943)

North Hālawa Valley overlies the Pearl Harbor aquifer, an important source of potable water for the island of Oʻahu. Freshwater in the Pearl Harbor aquifer is part of a large, lens-shaped body of ground water that is thickest in the central part of Oahu and thins toward the coastline.

This lens of freshwater, known as the ‘basal lens,’ floats on saltwater that penetrates from the ocean into the basalt flows of which the island is composed.  (Izuka, USGS)

In some early installations, vertical wells were drilled in the tunnels to develop additional water.  Hālawa was different; it is referred to as a skimming tunnel.  It’s commonly called the Hālawa Shaft.

Skimming tunnels consist essentially of a vertical or inclined shaft constructed from the ground surface down to about the water table and one or more horizontal, or nearly horizontal, tunnels constructed laterally at, or just below, the water level to collect water.  (Peterson)

The fundamental advantage of the skimming tunnels over conventional wells is their capability to produce large quantities of fresh water from lenses so thin that drilled wells would recover only brackish water.

For this reason, skimming tunnels are especially useful in some of the dry leeward coastal areas of Hawaiʻi, as well as on many small oceanic islands with extremely thin fresh-water lenses.

Owing primarily to economic considerations and also to the greater flexibility of modern deep-well pumping stations, no new major skimming tunnels have been constructed in Hawaiʻi since the early 1950s. (Peterson)

The Hālawa Shaft facility is at an elevation of 165 feet above sea level; it’s one of five main shafts operated by the Honolulu Board of Water Supply. (The other main shafts include Wai’alae, Kalihi, Makaha and Pearl City.)

Approximately 15-million gallons of pure water is pumped every day from the Hālawa shaft by three pumping units which have a capacity of 18 to 20-million gallons per day.

The water pool is a ‘hole’ at the top of a 919-foot long water development tunnel below. The Hālawa Shaft was put in operation on August 22, 1944.  (Papacostas)

The completion of the Hālawa Shaft made possible the importation of water from the Pearl Harbor area to Honolulu permitting a reduction in draft from the Honolulu aquifer.

This change in draft has raised the water levels in Honolulu to the extent that this aquifer now appears to be functioning well within the limits of its safe yield. (Ground Water Development, 1958)

While I was at DLNR, I had the opportunity to have a private tour of the Hālawa Shaft.  The lack of a key to unlock a gate on the stairs leading down the shaft caused quite an embarrassment to the Water staff.

Rather than turn back, we climbed over the gate and were able to view the shaft and water pool.  

© 2022 Hoʻokuleana LLC