Images of Old Hawaiʻi

by Peter T Young Leave a Comment

Kohala Field System

Throughout the younger islands of the Hawaiian archipelago, dryland agricultural field systems constituted a significant component of the late prehistoric subsistence economy.
 
The field systems produced large quantities of food to support local farmers and residents, as well as local and district-level chiefly elites.
 
It is generally thought that the dryland agricultural systems had spread to their maximum extent, nearly reaching the edge of productive lands.
 
Kohala supported a large and well-developed field system, covering over 15,000-acres with a dense network of field walls and paved trails.  It is one of the largest archaeological sites in Polynesia.
 
In the Kohala area, Hawaiian farmers found, farmed and intensified production on lands that were poised between being too wet and too dry.
 
The distribution of intensive rain-fed agricultural systems was constrained on its lower end by conditions that were too arid to support intensive agriculture reliably, while at their upper margin many millennia of leaching had depleted soil fertility to a point where intensive rain-fed agriculture was infeasible.
 
In essence, Hawaiians were farming the rock in intensive dryland agricultural systems; their field systems extended to the wettest point that still supplied nutrients via basalt weathering.
 
When the field system is plotted against the rainfall map it falls within the 30-70-in rainfall band.
 
Archaeological evidence of intensive cultivation of sweet potato and other dryland crops is extensive, including walls, terraces, mounds and other features.
 
The fields throughout the Kohala system were oriented parallel to the elevation contours and the walls (and perhaps kō (sugar cane) planted on them) would have functioned as windbreaks from the trade winds which sweep down the slopes of the Kohala mountains.
 
Configured in this way, the walls would also have reduced evapotranspiration and – with heavy mulching – retained essential moisture for the crops.  This alignment of fields also conserved water by retaining and dispersing surface run-off and inhibited wind erosion and soil creep.
 
The main development of the Kohala field system took place AD 1450-1800.  By the late-1600s the lateral expansion of the field system had been reached, and by AD 1800 the system was highly intensified.
 
The process of intensification involved shortened fallow periods, and agricultural plots divided into successively smaller units.
 
The archaeological map of the Kohala field system depicts over 5,400-segments of rock alignments and walls with a total length of nearly 500-miles.
 
The fields begin near the north tip of the island very close to the coast.  The western margin extends southward at an increasing distance from the coast, with the eastern margin at a higher elevation and also an increasing distance from the coast.
 
From north to south the field system is more than 12-miles in length.  At its maximum, it is more than 2.5-miles in width.
 
Scientists speculate that this farming did not just support the local population, but was also used by Kamehameha to feed the thousands of warriors under his command in his conquest of uniting the islands under a single rule in the late-1700s.
 
Based on experimental plantings, if only half of the Kohala Field System was in production in one year, it could be producing between 20,000 to 120,000-tons of sweet potato in one crop.
 
The system was abandoned shortly after European contact in the early- or mid-19th century.
 
The image shows remnants of the Kohala Field System walls in present pastureland.  A special thanks to Peter Vitousek, former Hawai‘i resident and now Professor at Stanford, for background information and images. 
 
 
 

by Peter T Young 1 Comment

Kōloa Heritage Trail

The Kōloa District is the name of a modern political-judicial district encompassing the south shore of Kauai.
 
In ancient times, the Kōloa District was part of a larger district called Kona.  The Kōloa Heritage Trail travels through four ahupuaʻa. From east to west, they are: Māhāʻulepu, Paʻa, Weliweli and Kōloa.
 
Poʻipū is part of the Kōloa ahupua’a.  One meaning of the name Poʻipū is crashing, as in waves crashing.
 
The Kōloa Heritage Trail is a 10-mile walk, bike ride or drive which includes 14 stops and monuments describing the significance of the location.
 
1. Spouting Horn Park
Spouting Horn Park was called puhi, or blowhole, by early Hawaiians.  Legends tell of a huge mo‘o, or lizard, caught in this puhi, which was formed when waves eroded softer, underlying rock and wore through the harder top rock.  Water rushing into the hole is forced through the narrow opening and shoots skyward.
 
2. Prince Kūhiō Birthplace & Park
Prince Jonah Kūhiō Kalaniana‘ole was born in Kōloa in a grass hut near this beach to Princess Kinoike Kekaulike and High Chief David Kahalepouli Pi‘ikoi.  He became a delegate to U.S. Congress after Hawai`i became a Territory in 1900, serving for 19 years.  He worked tirelessly on behalf of the Hawaiian people.
 
3. Hanakaʻape Bay & Kōloa Landing
Once, Kōloa Landing was the third largest whaling port in all of Hawai`i and the only port of entry for foreign goods.  The Sugar industry increased its use until 1912, when better facilities became available elsewhere.  Goods and people were transferred by hand and small boat to ships in Hanaka‘ape Bay.
 
4. Pa‘u a Laka – Moir Gardens
What began as a hobby garden by the Kōloa Plantation Manager’s wife became celebrated as one of the world’s best of its kind.  Numerous cactus planted in the 1930s thrived in the arid, rocky soil here.  Many escaped to surrounding areas to become naturalized over time.  You’ll also find water lily-filled lava rock ponds, koi and a variety of orchid and cactus species.
 
5. Kihahouna Heiau
The walled heiau (temple) that once stood here was 130 feet by 90 feet; dedicated to Kane, a major god of Hawaii; Hulukoki, a bird god; and Ku-hai-moana and Ka-moho-alii, two shark gods.  Three hala-lihilihi-ula trees situated on the outside of the naupaka hedge mark the heiau perimeter.
 
6. Po‘ipū Beach Park
Abundant, easy-to-view marine life in calm waters is a major attraction at Po‘ipū Beach.  The endangered native Hawaiian Monk seal and threatened Green sea turtle are frequent visitors.  From November through May, the endangered Humpback whale appears.  Ancient Hawaiians fished and played here and harvested salt in dug-out evaporating pans nearby.
 
7. Keoneloa Bay
Between 200 and 600 A.D., early visitors arrived at Keoneloa Bay, meaning long sand, likely from the Marquesas Islands.  They used the area as a temporary fishing camp, leaving behind stone-age tools, remnants of heiau, or temples, and ahu, or altars.  They prayed to Kane‘aukai, an important fishing god.
 
8. Makawehi & Pa‘a Dunes
The lithified sand dunes of Makawehi, calm face, and Pa‘a, hard rock, yield fossilized plant roots, bird bones, crab claws and other treasures.  Prior to extensive wave erosion, this prominent limestone ridge extended across Keoneloa Bay.  During March through November, water birds visit and sea birds nest and roost in the dunes.
 
9. Pu‘uwanawana Volcanic Cone
More than 5 million years ago, a hotspot in the earth spewed lava upward to form the volcanic mountain island of Kaua‘i. Nearby Ha‘upu Ridge and Mountain contain some of the oldest geologic formations.  Look for the youngest volcanic cones such as Pu‘uwanawana, within view.  Weathered volcanic material produced rich agricultural plains.
 
 10. Hapa Road (Hapa Trail)
Lava rock walls near Hapa Road signify Hawaiian habitation ca. 1200 AD, while the road dates to the late 1800s.  Nearby tracks once held trains hauling cane to Kōloa Plantation for milling.  Hapa Road served as a supply and emergency evacuation route during World War II, and at various times a foot- and bicycle path.
 
 11. Kōloa Jodo Mission
Buddhist temples provided Japanese immigrants a place to worship, study their language, learn martial arts and participate in social events.  This Jodo Mission used a specialist in temple architecture from Japan to build the large temple’s interior.  Hand-painted, wooden ceiling tiles were a gift from the Japanese artist who rendered them.
 
12. Sugar Monument
Ancient Polynesians were the first to bring sugar cane to Hawai’i.  Starting with its first cane seeding in 1835, Kōloa Plantation was the first in Hawai’i to successfully mill cane commercially for export.  It set the precedent for free housing and medical benefits for its immigrant employees from China, Japan, East and West Germany, Portugal and the Philippines.
 
13. Yamamoto Store & Kōloa Hotel
Built at the turn of the 20th century, The Yamamoto Building functioned at various times as a plantation camp store and general store with service station.  Behind it, the Kōloa Hotel offered rooms to traveling salesmen and actors.  The o-furo, or hot tub, provided a relaxing soak to guests.
 
14. Kōloa Missionary Church
Kōloa Missionary Church sanctuary is part of a homestead once owned by Dr. James W. Smith, a medical missionary.  In 1842, he began a practice of over 40 years, later becoming an ordained minister at The Church at Kōloa.  His grandson, Dr. Alfred Herbert Waterhouse, added a clinic to the homestead in 1933.
 
The Poʻipū Beach Resort Association and its Po‘ipū Beach Foundation are the major sponsors of the trail map and brochures.
 
All of these sites are Points of Interest in the Holo Holo Kōloa Scenic Byway; we worked with the Kōloa and Poʻipū communities and prepared the Corridor Management Plan for their Scenic Byway.
 
 

by Peter T Young Leave a Comment

Currents

Historically the world was thought of having 4 oceans the Pacific, Atlantic, Indian and Arctic. Today we have five oceans (adding the Southern (around Antarctica)) covering over 71 percent of the earth’s surface and over 97 percent of the earth’s water. (National Geographic)

The term ‘Seven Seas’ has referred to bodies of water along trade routes, regional bodies of water, or exotic and far-away bodies of water.

In Greek literature (which is where the phrase entered Western literature), the Seven Seas were the Aegean, Adriatic, Mediterranean, Black, Red and Caspian seas, with the Persian Gulf thrown in as a “sea.”

In Medieval European literature, the phrase referred to the North Sea, Baltic, Atlantic, Mediterranean, Black, Red and Arabian seas.

As trade picked up across the Atlantic, the concept of the Seven Seas changed again. Mariners then referred to the Seven Seas as the Arctic, the Atlantic, the Indian, the Pacific, the Mediterranean, the Caribbean and the Gulf of Mexico.

Not many people use this phrase today, but you could say that the modern Seven Seas include the Arctic, North Atlantic, South Atlantic, North Pacific, South Pacific, Indian and Southern Oceans.  (NOAA)

Oceans have currents, the continuous, predictable, directional movement of seawater driven by gravity, wind and water density. Ocean water moves in two directions: horizontally and vertically. Horizontal movements are referred to as currents, while vertical changes are called upwellings or downwellings. (National Geographic)

Ocean currents exist both on and below the surface. Some currents are local to specific areas, while others are global. And they move a lot of water. The largest current in the world, the Antarctic Circumpolar Current, is estimated to be 100 times larger than all the water flowing in all the world’s rivers.

A characteristic surface speed is about 2 to 20 inches per second. Currents generally diminish in intensity with increasing depth.

Vertical movements exhibit much lower speeds, amounting to only a few meters per month. As seawater is nearly incompressible, vertical movements are associated with regions of convergence and divergence in the horizontal flow patterns. (Britannica)

All of this moving water helps more stationary species get the food and nutrients they need. Instead of going looking for food, these creatures wait for the currents to bring a fresh supply to them.

Currents also play a major role in reproduction. The currents spread larvae and other reproductive cells. Without currents many of the ocean’s ecosystems would collapse. (Ocean Blue Project)

Ocean surface currents tend to form ring-like circulation systems called gyres. A gyre is a circular ocean current formed by a combination of the prevailing winds, the rotation of the Earth, and landmasses.

Continents interfere with the movement of both surface winds and currents. Gyres form in both the northern and southern hemispheres.

Gyres in the Northern Hemisphere travel in clockwise directions while gyres in the Southern Hemisphere travel in counter-clockwise directions. It takes about 54 months for water to travel the circuit of the North Pacific gyre, while only 14 months in the North Atlantic gyre.

In the Northern Hemisphere near the equator, trade winds drive currents westward, forming a North Equatorial Current (NE), which moves at about 1 m/sec. At the western boundary of an ocean basin, the water turns and flows towards the North Pole, forming the western-ocean boundary currents.

Western boundary currents are very strong. Two examples are the Gulf Stream (GS) that runs in the Atlantic ocean basin and the Kuroshio Current in the Pacific ocean basin.

They are narrower, but deeper and swifter, than the other currents in the gyre. For example, speeds of 2 m/sec have been measured in the Gulf Stream. These currents, as deep as 1 km, generally remain in deeper water beyond the continental shelf. Western-ocean boundary currents carry warm water from the equator north.

The broad, gentle pitch of the continental shelf gives way to the relatively steep continental slope. The more gradual transition to the abyssal plain is a sediment-filled region called the continental rise. The continental shelf, slope, and rise are collectively called the continental margin. (Britannica)

Eventually, the western boundary currents fall under the influence of the westerly winds and begin flowing to the east, forming the North Atlantic Current (NA) and North Pacific Current (NP).

When they approach the eastern-ocean boundaries of continents, they turn and flow south, forming the eastern-ocean boundary currents. Eastern-ocean boundary currents are shallower and slower than western-ocean boundary currents.

Current flow over the continental shelves (the edge of a continent that lies under the ocean), close to shore, carrying colder waters from the north to the south. Two examples are the California Current (Cal) in the Pacific Ocean basin and the Canary Current (Can) in the Atlantic Ocean basin.

One major current, the equatorial Countercurrent (EC), appears to be an exception to the circulation pattern set up by the gyres. This countercurrent forms just north of the equator in the region between the north equatorial current and the south equatorial current and flows in the opposite direction.  (Hawaii-edu)

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by Peter T Young Leave a Comment

The Feast

271 hogs, 482 large calabashes of poi, 602 chickens, 3 whole oxen, 2 barrels salt pork, 2 barrels biscuit, 3,125 salt fish, 1,820 fresh fish, 12 barrels luau and cabbages, 4 barrels onions, 80 bunches bananas, 55 pineapples, 10 barrels potatoes, 55 ducks, 82 turkeys, 2,245 coconuts, 4,000 heads of taro, 180 squid, oranges, limes, grapes and various fruits.

But we are already getting ahead of ourselves, let’s look back.

On April 25, 1825, Richard Charlton arrived in the Islands to serve as the first British consul. A former sea captain and trader, he was already familiar with the islands of the Pacific and had promoted them in England for their commercial potential (he worked for the East India Company in the Pacific as early as 1821.)

Charlton had been in London during Kamehameha II’s visit in 1824 and secured an introduction to the king and his entourage.  By the time he arrived in Hawai‘i in 1825, instructions had already arrived from Kamehameha II that Charlton was to be allowed to build a house, or houses, any place he wished and should be made comfortable.  This apparently was due to favors Charlton had done for the royal party.  (Hawaiʻi State Archives)

In 1840, Charlton made a claim for several parcels of land in Honolulu. To substantiate his claim, Charlton produced a 299-year lease for the land in question, granted by Kalanimōku.  There was no disagreement over the parcel, Wailele, on which Charlton lived, but the adjoining parcel he claimed, Pūlaholaho, had been occupied since 1826 by retainers and heirs of Kaʻahumanu.

In rejecting Charlton’s claim, Kamehameha III cited the fact that Kalanimōku did not have the authority to grant the lease.  At the time the lease was made, Kaʻahumanu was Kuhina Nui, and only she and the king could make such grants.  The land was Kaʻahumanu’s in the first place, and Kalanimōku certainly could not give it away.  (Hawaiʻi State Archives)  The dispute dragged on for years.

This, and other grievances purported by Charlton and the British community in Hawai‘i, led to the landing of George Paulet on February 11, 1843 “for the purpose of affording protection to British subjects, as likewise to support the position of Her Britannic Majesty’s representative here”.

On February 25, the King acceded to his demands and noted, “In consequence of the difficulties in which we find ourselves involved, and our opinion of the impossibility of complying with the demands in the manner in which they are made … “

“… we do hereby cede the group of islands known as the Hawaiian (or Sandwich) Islands, unto the Right Honorable Lord George Paulet … the said cession being made with the reservation that it is subject to any arrangement that may have been entered into by the Representatives appointed by us to treat with the Government of Her Britannic Majesty…”

Under the terms of the new government the King and his advisers continued to administer the affairs of the Hawaiian population.  For business dealing with foreigners, a commission was created, consisting of the King (or his representative,) Paulet and two officers from Paulet’s ship.  Judd served as the representative of the King.  (Daws)

On April 1, 1843, Lord Aberdeen, on behalf of Her Britannic Majesty Queen Victoria, assured the Hawaiian delegation that: “Her Majesty’s Government was willing and had determined to recognize the independence of the Sandwich Islands under their present sovereign.”

On November 28, 1843, the British and French Governments united in a joint declaration and entered into a formal agreement recognizing Hawaiian independence (Lord Aberdeen signed on behalf of Britain, French ambassador Louis Saint-Aulaire signed on behalf of France.)

After five months of British rule, Queen Victoria, on learning the injustice done, immediately sent Rear Admiral Richard Darton Thomas to the islands to restore sovereignty to its rightful rulers. On July 31, 1843 the Hawaiian flag was raised.  The ceremony was held in area known as Kulaokahuʻa; the site of the ceremony was turned into a park Thomas Square.  After five-months of occupation, the Hawaiian Kingdom was restored.

July 31, 1843 is now referred to as Ka La Hoʻihoʻi Ea, Sovereignty Restoration Day, and it is celebrated each year in the approximate site of the 1843 ceremonies.  The plot of land on which the ceremonies took place was known as Thomas Square. Kamehameha III later officially gave this name to the area and dedicated it as a public park.

“In the afternoon Kamehameha III went in a solemn procession with his chiefs to Kawaiahaʻo Church … A ten-day celebration of Restoration Day followed, and was annually observed. The last of the Restoration Day celebrations came in 1847.”  A thousand special riders, five abreast … were followed by 2,500 regular horsemen …” (Helena G Allen)

As the procession crossed Beretania street on Nuʻuanu royal salutes were fired from the fort and the king’s yacht, the Kamehameha III. They were headed to Kaniakapūpū, Kamehameha III’s summer home.  (Thrum)

Kaniakapūpū (translated roughly as “sound (or song) of the land shells” sits on land in the Luakaha area of Nuʻuanu Valley.  The structure at Kaniakapūpū (modeled on an Irish stone cottage) was completed in 1845 and is reportedly built on top or in the vicinity of an ancient heiau.  It was a simple cottage, a square with four straight walls.

The royal party reached the picnic grounds at about 11 o’clock in a pouring rain; in fact it rained in occasional showers throughout the day … A man stationed at the first bridge for the express purpose, counted 4,000 horses going up the valley and 4,600 returning-visitors from Koʻolau making the difference in numbers.  (Thrum)

Before dinner, which was set for 2 pm, the guests were entertained with some of the ancient games – a mock fight with spears ; the lua, hand to hand combat, and the hakoko, or wrestling match.

The dinner – the feeding of the immense crowd of men, women and children – was a sight to be remembered. Henry St John, the king’s steward, had the care of this department, and he well understood his business.

For the foreign guests, who were not supposed to squat on the mats with natives, tables were provided in the cottage, where was an abundant supply of food cooked in foreign style, but the multitude were fed in the long lanais, at the far end of which was seated the royal party, the ministers and chiefs.

First there was singing of hymns by a choir of native school children, led by Messrs. Marshall and Frank Johnson, to airs that sounded sweetly to New England ears. Grace before meat was solemnly said by John Ii, and then, on a signal from the king, the assembly went vigorously to work on the immense stores of food before them.

While the feast was going on, several old women in the immediate neighborhood of where the king sat, kept up a constant chanting of metes – native poems – in his honor and that of his ancestors, accompanying the chant with gyrations and motions of the arms. And in the evening, after the most of the company had departed, a company of hula girls gave a “concert” with their attendant drum and calabash beaters.  (Thrum)

In the evening there were religious services at Kawaiahaʻo church, which was filled to overflowing, the king and queen being present. A sermon apropos of the occasion was preached by Rev. Richard Armstrong, the text being taken from Psalms 37, 3 – ‘Trust in the Lord and do good; so shalt thou dwell in the land, and verily thou shalt be fed.’ There could have been no question but that his hearers had been fed on that day.  (Lots here from Thrum)

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by Peter T Young Leave a Comment

‘From the Countries whence originate the winds’

The first declaration of the creation of a law-making body in Hawai‘i is contained in a proclamation by King Kamehameha III dated October 7, 1829.

It named the King and regent and ten chiefs as entitled to sit in Council. This council was the forerunner of the legislature proper. Previous to its establishment the laws were mostly customary, many having their origin in the edicts of Ali‘i. (Lydecker)

On October 7, 1829, King Kamehameha III issued a Proclamation “respecting the treatment of Foreigners within his Territories.” It was prepared in the name of the King and the Chiefs in Council: Kauikeaouli, the King; Gov. Boki; Kaahumanu; Gov. Adams Kuakini; Manuia; Kekūanāoʻa; Hinau; ʻAikanaka; Paki; Kīnaʻu; John ‘Īʻi and James Kahuhu.

In part, he stated, “If any man shall transgress any of these Laws, he is liable to the penalty, – the same for every Foreigner and for the People of these Islands: whoever shall violate these Laws shall be punished.”

It continues with, “This is our communication to you all, ye parents from the Countries whence originate the winds; have compassion on a Nation of little Children, very small and young, who are yet in mental darkness; and help us to do right and follow with us, that which will be for the best good of this our Country.”

In Hiram Bingham’s book, Twenty-one Years in the Sandwich Islands, Bingham added a footnote addressing the “Countries whence originate the winds,” saying, “This passage … evidently solicits wise and mature counsels from men of countries to the north-east, whence come the trade winds, or figuratively whence come their frequent commotions, after the adoption of the Christian religion.”

“It was the thought of Kaahumanu, and widely different from what might once have issued from her insulted majesty. Her forbearance was very great towards foreigners and especially those employed by high powers.” (Bingham)

We tend to identify the people from the “Countries whence originate the winds” as the foreigners, more commonly referenced as haole.  Most Hawaiian dictionaries define haole as foreigners; some also suggest (such as Malo) that haole refers to white people.

But according to the Hawaiian law, the status of haole can change – from haole to kanaka maoli.

In 1846 the native Hawaiian government under Kamehameha III made the intentions clear: “Section III. All persons born within the jurisdiction of this kingdom, whether of alien foreigners, of naturalized or of native parents, and all persons born abroad of a parent native of this kingdom, and afterwards coming to reside in this, shall be deemed to owe native allegiance to His Majesty.  (1846 Statute Laws of His Majesty Kamehameha III,  Article I, Chapter V, Section III)

The law allowed to naturalization, “Section X. Any alien foreigner …  may, after a residence of one year in this kingdom, apply to his excellency the governor of the island of Oahu, at Honolulu, for permission to become naturalized …”  (1846 Statute Laws of His Majesty Kamehameha III,  Article I, Chapter V, Section X)

The Law goes on to state, “Section XIII. Every foreigner so naturalized, shall be deemed to all intents and purposes, a native of the Hawaiian Islands – be amenable only to the laws of this kingdom, and to the authority and control thereof – be entitled to the protection of said laws … .” (1846 Statute Laws of His Majesty Kamehameha III,  Article I, Chapter V, Section XIII)

Words matter … and the words are clear; a closer look at the wording of the 1846 law (the Hawaiian text and subsequent translation of that text) clearly state that a haole (foreigner) can become kanaka maoli (a native of Hawai‘i).  Following is the operative line in the law and then its translation,

“E manaoia kela haole keia haole hoohiki pela, ua lilo oia ma ke ano pili i na hana a pau, i kanaka maoli o Hawaii nei”.

“Every foreigner [haole] so naturalized, shall be deemed to all intents and purposes, a native of the Hawaiian Islands [kanaka maoli o Hawaii nei]”.

The above statement in the 1846 Statute Laws of His Majesty Kamehameha III, Chapter V, Article I, Section XIII was carried into the 1859 Civil Code: “428. The Minister of the Interior, with the approval of the King, shall have the superintendence and direction of the naturalization of foreigners.”  (1859 Civil Code, Title 2, Article VIII, Section 428)

“Section 432. Every foreigner so naturalized, shall be deemed to all intents and purposes a native of the Hawaiian Islands … and to the authority and control thereof, be entitled to the protection of said laws, and be no longer amenable to his native sovereign while residing in this Kingdom, nor entitled to resort to his native country for protection or intervention.”

“He shall be amenable, for every such resort, to the pains and penalties annexed to rebellion by the Criminal Code. And every foreigner so naturalized, shall be entitled to all the rights, privileges and immunities of an Hawaiian subject.”  (1859 Civil Code, Title 2, Article VIII, Section 432)

A Hawaiian citizen or subject is someone that has the political status of being a Hawaiian national. And it’s not limited to the native race or the aboriginal blood. (Keanu Sai)

If annexation did not happen, today descendants of Hawaiʻi-born or foreign-born naturalized Hawaiian citizens (with no proof of later naturalization to another nation) are still Hawaiian subjects, as their predecessors were in the Kingdom era. (Keanu Sai)

‘Nationality’ means the legal bond between a person and a State and does not indicate the person’s ethnic origin. Everyone has the right to a nationality. (European Convention on Nationality)

At one time, jus sanguinis (right of blood) was the sole means of determining nationality in Asia and Europe (where it is still widespread in Central and Eastern Europe.) An individual belonged to a family, a tribe or a people, not to a territory. It was a basic tenet of Roman law.

Jus soli (right of the soil,) also known as birthright citizenship, is a right by which nationality or citizenship can be recognized to any individual born in the territory of the related state.

At times, exceptions limit citizenship, typically when a child was born to a parent in the diplomatic or consular service of another state, on a mission to the state in question or a child born to enemy forces engaged in hostile occupation of the country’s territory.

One of the earliest laws in Hawaiʻi dealt with citizenship; it was part of King Kamehameha III’s Statute Laws 1845-1846. The Chapter for that law was titled: “Of Subjects and Foreigners” and the specific Article was labeled “Aliens, Denizens and Natives.”

Section III of that law noted: “All persons born within the jurisdiction of this kingdom, whether of alien foreigners, of naturalized or of native parents, and all persons born abroad of a parent native of this kingdom, and afterwards coming to reside in this, shall be deemed to owe native allegiance to His Majesty. All such persons shall be amenable to the laws of this kingdom as native subjects.”

All persons born abroad of foreign parents, shall, unless duly naturalized, be deemed aliens, and treated as such, pursuant to the laws. (Ka Huli Ao Digital Archives – Punawaiola-org)

Hawaiʻi followed the Anglo-American common law rule of “jus soli;” those born in the country and subject to its jurisdiction are citizens. Subsequent interpretation of the laws and practices affirmed who were Hawaiian citizens and what rights and obligations they possessed.

In 1850, HW Whitney, born in Hawaiʻi of foreign parents, asked the Minister of the Interior, John Young II, about his status. The question was referred to Asher B Bates, legal adviser to the Government, who replied that …

“not only the Hawaiian Statutes but the Law of Nations, grant to an individual born under the Sovereignty of this Kingdom, an inalienable right, to all of the rights and privileges of a subject.” (Hanifin)

In 1856, the Kingdom’s Supreme Court decided Naone v. Thurston, recognizing that persons born in Hawaiʻi of foreign parents were Hawaiian subjects.

On January 21, 1868, the Minister of the Interior for the Hawaiian Kingdom, Ferdinand Hutchison, stated the criteria for Hawaiian nationality:

“In the judgment of His Majesty’s Government, no one acquires citizenship in this Kingdom unless he is born here, or born abroad of Hawaiian parents (either native or naturalized,) during their temporary absence from the kingdom, or unless having been the subject of another power, he becomes a subject of this kingdom by taking the oath of allegiance.”

Subsequent laws through the Republic, Territory and State provide that “All persons born or naturalized in the Hawaiian Islands, and subject to the jurisdiction of the Republic, are citizens thereof.”

A lot of haole (foreigners) were born in the Islands or became naturalized citizens, or are descendants of such. By laws and practice, they, too, are Hawaiian citizens … history and the laws related to Hawaiian citizen status are clear and unambiguous.

In 1893, all Hawaiian citizens lost their nation … Hawaiian citizens with varying ethnicities. As noted by Keanu Sai, “Hawai‘i was a country of laws and nationality and not necessarily a specific race.”

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