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October 6, 2019 by Peter T Young Leave a Comment

Keʻanae

“Wai o ke ola! Wai, waiwai nui! Wai, nā mea a pau, ka wai, waiwai no kēlā!” (Water is life! Water is of great value! Water, the water is that which is of value for all things!) (Joe Rosa, in Maly)

If you are going to tell a story about Keanae, in Koʻolau on the coast of Maui, the story starts with water, and with it, the life of the land.

From ancient times, the abundant rains, supported the development of rich forests; the rains and forests have in turn led to the formation of hundreds of streams (kahawai) that have molded the landscape of Maui into one with many large valleys (awāwa) and smaller gulches (kahawai). (Maly)

These watered valleys and gulches, and their associated flat lands (kula), have been home to and have sustained native Hawaiian families for centuries.

Handy, Handy & Pukui report that there were several major population centers on the Island of Maui: Kahakuloa (West Maui) region; the deep watered valleys of Nā Wai ‘Ehā (Waihe‘e, Wai‘ehu, Wailuku and Waikapū); the ‘Olowalu to Honokōhau region of Lāhainā; the Kula – ‘Ulupalakua region and the Koʻolau – Hana region.

They note the importance of the Ko‘olau region in this discussion: “On the northeast flank of the great volcanic dome of Haleakala…the two adjacent areas of Ke‘anae and Wailua-nui comprise the fourth of the main Maui centers and the chief center on this rugged eastern coast.”

“It supported intensive and extensive wet-taro cultivation. Further eastward and southward along this windward coast line is the district of Hana… [Handy, Handy and Pukui.]” (Maly)

Settlement in the watered valleys along the Koʻolau coast consisted primarily of permanent residences near the shore and spread along the valley floors. Residences also extended inland on flat lands and plateaus, with temporary shelters in the upper valleys.

Two primary forms of agricultural sites occur in these river valleys: lo‘i kalo (irrigated and drainage taro farming field systems) on the valley floors and slopes; and the kula and kīhāpai dry land farming plots where crops such as ‘uala (sweet potatoes), kō (sugar canes), kalo (taro), mai‘a (bananas and plantains) and wauke (paper mulberry.)

Handy, Handy and Pukui further that “…Ke‘anae lies just beyond Honomanu Valley. This is a unique wet-taro growing ahupua‘a… It was here that the early inhabitants settled, planting upland rain-watered taro far up into the forested area. In the lower part of the valley, which is covered mostly by grass now, an area of irrigated taro was developed on the east side.”

“A much larger area in the remainder of the valley could have been so developed. However, we could find no evidence of terracing there. This probably was due to the fact that the energies of the people were diverted to create the lo‘i complex which now covers the peninsula.” (Maly)

Anciently, the peninsula was barren lava. But a chief, whose name is not remembered, was constantly at war with the people of neighboring Wailua and was determined that he must have more good land under cultivation, more food, and more people.

So he set all his people to work (they were then living within the valley and going down to the peninsula only for fishing,) carrying soil in baskets from the valley down to the lava point. (Maly)

The soil and the banks enclosing the patches were thus, in the course of many years, all transported and packed into place. Thus did the watered flats of Keʻanae originate.

A small lo‘i near the western side of the land formerly belonged to the chief of Keʻanae and has the name Ke-‘anae (the Big Mullet); it is said that the entire locality took its name from this small sacred lo‘i. Here, as at Kahakuloa, the taro that grew in the sacred patch of the aliʻi was reputed to be of great size. (Maly)

This area was nearly completely destroyed by a tsunami in 1946 (April 1.) Reportedly, the only building said to have been left standing was the Lanakila ʻIhiʻihi O Iehova o na Kaua (now called the Keʻanae Congressional Church.)

In 2005, the DOE announced the closure of the last one-room school in the state of Hawaiʻi (in Keʻanae,) just a few weeks before the school year began. The village of Keʻanae had its own school for 96 years.

Since then, Keʻanae students have made the 16-mile, one-way trek to Hana School. Reportedly, a Keʻanae Charter School has been proposed by community members. Last year, the non -profit group Ka Waianu o Hāloa launched a fund-raising effort in support of the establishment of a charter school in Keʻanae.

Today, Keʻanae continues to be a relatively isolated, but significant taro-growing community; it is one of the major commercial wetland taro farming regions in the state.

Keʻanae residents reportedly use the terms “inside” and “outside” to express the difference between life in their rural heartland and the new world of towns and cities where most Hawaiians live today.

Keʻanae lies on the windward coast of Maui, about a two-hour drive over the narrow, winding Hana Highway. Heading toward Hana leads you further to the “inside,” heading towards Kahului is taking you “outside.”

While at DLNR, I was involved through the Land Board and the Water Commission (both of which I chaired) on several issues related to Keʻanae – all focused on historic stream diversions and the impacts to downstream users, particularly the taro farmers there.

We authorized the release of an additional 6-million gallons per day for downstream uses, as well as appointment of a monitor to determine that this amount will meet the needs of the downstream farmers, as well as monitor other aspects of the decision.

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Filed Under: Hawaiian Traditions, Place Names Tagged With: Koolau, Hana, Kalo, Taro, Keanae, Hawaii

May 25, 2019 by Peter T Young Leave a Comment

Kawainui Marsh

Ko‘olau volcano started its life as a seamount above the Hawaiian hotspot around 4-million years ago. It broke sea level some time prior to 2.9-million years ago.

About 2-million years ago, much of the northeast flank of Ko‘olau volcano was sheared off and material was swept more than 140-miles north of O‘ahu and Moloka‘i onto the ocean floor (named the Nu‘uanu Avalanche) – one of the largest landslides on Earth.

Following a period of dormancy, Ko‘olau eruptions about 1-million years ago (known as the Honolulu Volcanic Series) created landmarks such as Diamond Head, Hanauma Bay and Punchbowl Crater. Ko‘olau’s eroded remnants make up the Ko‘olau Mountain Range.

About 6,000 years ago and before the arrival of the Hawaiians, Kawainui (“the large [flow of] fresh water”) and Ka‘elepulu (“the moist blackness”) were bays connected to the ocean and extended a mile inland of the present coastline. This saltwater environment is indicated by inland deposits of sand and coral.

A sand bar began forming across Kawainui Bay around 2,500 years ago creating Kawainui Lagoon filled with coral, fish and shellfish. The Hawaiians probably first settled along the fringes of this lagoon.

Gradually, erosion of the hillsides surrounding Kawainui began to fill in the lagoon with sediments.

About 500 years ago, early Hawaiians maintained the freshwater fishpond in Kawainui; the fishpond was surrounded on all sides by a system of canals (‘auwai) bringing water from Maunawili Stream and springs to walled taro lo‘i.

In 1750, Kailua was the political seat of power for the district of Ko‘olaupoko and a favored place of the O‘ahu chiefs for its abundance of fish and good canoe landings.

Kawainui was once the largest cultivated freshwater fishpond on Oahu. Rimming the wetland are numerous heiau (temples.)

Farmers grew kalo (taro) in the irrigated lo‘i (fields) along the streams from Maunawili and along the edges of the fishponds. Crops of dryland kalo, banana, sweet potato and sugarcane marked the fringes of the marsh. Fishermen harvested fish from the fishponds and the sea.

In the 1880s, Chinese farmers converted the taro fields of Kawainui to rice, but abandoned their farms by 1920. Cattle grazed throughout much of Kawainui.

The marsh drains into the ocean at the north end of Kailua Beach through Kawainui Canal (Oneawa Channel.)

The marsh attracts migratory seabirds and is home to four species of endangered waterbirds: the Hawaiian stilt (aeʻo), the Hawaiian coot (ʻalae keʻokeʻo), the Hawaiian gallinule (ʻalaeʻula) and the Hawaiian duck (kōloa maoli).

In 1979, the US National Registrar for Historic Places issued a “Determination of Eligibility Notification” finding that Kawainui Marsh area is eligible for listing in the National Register for Historic Places.

According to the determination, “Kawainui Marsh is important as a major component of a larger cultural district which would include … the ponding/wet agricultural area … remains of extensive terracing systems, ceremonial sites, burial sites, and habitation areas associated with this agricultural complex”.

In 2005, the Kawainui and Hāmākua Marsh Complex was designated as a Wetlands of International Importance and added to the Ramsar List (Ramsar site no. 1460.)

The Convention on Wetlands (Ramsar, Iran, 1971) – called the “Ramsar Convention” – is an intergovernmental treaty that embodies the commitments of its member countries to maintain the ecological character of their Wetlands of International Importance and to plan for the “wise use”, or sustainable use, of all of the wetlands in their territories.

Kawainui Marsh also functions as a flood storage basin to protect Kailua. As part of flood control measures, the Oneawa Canal and levee started in 1950 and were completed a few years later. When flood waters over-topped the levee and flooded Coconut Grove in the December 31, 1987-January 1, 1988 flood, the levee was raised and floodwall added.

Projects are underway to restore waterbird habitat, as well as care for some of the historic sites. DLNR has plans for visitor center and trails around the wetland – they have been on the books for a long time, it would be nice to see those community visions come to fruition.

Lots of good work is being done by lots of dedicated folks in helping to restore Kawainui Marsh, including ‘Ahahui Mālama I Ka Lōkahi (led by Doc Burrows,) Kailua Hawaiian Civic Club and others.

When I was a kid, we referred to this area as the “swamp” – many of the old maps referred to it as such. Auto parts shops lined the road at its edge; the dump was nearby. Times have changed.

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Filed Under: Hawaiian Traditions, Place Names Tagged With: Hamakua Marsh, Coconut Grove, Oneawa Channel, Hawaii, Kailua, Koolau, Kawainui Marsh

October 28, 2018 by Peter T Young 2 Comments

Koʻolau Volcano

O‘ahu used to be nearly twice as big as it is now. (Thompson) The Island consists of two major shield volcanoes: Waiʻanae and Koʻolau; the eroded remnants of which are the Waiʻanae Range and the Koʻolau Range.

Waiʻanae is the older of the two (breaking the ocean surface ~3.9 to ~2.8 million-years ago) and makes up the western part of O‘ahu. Koʻolau volcano started as a seamount above the Hawaiian hotspot around 4-million years ago. It broke sea level some time prior to 2.9-million years ago.

Koʻolaupoko, one of O‘ahu’s six ancient moku (districts,) is bounded by Kalaeoka‘ō‘io, which is a point near the center of the northeast coast at Kualoa; the crest of the Koʻolau Range to the west; and Makapuʻu Point on the southeastern tip of the island.

This expanse also generally delineates the extent of Koʻolau Volcano – effectively from and including Kāne‘ohe to Kailua to Waimānalo. A significant landslide and ongoing erosion reshaped the volcano.

About 2-million years ago, much of the northeast flank of Koʻolau volcano was sheared off and material was swept onto the ocean floor (named the Nuʻuanu Avalanche) – one of the largest landslides on Earth.

The Pali is the remaining edge of the giant basin, or caldera, formed by the volcano. At its base are the towns of Kāne’ohe, Kailua and Waimānalo – beyond that, open ocean. The other half of the caldera, an area the size of Brooklyn, tore away and tumbled into the ocean. (Sullivan)

Material swept more than 140-miles north of O‘ahu and Molokai. For the last 85-miles of its journey, the avalanche traveled uphill by about 1000 feet, leaving jumbled blocks – once part of O‘ahu – scattered over more than 9,000-square miles of seafloor. (Sinton)

Residual ridges, remnants of the old Koʻolau volcano, extend northeast from the Pali. These include the Mokulua islands, Olomana, Kapaʻa (where the quarry is,) Mahinui (Oneawa, Kalaheo) and Keolu Hills.

Mōkapu Peninsula (where Marine Corps Base Hawai‘i is situated) is evidence of subsequent secondary volcanic eruptions that formed Ulupaʻu Crater (the large hill on the Kailua side of the peninsula,) Pu‘u Hawaiiloa (the central hill that originally had the base control tower, now has radar (‘the hill’,)) Pyramid Rock and the nearby Moku Manu (Bird Island.)

Following a period of dormancy, Koʻolau erupted about 1-million years ago (known as the Honolulu Volcanic Series) and created landmarks such as Lēʻahi (Diamond Head,) Hanauma Bay, Pūowaina (Punchbowl Crater) and Āliapaʻakai (Salt Lake.) Another tuff cone is Mānana Island (Rabbit Island.)

Pounded by the tradewind and rains, the windward side of O‘ahu is more weathered than the leeward areas of the island, and now this vast caldera wall is reduced to a line of sheer cliffs stretching from Makapuʻu to Kualoa and beyond.

The flat valley floors are extensively eroded, and are now mostly joined, studded here and there with isolated remnant peaks and ridges connected to the central range. (Klieger)

Coral reefs and marine terraces were formed at different elevations due to the changing sea levels over time. There are some broad lowland areas in the lower reaches of deeply alluvial valleys. (Moberly)

It was the broadness of this coastal plain (which included swampy areas near the shore) that distinguished Koʻolaupoko from other areas of O‘ahu, and most likely helped account for the intensity and productiveness of agriculture.

The abundant rainfall produces constantly flowing streams that supported the vast expanse of wetland kalo (taro) lo‘i (pondfields) that once extended throughout Koʻolaupoko. (Klieger)

Because Kāne’ohe Bay has a deep lagoon between an outer reef and the shore, the reef is considered by some geologists to be a barrier reef, the only example in Hawaii. Several fishponds lined the bay.

Mokoliʻi (Chinaman’s Hat) and Mokuoloe (Coconut Island) are erosional remnants of the bedrock Koʻolau basalt; Kapapa and Kekepa (Turtleback) Islands are of limestone; and Ahu O Laka Island is a sand bar that is uncovered at low tide. (Moberly)

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Filed Under: General, Place Names Tagged With: Hawaii, Oahu, Koolau, Koolaupoko, Waianae, Nuuanu Avalanche

February 12, 2014 by Peter T Young Leave a Comment

Kauai

Poetically the island is reportedly called, “Manōkalanipō”, or “Kauai a Manō” after the ancient chief who was largely responsible for elevating Kauai’s ancient society to sophisticated heights of advancement and productivity.  (NativeKauai)

Geologically, Kauai is the oldest of the main inhabited islands in the chain. It is also the northwestern-most island, with Oʻahu separated by the Kaʻieʻie Channel, which is about 70-miles long. In centuries past, Kauai’s isolation from the other islands kept it safe from outside invasion and unwarranted conflict.

Kauai was traditionally divided into 5 moku (districts) including: Koʻolau, Haleleʻa, Nā Pali, Kona and Puna. (Common district names that are universally used across of the Hawaiian archipelago include “Koʻolau” marking the windward sides of the islands; “Kona” – the leeward sides of the islands; and “Puna” – indicating regions where springs and fresh water abound.)

The whole of the northwest coast (Napali) show the remains of extensive agricultural work and a fairly extensive population; the Mana region had clusters of house sites in the dry valleys that cut through the cliffs. Nearly all the great river valleys are thoroughly terraced and show evidence of population.

The principal location of the house sites is on the shore line, especially near the mouths of the river valleys where the taro was growing; in the mountains are some house sites and small villages.

The principal cultivated products on Kauai were taro, sweet potatoes, yams and gourds among the vegetables, and banana, breadfruit, coconut palm and paper mulberry among the trees.  (Bennett)

Malo notes that the “cultivation of kula lands is quite different from that of irrigable lands. The farmer merely cleared of weeds as much land as he thought would suffice. If he was to plant taro (upland taro), he dug holes and enriched them with a mulch of kukui leaves, ashes or dirt, after which he planted the taro.”

“In some places they simply planted without mulch or fertilizer … If a field of potatoes was desired, the soil was raised into hills, in which the stems were planted; or the stems might merely be thrust into the ground anyhow, and the hilling done after the plants were grown.”

The boundaries of the five moku on Kauai were changed in the late-1800s to reflect the present day judicial land districts, Kawaihau, Hanalei, Waimea, Kōloa and Līhuʻe.

In 1877, Hanalei and Līhuʻe shared a common boundary.  Kawaihau was set apart by King Kalākaua, who gave that name to the property lying between the Wailua River and Moloaʻa Valley.  A bill was introduced into the legislature and the eastern end of Hanalei District was cut out and Kawaihau became the fifth district on the island of Kauai.

Though comprising only 547-square miles, Kauai is large enough to have figured at all times as a major influence on Hawaiian culture. Together with Niʻihau it forms a group which is considerably isolated from the other Hawaiian islands.  (Bennett)

Fornander notes, “the ruling families of Kauai were the highest tapu chiefs in the group is evident from the avidity with which chiefs and chiefesses of the other islands sought alliance with them. They were always considered as the purest of the “blue blood” of the Hawaiian aristocracy; … But of the exploits and transactions of most of the chiefs who ruled over Kauai during this period, there is little preserved to tell.”

He further notes that during the “nine generations from Laamaikahiki (about the 14th century – he reportedly came from Tahiti,) the island of Niihau bore about the same political relation to the mōʻi (king) of Kauai as the island of Lanai did to the mōʻi of Maui – independent at times, acknowledging his suzerainty at others. … Springing from and intimately connected with the Kauai chiefs, there was a community of interests and a political adhesion which, however strained at times by internal troubles, never made default as against external foe.”

Then things changed for Kauai and the rest of the Islands.  In the dawn hours of January 18, 1778, on his third expedition, British explorer Captain James Cook on the HMS Resolution and Captain Charles Clerke of the HMS Discovery first sighted what Cook named the Sandwich Islands (that were later named the Hawaiian Islands.)  He first landed at Waimea, Kauai.

“The height of the land within, the quantity of clouds which we saw, during the whole time we staid, hanging over it, and frequently on the other parts, seems to put it beyond all doubt, that there is a sufficient supply of water; and that there are some running streams which we did not see, especially in the deep valleys, at the entrance of which the villages commonly stand.”  (James Cook Journal)

“From the wooded part to the sea, the ground is covered with an excellent sort of grass, about two feet high, which grows sometimes in tufts, and though not very thick at the place where we were, seemed capable of being converted into plentiful crops of fine hay. But not even a shrub grows naturally on this extensive space.”  (James Cook Journal)

Throughout their stay the ships were plentifully supplied with fresh provisions which were paid for mainly with iron, much of it in the form of long iron daggers made by the ships’ blacksmiths on the pattern of the wooden pāhoa used by the Hawaiians.  The natives were permitted to watch the ships’ blacksmiths at work and from their observations gained information of practical value about the working of iron. (Kuykendall)

After a month’s stay, Cook got under sail again to resume his exploration of the Northern Pacific. Shortly after leaving Hawaiʻi Island, the foremast of the Resolution broke and the ships returned to Kealakekua Bay for repairs.  On February 14, 1779, at Kealakekua Bay, Cook and some of his men were killed.

At the time of Cook’s arrival, the Hawaiian Islands were divided into four kingdoms: (1) the island of Hawaiʻi under the rule of Kalaniʻōpuʻu, who also had possession of the Hāna district of east Maui; (2) Maui (except the Hāna district,) Molokai, Lanai and Kahoʻolawe, ruled by Kahekili; (3) Oʻahu, under the rule of Kahahana; and at (4) Kauai and Niʻihau, Kamakahelei was ruler.

Kamakahelei was the “queen of Kauai and Niʻihau, and her husband (Kāʻeokūlani (Kāʻeo)) was a younger brother to Kahekili, while she was related to the royal family of Hawaiʻi. Thus, it will be seen, the reigning families of the several islands of the group were all related to each other, as well by marriage as by blood. So had it been for many generations. But their wars with each other were none the less vindictive because of their kinship, or attended with less of barbarity in their hours of triumph.”  (Kalākaua)

Kaumuali‘i was the only son of Kamakahelei and Kāʻeo; he was born in 1778 at Holoholokū, a royal birthing heiau specifically designated for the birth of high ranking children.  Kaumuali‘i became ruling chief of Kauai upon the death of his parents.

In 1784, Kamehameha I began a war of conquest, and, by 1795, with his superior use of modern weapons and western advisors, he subdued all other chiefdoms, with the exception of Kauai.  King Kamehameha I launched his first invasion attempt on Kauai in April of 1796, having already conquered the other Hawaiian Islands, and having fought his last major battle at Nuʻuanu on O‘ahu in 1795.

Kauai’s opposing factions (Kaumuali‘i versus Keawe) were extremely vulnerable as they had been weakened by fighting each other (Keawe died and Kaumuali‘i was, ultimately, ruler of Kauai and Ni‘ihau.)  Kamehameha’s two attempts at invading Kauai were foiled (by storm and sickness.)

The island was never conquered; in the face of the threat of a further invasion, in 1810, at Pākākā on Oʻahu, negotiations between King Kaumuali‘i and Kamehameha I took place and Kaumualiʻi yielded to Kamehameha. The agreement marked the end of war and thoughts of war across the islands.

After King Kamehameha I died in 1819, Kaumuali‘i pledged his allegiance to Liholiho, Kamehameha’s son and successor.    Kaumuali‘i settled in Honolulu and became a husband of Kaʻahumanu, widow of Kamehameha I.

Hiram Bingham was on a preaching tour of the island of Kauai in 1824, shortly before King Kaumuali‘i died.  Kaumuali‘i had been living on Oahu for three years.  Bingham spoke to him just before coming to Kauai.

Bingham writes:
“We found Kaumuali‘i seated at his desk, writing a letter of business.  We were forcible and pleasantly struck with the dignity and gravity, courteousness, freedom and affection with which he rose and gave us his hand, his hearty aloha, and friendly parting smile, so much like a cultivated Christian brother.”

When the king died, Bingham said a gloom fell over Kauai.

Kaumuali‘i was buried at Waine‘e Church (Wai‘ola Church,) on Maui (he wanted to be buried near Keōpūolani, another of Kamehameha’s wives – mother of Liholiho (Kamehameha II) and Kauikeaouli (Kamehameha III.))  (King Kaumuali‘i’s granddaughter Kapiʻolani (1834–1899) married King Kalākaua.)

The image shows a map of the island of Kauai, noting moku (districts) and ahupuaʻa. I added a couple of other images in a folder of like name in the Photos section on my Facebook and Google+ pages.

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Filed Under: Ali'i / Chiefs / Governance, Place Names Tagged With: Koolau, Na Pali, Kaahumanu, Liholiho, Hawaii, Waiola, Kona, Wainee, Kapiolani, Keopuolani, Captain Cook, Kamakahelei, Puna, Kaeo, Kamehameha, Kaumualii, Kauai

January 19, 2014 by Peter T Young Leave a Comment

Moku

Prior to European contact, each of the major islands or independent chiefdoms in the Hawaiian chain comprised a mokupuni (island.) Over the centuries, as the ancient Hawaiian population grew, land use and resource management also evolved.

The traditional land division of pre-contact Hawaiians was based on the sustainability and self-reliance within ahupuaʻa (community watershed areas) as well as within larger regions (moku) and lastly individual sovereign islands (mokupuni.)

The mokupuni were subdivided into land units of varying sizes, and the largest division was the moku (district – literally: interior island,) administered by high-ranking chiefs.

They were either relatives of the high chief of the island, trusted supporters or high ranking individuals who pledged their support to the high chief but were allowed to remain relatively independent.

Each island was divided into several moku or districts, of which there are six in the island of Hawaiʻi, and the same number in Oʻahu. There is a district called Kona on the lee side and one called Koʻolau on the windward side of almost every island.  (Alexander)

It appears that the six districts on the islands of O‘ahu and Hawai‘i, and the system of developing smaller manageable units of land became formalized in the reigns of Māʻilikūkahi and ʻUmi-a-Līloa, respectively (about the time Columbus was sailing across the Atlantic.)

Māʻilikūkahi is noted for clearly marking and reorganizing land division palena (boundaries) on O‘ahu.  Palena, or possibly an evolved term “palena ʻāina” are place boundaries.  (Beamer)

Defined palena brought greater productivity to the lands; lessened conflict and was a means of settling disputes of future aliʻi who would be in control of the bounded lands; protected the commoners from the chiefs; and brought (for the most part) peace and prosperity.

Fornander writes, “He caused the island to be thoroughly surveyed, and boundaries between differing divisions and lands be definitely and permanently marked out, thus obviating future disputes between neighboring chiefs and landholders.”

Kamakau tells a similar story, “When the kingdom passed to Māʻilikūkahi, the land divisions were in a state of confusion; the ahupuaʻa, the ku, the ʻili ʻāina, the moʻo ʻāina, the pauku ʻāina, and the kihapai were not clearly defined.”

“Therefore, Māʻilikūkahi ordered the chiefs, aliʻi, the lesser chiefs, kaukau aliʻi, the warrior chiefs, puʻali aliʻi, and the overseers (luna) to divide all of Oʻahu into moku, ahupuaʻa, ʻili kupono, ʻili ʻāina, and moʻo ʻāina.”

Malo gives a detailed description of the kuleana that a kālaimoku aliʻi who divided lands for Mōʻī had to fulfill:  “There are two important aspects in being a kālaimoku, to take care of the aliʻi, and to take care of the makaʻāinana, for these two reasons the kālaimoku guides the aliʻi at his side, with the careful attention to these two things, things were to be done properly.”  (Malo, Beamer)

What is commonly referred to as the “ahupuaʻa system” is a result of the firm establishment of palena (boundaries.)  This system of land divisions and boundaries enabled a konohiki (land/resource manager) to know the limits and productivity of the resources that they managed.

In the late-1400s, through warfare and alliances with other chiefs, ʻUmi gained control of the entire Island of Hawaiʻi. ʻUmi made himself the aliʻi nui, or high chief, for the whole island.

ʻUmi divided his island into separate moku, or districts. These moku were subdivided into smaller sections called ahupuaʻa.

In the time of ʻUmi, son of the great chief Līloa, the Hawaiian islands were divided into political regions. The four mokupuni (larger islands) of Kauaʻi, Oʻahu, Maui, and Hawaiʻi were divided into moku (districts).

The smaller islands of Molokaʻi, Lānaʻi and Kahoʻolawe became moku of Maui, and Niʻihau a moku of Kauaʻi.

Traditionally, the Island of Kaua‘i was divided into five moku (districts): Haleleʻa, Kona, Koʻolau, Nāpali and Puna. However, after the battle of Wahiawa in 1824, the land of Kaua‘i was redistributed and district boundaries changed. The new district names became: Hanalei, Kawaihau, Līhuʻe, Kōloa and Waimea.  (Cultural Surveys)

For ease in collecting annual tribute, the moku were subdivided into ahupuaʻa, land sections that usually extended from the mountain summits down through fertile valleys to the outer edge of the reef in the sea (or if there was not reef, one-mile from shore.)

The size of the ahupuaʻa depended on the resources of the area with poorer agricultural regions split into larger ahupuaʻa to compensate for the relative lack of natural abundance. Each ahupuaʻa was ruled by an aliʻi or local chief and administered by a konohiki.

These natural land divisions were the result of the flow of water over the land (streams or springs.)

From the earliest days, streams were among the most important natural resources sought after by native Hawaiians. Battles were fought and lives sacrificed for the right to use stream water.

The Hawaiians called freshwater wai, and considered it to be sacred. People using wai from streams took only what was absolutely necessary. They were expected to share the wai with others. This was done without greed or selfishness.

Such practices gave Hawaiians their word for law which is kanawai, or the “equal sharing of water.” Water was so valuable to Hawaiians that they used the word “wai” to indicate wealth. Thus to signify abundance and prosperity, Hawaiians would say waiwai.

In keeping with this concept of wealth being fresh water, the traditional land tenure system in ancient Hawaii had at its very core the presence of streams, or kahawai. Although of many shapes and sizes, each ahupua’a consisted of three area types: mountain, plain and sea.

The image shows the Moku of Oʻahu (ksbe.) In addition, I have added other related images in a folder of like name in the Photos section on my Facebook and Google+ pages.

Follow Peter T Young on Facebook  Moku

Prior to European contact, each of the major islands or independent chiefdoms in the Hawaiian chain comprised a mokupuni (island.) Over the centuries, as the ancient Hawaiian population grew, land use and resource management also evolved.
The traditional land division of pre-contact Hawaiians was based on the sustainability and self-reliance within ahupuaʻa (community watershed areas) as well as within larger regions (moku) and lastly individual sovereign islands (mokupuni.)
The mokupuni were subdivided into land units of varying sizes, and the largest division was the moku (district – literally: interior island,) administered by high-ranking chiefs.
They were either relatives of the high chief of the island, trusted supporters or high ranking individuals who pledged their support to the high chief but were allowed to remain relatively independent.
Each island was divided into several moku or districts, of which there are six in the island of Hawaiʻi, and the same number in Oʻahu. There is a district called Kona on the lee side and one called Koʻolau on the windward side of almost every island.  (Alexander)
It appears that the six districts on the islands of O‘ahu and Hawai‘i, and the system of developing smaller manageable units of land became formalized in the reigns of Māʻilikūkahi and ʻUmi-a-Līloa, respectively (about the time Columbus was sailing across the Atlantic.)
Māʻilikūkahi is noted for clearly marking and reorganizing land division palena (boundaries) on O‘ahu.  Palena, or possibly an evolved term “palena ʻāina” are place boundaries.  (Beamer)
Defined palena brought greater productivity to the lands; lessened conflict and was a means of settling disputes of future aliʻi who would be in control of the bounded lands; protected the commoners from the chiefs; and brought (for the most part) peace and prosperity.
Fornander writes, “He caused the island to be thoroughly surveyed, and boundaries between differing divisions and lands be definitely and permanently marked out, thus obviating future disputes between neighboring chiefs and landholders.”
Kamakau tells a similar story, “When the kingdom passed to Māʻilikūkahi, the land divisions were in a state of confusion; the ahupuaʻa, the ku, the ʻili ʻāina, the moʻo ʻāina, the pauku ʻāina, and the kihapai were not clearly defined.”
“Therefore, Māʻilikūkahi ordered the chiefs, aliʻi, the lesser chiefs, kaukau aliʻi, the warrior chiefs, puʻali aliʻi, and the overseers (luna) to divide all of Oʻahu into moku, ahupuaʻa, ʻili kupono, ʻili ʻāina, and moʻo ʻāina.”
Malo gives a detailed description of the kuleana that a kālaimoku aliʻi who divided lands for Mōʻī had to fulfill:  “There are two important aspects in being a kālaimoku, to take care of the aliʻi, and to take care of the makaʻāinana, for these two reasons the kālaimoku guides the aliʻi at his side, with the careful attention to these two things, things were to be done properly.”  (Malo, Beamer)
What is commonly referred to as the “ahupuaʻa system” is a result of the firm establishment of palena (boundaries.)  This system of land divisions and boundaries enabled a konohiki (land/resource manager) to know the limits and productivity of the resources that they managed.
In the late-1400s, through warfare and alliances with other chiefs, ʻUmi gained control of the entire Island of Hawaiʻi. ʻUmi made himself the aliʻi nui, or high chief, for the whole island.
ʻUmi divided his island into separate moku, or districts. These moku were subdivided into smaller sections called ahupuaʻa.
In the time of ʻUmi, son of the great chief Līloa, the Hawaiian islands were divided into political regions. The four mokupuni (larger islands) of Kauaʻi, Oʻahu, Maui, and Hawaiʻi were divided into moku (districts).
The smaller islands of Molokaʻi, Lānaʻi and Kahoʻolawe became moku of Maui, and Niʻihau a moku of Kauaʻi.
Traditionally, the Island of Kaua‘i was divided into five moku (districts): Haleleʻa, Kona, Koʻolau, Nāpali and Puna. However, after the battle of Wahiawa in 1824, the land of Kaua‘i was redistributed and district boundaries changed. The new district names became: Hanalei, Kawaihau, Līhuʻe, Kōloa and Waimea.  (Cultural Surveys)
For ease in collecting annual tribute, the moku were subdivided into ahupuaʻa, land sections that usually extended from the mountain summits down through fertile valleys to the outer edge of the reef in the sea (or if there was not reef, one-mile from shore.)
The size of the ahupuaʻa depended on the resources of the area with poorer agricultural regions split into larger ahupuaʻa to compensate for the relative lack of natural abundance. Each ahupuaʻa was ruled by an aliʻi or local chief and administered by a konohiki.
These natural land divisions were the result of the flow of water over the land (streams or springs.)
From the earliest days, streams were among the most important natural resources sought after by native Hawaiians. Battles were fought and lives sacrificed for the right to use stream water.
The Hawaiians called freshwater wai, and considered it to be sacred. People using wai from streams took only what was absolutely necessary. They were expected to share the wai with others. This was done without greed or selfishness.
Such practices gave Hawaiians their word for law which is kanawai, or the “equal sharing of water.” Water was so valuable to Hawaiians that they used the word “wai” to indicate wealth. Thus to signify abundance and prosperity, Hawaiians would say waiwai.
In keeping with this concept of wealth being fresh water, the traditional land tenure system in ancient Hawaii had at its very core the presence of streams, or kahawai. Although of many shapes and sizes, each ahupua’a consisted of three area types: mountain, plain and sea.
The image shows the Moku of Oʻahu (ksbe.) In addition, I have added other related images in a folder of like name in the Photos section on my Facebook and Google+ pages.
Follow Peter T Young on Facebook  
Follow Peter T Young on Google+    
© 2014 Hoʻokuleana LLC

Filed Under: Place Names, Hawaiian Traditions Tagged With: Niihau, Hawaii, Mailikukahi, Hawaii Island, Kahoolawe, Oahu, Ahupuaa, Kona, Palena, Molokai, Kanawai, Maui, Moku, Umi-a-Liloa, Kauai, Lanai, Koolau

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