Built in About an Hour

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

The younger volcanic craters are all less than 500,000 years old. They formed after Oʻahu had moved well off the hot spot and the main shield volcanoes had gone dormant for at least two-million years.

Scientists say Lēʻahi (Diamond Head) (one of these later eruptions) is a tuff cone, formed by hydromagmatic activity.  Tuff is a volcanic rock made up of a mixture of volcanic rock and mineral fragments. Wherever there are explosive volcanic eruptions you can expect to find tuff.  (SOEST)

A hundred years ago, Hawaiʻi missionary Reverend Sereno Bishop noted Diamond Head was made in less than an hour’s time and is “composed not of lava, like the main mountain mass inland, but of this soft brown rock called tuff.” (Bishop, Commercial Advertiser, July 15, 1901)

Others noted, “the duration of eruption of Diamond Head was of the order of five hours. The eruption may have been intermittent with interruptions sufficient to extend the whole period of activity to as much as five days, but probably not more.”    (Wentworth, Bishop Museum, 1926)

“Volcanic eruptions may be distinguished into two classes, the effusive and the explosive. In the former the molten rock is poured out and covers the mountain slopes with great floods.”

“If you look up at the sides of yonder ravines (on the Koʻolau mountains,) which the rainstorms of many hundred thousands of years have worn out of the original dome-shaped mountain, you will see the back edges of the ancient lava streams lying in layers.”

“The tuff cones are entirely different, and are produced by very brief and sudden explosive eruptions.  The tuff was violently shot high aloft into the air in the form of superheated mud. This hot mud cooled and thickened by the expansion of its water and its partial escape as steam before reaching the ground.”

“It hardened and cemented as it fell, though still liquid enough to form in thin layers or laminations as we see it lying around us at the base of the hill. … The tuff-fountain escaping from its confinement, at once expanded and spread out like a vast tree.”

“Here at Diamond Head, which is one mile in diameter, the bulk of the mud spread out half a mile in all directions before ending its fall. Thus a very exact circular ring was piled up of one mile in diameter. There was, however, another influence, that of a violent easterly-wind which deflected the entire fountain westward”.

“The wind also acted with especial force upon the highest part of the fountain, flinging and piling it up on the western side of the crater in a lofty cone. A large part of that cone has been weathered away by the impact of rainstorms upon the soft rock; but it still stands in a peak some 200 feet higher than the main run.”

“The vent or point of issue of the tuff-fountain must have been at the lowest point of the interior, where lies the present pond of water.”  (Bishop, Commercial Advertiser, July 15, 1901)  (The same series of eruptions produced Punchbowl and Koko Head Crater.)

Somewhat more than half of the craters of southeast Oahu are arranged in linear groups, those dominated by the craters Tantalus, Diamond Head, and Koko Crater.  In the Diamond Head group is the main Diamond Head vent, Kaimuki crater and Mauʻumae crater.

(A cinder cone is a volcanic cone built almost entirely of loose volcanic fragments called cinders or pumice that accumulate around and downwind from a vent.)

(Cinders are glassy and contain numerous gas bubbles "frozen" into place as magma exploded into the air and then cooled quickly.)  (USGS)

The image shows a 1928 aerial of Lēʻahi, Diamond Head.   In addition, I have added others similar images in a folder of like name in the Photos section on my Facebook and Google+ pages.

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Kauaʻi

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

Geologically, Kauaʻi 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, Kauaʻi’s isolation from the other islands kept it safe from outside invasion and unwarranted conflict.

Kauaʻi 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 Kauaʻi 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 Kauaʻi.

Though comprising only 547-square miles, Kauaʻi 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 Kauaʻi 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, Kauaʻi.

“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,) Molokaʻi, Lānaʻi and Kahoʻolawe, ruled by Kahekili; (3) Oʻahu, under the rule of Kahahana; and at (4) Kauaʻi and Niʻihau, Kamakahelei was ruler.

Kamakahelei was the "queen of Kauaʻi 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 Kaua‘i 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 Kaua‘i.  King Kamehameha I launched his first invasion attempt on Kaua‘i 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.

Kaua‘i’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 Kaua‘i and Ni‘ihau.)  Kamehameha’s two attempts at invading Kauaʻi 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 Kaua‘i 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 Kaua‘i.

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 Kaua‘i.

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 Kauaʻi, 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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It's Raining ... Inside

The Koʻolaupoko moku (district) encompasses lands from Kualoa Point to Makapuʻu Point. Encompassing 43,598-acres (68-square miles,) Koʻolaupoko makes up approximately 11-percent of Oʻahu's land mass.

The Koʻolau Mountain Range forms the inland (mauka) boundary of the district. The ridge elevation generally ranges from 2,500 to 2,800-feet; Kōnāhuanui, the tallest peak on the Koʻolau Mountain Range (3,150-feet) is found in Koʻolaupoko. (BWS)

Koʻolaupoko is the remnant of the Koʻolau volcano. Eruptions forming the mountains occurred approximately 2-million years ago and left lava flows that layered over each other.  Magma pouring out of fissures in the volcano solidified in the narrow cracks; the rock that is created is much denser and much less permeable than the surrounding porous lava flows.

These dense, usually vertical geological structures are known as volcanic dikes. These dikes form wall-like areas that can capture and contain water.

Trade winds, which blow over the Pacific from the northeast across the Hawaiian Islands, bring large quantities of moist air to the Koʻolau Range. When these winds are deflected up and over the range, the water vapor condenses into clouds and falls as rain.

The rainfall does one of three things: (1) it runs off, eroding the land, forming valleys and gouges in the mountain slopes (and also creates some spectacular periodic waterfalls;) (2) 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;) or (3) it percolates into the ground (slowly sinks into the ground and becomes groundwater.)

For the latter, it takes about 9-months for the rain, now groundwater, to seep down through cracks and permeable materials in the mountain; much of the groundwater ends up contained in dikes inside the mountain.

As these dike compartments become filled with water and overflow the dike edges, sometimes the water emerges at the surface as springs or streams.

Dike water is good for drinking water.

Development of dike-impounded reservoirs for domestic water offers two basic benefits: (1) the water level is typically high (limiting pumping (as in energy to pump water up wells) and allowing gravity to distribute to the needs at lower elevations) and (2)  the reservoirs are isolated from saline water.

Groundwater impounded by dikes in the Koʻolau Range is a major source of water for the island of Oʻahu, and many tunnels have been bored into the range to develop it. (USGS)

The typical sequence of excavation of a high-altitude tunnel starts with the removal of a zone of weathered rocks, either by tunneling or trenching and is followed by penetration of dike intrusions in the basalt rock.

As tunneling advances farther and farther through the dikes and basalts, the contained dike water leaks and water flow increases, often in instantaneous jumps when key restraining dikes are punctured, until either a single dike, or a series of them, releases such a large volume of stored water that excavation must be halted.  (Mink; USGS)

When a tunnel is bored into a dike-water reservoir, if allowed to flow freely, it will drain water out of storage. Over the course of water exploration in this area, several dikes were struck.

The reduction of dike-confined groundwater storage caused by construction of eight tunnels in Oʻahu has been estimated at 25,800-Million gallons, equivalent, then, to the total ground-water withdrawal on Oʻahu for about 60 days.   (USGS)

Little consideration was given to the storage potential of dike compartments tapped and dewatered by water-development tunnels until a bulkhead was placed in a Waikāne tunnel of the Waiāhole system in 1934 to stop the draining and allow the dike to refill with water (about 40 years after high-altitude water-development tunnels were first constructed in Hawaiʻi.)

The bulkhead at Waikāne held back some water in storage, but not in sufficient volume to be considered successful. Use of the Waikāne bulkhead was discontinued, but other attempts at bulkheading were tried elsewhere, also without much success.

That changed on February 8, 1955.  A 12-foot dike 1,600 feet into the Waiheʻe tunnel was penetrated and water gushed out at an initial rate of about 2.5-mgd (million gallons per day.)   A bulkhead was built to contain the water.

The bulkhead held and the concept of inducing and controlling storage was resoundingly proved with the placement of the bulkhead in Waiheʻe tunnel.  The storage above the tunnel in Waiheʻe Valley has been estimated at 2,200-Million gallons.  (Mink; USGS)

In Koʻolaupoko, fresh water comes entirely from precipitation along the Koʻolau Mountain Range; Waiheʻe provides much of the drinking water to Windward Oʻahu, from Kahaluʻu to Kailua.

The Honolulu Board of Water Supply recently drilled an inclined well to tap dike-impounded water. This technique permitted the development of dike impounded water without the large initial and uncontrollable waste of stored water common to prior development by tunneling.

Dike tunnel systems are also at Waimānalo, Luluku, Haiku, Kahaluʻu, Pālolo, Mānoa and two Waianae tunnels, as well as in the Kohala region of the island of Hawaiʻi and in West Maui.

Oh, It’s Raining … Inside (?)

While the bulkhead holds the dike water, along the Waiheʻe tunnel into the Koʻolau, whatever the weather outside, rainwater (now groundwater) that missed the dike continues to make its downward percolation through the mountain, through cracks in the ceiling … producing a constant ‘rainfall’ for all in the darkness of the tunnel to the Waiheʻe bulkhead.

The image shows it “raining” underground in the Waiheʻe Tunnel (hawaii-edu.) In addition, I have added other related images in a folder of like name in the Photos section on my Facebook and Google+ pages.

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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.

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Keʻanae Prison Camp

In June, 1925, Governor Wallace Farrington and the County Board of Supervisors Chairman Samuel Kalama led a grand procession of cars on the official opening of the road from Kailua to Hana.

The road was called the Belt Road and would link the isolated communities of East Maui with the rest of the island. By December, 1926, the governor and the board chairman were able to drive all the way to Hana on the dream road that was fast becoming a reality.

Wait ... Let’s step back a bit.

Handy, Handy & Pukui report that in ancient times there were several major population centers on the Island of Maui: Kahakuloa (West Maui) region; the deep watered valleys of Nā Wai ‘Ehā (Waiheʻe, Wai‘ehu, Wailuku and Waikapū;) the ‘Olowalu to Honokōhau region of Lāhainā; the Kula - ʻUlupalakua region and the Koʻolau - Hāna region.

They note the importance of the Koʻolau region in this discussion:
“On the northeast flank of the great volcanic dome of Haleakala…the two adjacent areas of Keʻanae 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 Hāna…” (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.

Handy, Handy and Pukui further note 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)

In modern times, when Hāna was without a road, and the coastal steamer arrived on a weekly schedule, Hana-bound travelers unwilling to wait for the boat drove their car to the road's end at Kailua, rode horseback to Kaumahina ridge, then walked down the switchback into Honomanu Valley. (Wenkam, NPS)

Friends carried them on flatbed taro trucks across the Keʻanae peninsula to Wailua cove. It was a short ride by outrigger canoe beyond Wailua to Nāhiku landing where they could borrow a car for the rest of the involved trip to Hana. Sometimes the itinerary could be completed in a day. Bad weather could make it last a week.  (Wenkam, NPS)

It was not until 1847, that the historic and modified trail and road alignments became a part of a system of “roads” called the “Alanui Aupuni” or Government Roads. Work on the roads was funded in part by government appropriations, and through the labor or financial contributions of area residents, or prisoners working off penalties.  (Maly)

The law (Sec 1536DD. Warden, Deputy, Duties, Powers) allowed a warden to have "the immediate charge and direction of all Territorial prisons and prison camps and the administration thereof. The warden shall be responsible for the safekeeping of all prisoners and persons who may be committed to said prisons and for the enforcement of proper order and discipline among and concerning prisoners and prison officers and employees."  (Attorney General)

Neighbor Island prison camps were set up, there were 4: Maui had three, the other was on the Big Island (outside Hilo.) Keʻanae camp had 22-prisoners and 3-guards; Olinda camp had 31-prisoners, with Jailer and 3-guards and Paukakulo camp had 27-prisoners, with 1-jailer and 3-guards. The three camps on Maui are engaged in road work and forest lines.

A large part of the road to Hāna was constructed by prison labor based at the Keʻanae Prison Camp. The camp was built in 1926 to house the prisoners who would construct the road, including several bridges from Kailua to Hana. When the road was completed in 1927, men from Keʻanae to Hāna town were hired to maintain the road, especially during the rainy season.  (McGregor)

Later, an announcement in the Maui News (January 20, 1934) carried the headline, “Conservation Program Will Be Launched Within Week or 10 Days.”  Sub-headlines were “$421,000 Is Provided” and “…To be Located at Keʻanae’s Old Prison Site.”

No longer needed, the Keʻanae prison camp was converted into quarters for the Civilian Conservation Corps. This federal program, created by President Franklin D. Roosevelt to provide jobs to get the US through the depression, brought in men from other parts of Maui and other islands to plant thousands of eucalyptus and other introduced trees throughout the Hana coast.  (McGregor)

In December 1942, during World War II, Governor Ingram Stainback tried to assist the war effort by sending forty inmates from Oʻahu Prison to the former Keʻanae Prison camp to revive the old Nāhiku rubber plantations in the hope of yielding 20,000 to 50,000-pounds of crude rubber annually. The venture was no more successful than the earlier ones had been.

Eventually, in 1949, the camp was acquired by the YMCA and is still used by the “Y;” part of the land area continues to be used as a roadway base yard.

The image shows Hāna Highway (BlueHawaiiHelicopters.)  In addition I have added other images related to the property in a folder of like name in the Photos section on my Facebook and Google+ pages.

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Ahupuaʻa ‘Anomalies’

Typically, we think of ahupuaʻa in the general context of the modern day watershed – from the mountains to the sea (ridges to reefs,) affording occupants access to the various climatic and resource zones.

Ahupuaʻa served as a means of managing people and taking care of the people who support them, as well as an easy form of collection of tributes by the chiefs.  Ultimately, this helped in preserving resources.

Shaped by island geography, ahupuaʻa varied in shape and size (from as little as 100-acres to more than 100,000-acres.)

Each ahupuaʻa had its own name and boundary lines.  Often the markers were natural features such as a large rock or a line of trees or even the home of a certain bird.  A valley ahupuaʻa usually used its ridges and peaks as boundaries.

In ancient Hawaiian times, relatives and friends exchanged products.  The upland dwellers brought poi, taro and other foods to the shore to give to kinsmen there.  The shore dweller gave fish and other seafood.  Visits were never made empty-handed but always with something from one's home to give.

Ahupuaʻa contained nearly all the resources Hawaiians required for survival.  Fresh water resources were managed carefully for drinking, bathing and irrigation.

A typical ahupuaʻa was a long strip of land, narrow at its mountain summit, becoming wider as it ran down a valley into the sea to the outer edge of the reef.  If there was no reef, then the sea boundary would be one-mile from the shore.

However, there are several ‘anomalies’ to this conventional ahupuaʻa layout.

Some include multiple parts, even skipping over water.  Others do not have contact with the ocean, nor reach a mountain peak.  Another includes portions of a couple of mountains.  Here are some examples (there are others, as well.)

On the island of Hawaiʻi, the ahupuaʻa of Kīʻao in the moku (district) of Kāʻu is land-locked and doesn’t reach the ocean.  (Paman)  In addition, it doesn’t reach a mountain summit.

Also on the Island of Hawaiʻi, the ahupuaʻa of Humuʻula starts at the summit of Mauna Loa, crosses the saddle between the two mountains and skirts along the side of Mauna Kea and eventually runs down to the ocean along the Hāmākua coast.

This traversing along a relatively similar contour on the side of Mauna Kea is unique; in addition, in doing so, it essentially cuts off the numerous ahupuaʻa along the South Hilo, North Hilo and Hāmākua coasts to the Mauna Kea summit.

Interestingly, the entire island of Kahoʻolawe is part of the Honuaʻula moku (district) across the ocean on Maui.  Kahoʻolawe is not its own ahupuaʻa; rather, it is divided into ʻili (smaller land units within ahupua‘a.)

Historically, a “cloud bridge” connected Kahoʻolawe with the slopes of Haleakalā.  The Naulu winds brought the Naulu rains that are associated with Kahoʻolawe (a heavy mist and shower of fine rain that would cover the island.)

Heʻeia on the windward side of Oʻahu runs from the mountains to the sea, but also crosses over a portion of the water in Kāneʻohe Bay and includes a portion of a Mōkapu peninsula across the Bay.

The Waiʻanae ahupuaʻa also has an un-typical shape – it is sometimes referred to in two parts: Waiʻanae Kai, on its western side, runs from the ocean to the Waiʻanae Mountains (like a typical ahupuaʻa – this portion of Waiʻanae runs from the mountain to the sea.)

From there, however, the section referred to as Waiʻanae Uka continues across Oʻahu’s central plain and extends up into the Koʻolau Mountains – extending approximately 15-miles from the Waianae Mountains to the Koʻolau Mountains and ends up overlooking the windward coastline.  (Each section is within the same ahupuaʻa.)

Waimānalo is another Oʻahu ahupuaʻa that is ‘anomalous’ to the ‘ridges to reefs’ characterization of the ‘typical’ ahupuaʻa.

Waimānalo extends from the ridge behind Keolu Hills, around Makapuʻu and ending at Kuliʻouʻou Ridge (Koʻolaupoko Hawaiian Civic Club;) it essentially wraps over the Koʻolau range from the windward coast to the leeward coast Oʻahu.

Waimānalo incorporates what was once the large fishpond of Maunalua, now known as Hawaiʻi Kai. Kamakau notes, “The ahupuaʻa of Waimānalo, including the fishpond at Maunalua and the travelling uhu of Makapuʻu, belonged to Mauimua (First-Maui.)”  (Koʻolaupoko Hawaiian Civic Club)

The image shows a map of the Islands with some of the anomalies to the typical’ ahupuaʻa.  In addition, I have included other related images in a folder of like name in the Photos section on my Facebook and Google+ pages.

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Keʻanae, Maui

“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.

The Land Board 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.

The image shows Keʻanae point.  In addition, I have added other images of Keʻanae in a folder of like name in the Photos section on my Facebook page.

http://www.facebook.com/peter.t.young.hawaii

© 2012 Hoʻokuleana LLC

Kawainui Marsh - Kailua, O‘ahu

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.

The image shows a 1951 aerial photo of the Kailua area, with Kawainui Marsh centered in the image (photo from UH-Mānoa and USGS.)  In addition other images and maps of Kawainui are included in a folder of like name in the Photos section on my Facebook page.

http://www.facebook.com/peter.t.young.hawaii

© 2012 Hoʻokuleana LLC