Images of Old Hawaiʻi

by Peter T Young 3 Comments

Hāmākua Ditch

As a result of the 1902 Arthur S Tuttle report commissioned by the Bishop Estate to study the feasibility of bringing water to the Hāmākua area, two major ditches were proposed – the Upper Ditch and the Lower Ditch.

“The object of the Hawaiian Irrigation Company, Limited, is in brief, the supplying of mountain water, by means of one upper and one lower irrigation canal, from the large watershed and permanent streams of the Kohala mountains, Hawaii …”

“… to the sugar estates in the Hāmākua district, where a large area, which is capable of considerable extension, is now under cultivation.” (Hawaiian Star, July 2, 1910)

The Hawaii Irrigation Company was originally known as the Hāmākua Ditch Company, Ltd., which was incorporated on February 9, 1904. Among the local bond subscribers were FA Schaefer & Co, Honokaa Sugar Co, Pacific Sugar Mill, Allen & Robinson, H Hackfeld, Mr Ahrens and Mr Jorgensen.

Sometime between August 1908 and April 1909, the Hāmākua Ditch Company changed its name to Hawaiian Irrigation Company, Ltd.

“Efforts to obtain water on a large scale for the ‘dry’ Hāmākua section of Hawaii had begun, however, prior to the active association of Mr. McCrosson with the projects. In 1884 Claus Spreckels, WG Irwin, HP Baldwin and others had surveys made and did considerable preliminary work, but the scheme was abandoned owing to the decision of Mr. Baldwin to concentrate his energies and capital upon the island of Maui.”

“In 1892 LA Thurston, then minister of the interior, made an official survey of the country (with a view to devising a scheme for taking water into Hamakua.) These several surveys formed the basis of Mr McCrosson’s later operations and the survey basis of the three great systems as they appear today.” (Hawaiian Star, July 2, 1910)

Water sources for the Upper Hāmākua Ditch were the Kawainui and the Alakahi streams, as well as general runoff from the watershed into the ditch; construction apparently commenced in April 1906. The Ditch was completed in January of 1907 and was initially able to deliver 15 MGD (million gallons per day.)

John T McCrosson oversaw the construction of the ditch. The Upper Ditch was approximately 23-miles in length and some 15 miles of it ran through Honokaa Sugar Co. and Pacific Sugar Mill land. Originally the Upper Ditch consisted of dirt ditches and galvanized flumes patched with lumber.

The Lower Ditch construction began in June 1907 (water sources were the Kawainui, Alakahi, Koeawi, and later, the Waimea streams,) but serious construction work did not start until September 1908. The ditch was opened on July 1, 1910 with a delivery of 30 MGD.

It was the occasion of two days of banquets, speeches and merry-making … “According to rumors aboard the Mauna Kea, the Hamakua Ditch opening on Friday will be the scene of an immense gathering, if the weather be favorable. It is understood that the entire population of the district will foregather there…” (Hawaiian Star, June 30, 1910)

The original length of the Lower Ditch was approximately 24 miles. Later on it was extended about 5 miles to supply water to Pauʻuilo Plantation.

“(F)rom the water head to the exit from Waipio Valley a distance of nearly nine miles, the ‘ditch’ is no ditch at all but a continuous tunnel with only three breaks where it comes out of the face of the bluff to span a narrow gorge and plunge into the face of the opposite precipice once more to bury itself in the lava depths …”

“… and that there are as yet unused possibilities for the incidental development of 8000 horsepower which can be distributed as electric energy all over the Island of Hawaii, give some conception of what the Great Ditch means.” (Hawaiian Gazette, July 5, 1910)

Japanese laborers built the ditch tunnels, the tunnel of the Lower Ditch, traveling the 8.9-miles from the Kawainui intake to the weir at Kukuihaele, was one of the longest in Hawai‘i. It was further distinguished by being quite large, approximately 10 X 12 feet in diameter. In 1920, another tunnel was constructed through Lalakea Gulch.

Apparently, three people were killed as a result of the building of the ditch. In July 1909, an engineer, Thomas F Kelly, drowned (with his horse) in Waipi`o Valley as he was returning from Kukuihaele with supplies.

A month later, a Japanese laborer was “pinned down by a large rock falling on him; he died shortly after the accident.” There is mention of a third, a Japanese workman, who, during the cutting of a trail across the face of the pali, was struck by a falling rock, “and he tumbled to death hundreds of feet below.” (EnvHawaii)

Due to various disputes , by February of 1915, Hawaiian Irrigation Co. was taken over by new management (essentially that of Honokaa Sugar Co.)

The company became involved in the growing and selling of rice. A rice mill was operated and became a source of revenue. There were also a few small independent poi factories located in the valley. The records also reflect other attempts regarding diversified agriculture in the valley.

In 1960, Honokaa Sugar Co. bought the remaining outstanding shares of the Hawaiian Irrigation Company, making Hawaiian Irrigation Company a wholly owned subsidiary of that firm.

For half a century it was the sole source for potable water for the communities along its path. The Hāmākua Ditch is woven into the history and culture of the local communities beyond its length. The ditch continues to serve the needs of the Hāmākua community.

The demise of the sugar industry, including the closure of Hāmākua Sugar in 1994, left a void in communities on the Big Island and throughout the state. At that time, the community expressed a strong desire to retain an agricultural lifestyle, which helped define the character of the community.

A movement toward growing a diversified agricultural community began with an eye on the highly desirable lower elevation lands. The Hāmākua Ditch remained a critical and important piece in this vision.

The Hamakua Ditch Work Group (comprised of local farmers and ranchers, representatives from the Hāmākua Farm Bureau and Hāmākua/North Hilo Cooperative, USDA Natural Resource Conservation Service, State Department of Agriculture, State Legislators and Kamehameha Schools) formed shortly after the 1994 closing of the plantation and has focused on maintenance and preservation of the Hāmākua Ditch system. (Takamine)

“John T McCrosson, the builder of the Hāmākua ditch, was born In Delaware, and arrived in the Islands first in March, 1880, going to Kohala plantation, where he had charge of theo traction engines. Remained there and at other plantations until 1885, when he went to San Francisco and engaged in the machinery business.”

“While at Kohala, Mr McCrosson studied deeply into the water problem of that rich country, and worked out during the years at San Francisco the great systems which are now under way there.”

“He returned to the Islands in 1895 and, with the exception of business visits to Washington, London, and other cities, has been here ever since. The Kohala ditch was the first planned and carried out by Mr. McCrosson.”

“This was completed June 11, 1906, and was the occasion of a monster ‘celebration’ in which almost the whole Island of Hawaii joined.” (Hawaiian Star, July 2, 1910) (Lots of information here is from HSPA, EnvHawaii and Takamine.)

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by Peter T Young Leave a Comment

Kaluaikonahale

He was born about 1789 with the name Kaluaikonahale, the son of Keʻeaumoku and his wife Nāmāhana. He was the youngest of four famous siblings.

His sisters were Queen Kaʻahumanu, Kamehameha’s favorite wife who later became the powerful Queen Regent and Kuhina nui, Kalākua Kaheiheimālie and Namahana-o-Piʻia (also queens of Kamehameha) and brother George Cox Kahekili Keʻeaumoku.

His father, Keʻeaumoku, was a “tried friend of Kamehameha and one of the principal promoters of his fortunes. Being of prodigious personal strength, his valor powerfully assisted Kamehameha in securing the entire dominion of the group.” (Polynesian, January 4, 1845)

Kaluaikonahale was born on Maui, but as an infant he was taken to Keauhou to grow up; he excelled in canoeing and other sports. In his youth, he once jumped a stone wall and injured his foot; he almost died from the injury, but recovered and remained lame for the rest of his life. (Oaks)

He married Analeʻa (Ane or Annie) Keohokālole; they had no children. (She later married Caesar Kapaʻakea. That union produced several children (including the future King Kalākaua and Queen Liliʻuokalani.))

He later married Lydia Haʻaheo Kaniu. They had one son Keōua, who died in infancy, and one daughter Kamanele (1814–1834.)

With the introduction of Christianity and adoption of western names, he changed his name and chose the name John Adams after John Quincy Adams (the US President at the time.)

From then, he was called John Adams Kuakini.

His physical appearance was formidable; standing 6-feet, 3-inches “and even heavier than this gigantic stature would indicate.” Ellis noted he was “tall, stout, well made and remarkably handsome.” (Oaks)

His wife “was like himself, a royal chief of highest rank, and not quite equally ponderous. I remember seeing the princely pair lolling on their own pile of rich Niʻihau mats, with many attendants busily kneading their bodies and limbs (lomi-lomi). Ages of nourishing diet and massage for digestion had bred a royal Hawaiian race of immense stature and girth.” (Bishop)

Kuakini was an important adviser to Kamehameha I in the early stages of the Kingdom of Hawai‘i. His “first office of importance under Kamehameha I was that of captain of the ordnance at Oʻahu. Upon the King’s last return to Hawaiʻi in 1813, he was raised to the rank of counselor.”

“Immediately after the death of the King, Kaʻahumanu made him Governor of Hawaii; his original charge was limited to the district of Kona. In 1830, she further appointed him to the governorship of Oahu, which office he retained until December, 1831, when he returned to Hawaiʻi.”

“(Kuakini’s) administrations were vigorous and effective. Energetic in action, but reserved in manners, he assumed to himself much responsibility. It was difficult to secure his confidence in matters of council, as he relied much upon his own judgment.”

“While in Hawaiʻi, being remote from the seat of government and the influence of other chiefs mostly assembled around the King, he acted in a great measure independently of them, and sometimes contrary to their opinions.”

“His acquaintance with the English language, and his thirst for knowledge, gave him a superiority in general intelligence, over most of the chiefs of his rank; and afforded him a better insight into the nature of things than others attained.”

“He was more enterprising in deed than other native rulers, and many of the objects which claimed his attention, such for instance as the building of churches and the making of roads, were intended for the public benefit”.

“(Y)et in most of his enterprises, his aim was to accumulate property. But he was correct in his business transactions and a man of his word.” (Polynesian, January 4, 1845)

“By sea and by land we have enjoyed the protection of God, and the countenance and patronage of the king and chiefs. Especially would we notice the kindness of Kuakini, the Governor of Owhyhee (Hawaiʻi,) who received us with great hospitality, and freely lent his influence and authority to aid us in the attainment of our immediate objects”.

“… with a view to the permanent establishment of a missionary station there, (Kuakini) has promptly commenced the erection of a chapel at Kairua for the worship of Jehovah, whose rightful and supreme authority he has publicly acknowledged.” (Ellis)

Kuakini gave land to missionary Asa Thurston to build Mokuʻaikaua Church. “This was erected by Governor Kuakini about 1828. It was a wholly native structure, framed with immense timbers cut and dragged from the great interior forest by Kuakini superintending his subjects in person.” (Bishop)

“(I)n 1835, the great church was burned by some incendiary, and the services were then conducted in a large canoe-shed of the Governor, which was vacated for the purpose.”

“The energetic Kuakini immediately set about building the great stone church now standing on the site of the old one. … the corners were built up with large square blocks of pāhoehoe lava, which were transported by the people from some heiau at a distance. They were smoothly hewn, evidently with great labor. (Bishop)

During his tenure, Kuakini built other historical sites that dominate Kailua-Kona today. The Great Wall of Kuakini, probably a major enhancement of an earlier wall, was one of these.

The Great Wall of Kuakini extends in a north-south direction for approximately 6 miles from Kailua to near Keauhou, and is generally 4 to 6-feet high and 4-feet wide.

He built Huliheʻe Palace in the American style out of native lava, coral lime mortar, koa and ‘ʻōhiʻa timbers. Completed in 1838, he used the palace to entertain visiting Americans and Europeans with great feasts.

The Palace was constructed by foreign seamen using lava rock, coral, koa and ʻōhiʻa timbers. Kuakini oversaw the construction of both Mokuʻaikaua Church and Huliheʻe Palace and these landmarks once shared a similar architectural style with exposed stone.

Kuakini died December 9, 1844 in Kailua-Kona; the Palace passed to his adopted son, William Pitt Leleiōhoku. Leleiōhoku died a few months later, leaving Huliheʻe to his wife, Princess Ruth Luka Keʻelikōlani. It became a favorite retreat for members of the Hawaiian royal family.

A highway is named “Kuakini Highway,” which runs from the Hawaii Belt Road through the town of Kailua-Kona, to the Old Kona Airport Recreation Area. He is also the namesake of Kuakini Street in Honolulu, which is in turn the namesake of the Kuakini Medical Center on it.

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by Peter T Young Leave a Comment

Kaʻawaloa

Kealakekua translates as ‘pathway of the gods’ and is one of the most significant historic and cultural places in Hawaiʻi.

Kealakekua Bay State Historical Park is comprised of portions of the Kealakekua and Kaʻawaloa ahupuaʻa, which surround Kealakekua Bay. From Kaʻawaloa south to Palemano Point, the bay measures about one and one-half miles in length and about one mile in width.

“The Sandy beech forms the West side, behind which is a grove of Coco nut trees & a pond of indifferent water; on the N side of this beach lies a Village, & the Well we waterd at, which is close to the Sea & under the high hill.”

“At the other end of the beach is the Morai, or Oheekeeow (heiau of Hikiau.) A field of Taboo’d ground seperates the Morai from a Village to the s, or rather a continued range of Stragling houses in that direction.” (King; Maly)

Kealakekua was selected by the aliʻi as one of the seven royal centers of Kona in the 1700s, because of its sheltered bay and abundance of natural resources.

Kaʻawaloa, meaning ‘ the distant ʻawa plant’, is a flat, fan-shaped lava peninsula near sea level, which rises gradually to the edge of the 600-ft Pali Kapu O Keoua. These forty acres of land define the northwest side of Kealakekua Bay.

Historically, Kaʻawaloa was the royal burial grounds of Hawaiʻi’s rulers and their families, including Kalaniopuʻu, the ruling chief in power when Captain Cook sailed into Kealakekua Bay.

The British ships, Discovery and Resolution, under the command of Captain James Cook, sailed into Kealakekua Bay on January 17, 1779; Cook was killed at Kaʻawaloa on February 14, 1779.

In their journals, Cook’s crew recorded four “villages” of about 80 houses each along the shoreline around Kealakekua Bay. Settlements lined the bay in the pre-contact period, as do the small residential communities of Nāpōʻopoʻo and Keʻei, today.

“The Towns of the Natives are built along the Sea side. At Cari’ca’coo’ah (Kealakekua) Bay there were three, one (Kealakekua-Nāpoʻopoʻo) on the SE-tern side of the Bay which was very large extending near two miles along the shore, another (Kaʻawaloa) upon the NWtern side which was not so large, and a small Village (Palemano) in the cod or bottom of the Bay.”

“At the back of the villages upon the Brow of the Hill are their plantations of Plantains, Potatoes, Tarrow, Sugar Canes &c, each mans particular property is fenced in with a stone wall; they have a method of making the Sugar Cane grow about the walls so that the stones are not conspicuous at any distance, but the whole has the appearance of fine green fences.” (Clerke; Maly)

“Kaʻawaloa, at the landing-place on the north side of Kealakekua bay, however conveniently accessible to the people of the district, who live much along the shores, was cramped and rocky, being composed almost exclusively of lava.”

“It was hot, dry, and barren, affording neither brook nor well, nor spring of fresh water, nor field, nor garden-spot for plantation, though a few cocoanut trees, so neighborly to the sea, find nourishment there.” (Bingham; Maly)

As the west learned of Hawaiʻi, this area became known as one of the first major shipping and provisioning port for ships involved in exploration, whaling and trans-Pacific trade.

About 40-years after Cook’s visit, the missionaries arrived and established one of the earliest mission stations in Hawai‘i at Kaʻawaloa in 1824.

Access was improved to Kaʻawaloa and Nāpoʻopoʻo with the development of cart roads to transport goods from the bay to upland communities.

By the 1850s, traditional fishing and farming were giving way to ranching and coffee. Cattle were herded down the roads to wharfs at Nāpoʻopoʻo and Kaʻawaloa where they were loaded onto ships in the bay.

Nāpoʻopoʻo Light was established in 1908 at Kaʻawaloa on the north side of Kealakekua Bay (but apparently named for Nāpoʻopoʻo Landing on the south side of the bay.) The 22-foot light tower was built in 1922.

Several families remained at Kaʻawaloa until World War II, but most of the activity had shifted to Nāpoʻopoʻo by that time.

In 1969 the state set aside the entire bay as a marine life conservation district (MLCD.) The MLCD is inshore of a straight line between Kaʻawaloa point and the north end of Nāpōʻopoʻo Beach Park. The cove fronting the Captain Cook Monument is a popular snorkeling area.

On December 12, 1973 the Kaʻawaloa area was designated as the Kealakekua Bay Historical District (a District w/multiple sites) and placed on the National Register of Historic Places.

The obelisk monument commemorating Captain Cook was constructed in 1874, near the spot where Cook died. (Contrary to urban legend, the monument site is not owned by the British Government; ownership is in the name of the British Consul General (the individual) – a representative would check in with DLNR, from time to time.)

While at DLNR, we issued a curator agreement to Hale Mua – The Royal Order of King Kamehameha I to help protect the sites under DLNR’s jurisdiction and to help provide public access.

The photo captures the awa ceremony we participated in to commemorate the signing of the Curator Agreement. (It was a moving experience; I was proud and honored to be there.  Yes, that is me, all by myself (representing the State,) and the descendent families, members of the Order and others on the other side.)

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by Peter T Young 3 Comments

Kazumura Cave

The ʻAilaʻau eruption is considered the longest memorable eruption of Kilauea.

(Before Pele, there was ʻAilaʻau (Ai means the ‘one who eats or devours.’ Laʻau means ‘tree’ or a ‘forest.’) ʻAilaʻau was, therefore, the fire-god devouring forests. When Pele came, she took over as fire goddess, ʻAilaʻau left.) (Westervelt)

The ʻAilaʻau eruption took place from a vent area just east of Kilauea Iki. The eruption built a broad shield. The eastern part of Kilauea Iki Crater slices through part of the shield, and red cinder and lava flows near the center of the shield can be seen on the northeastern wall of the crater.

The eruption probably lasted about 50-years, from about 1420 to 1470 AD. The large volume of lava covered a huge area, about 166 square miles (106,240-acres) – larger than the Island of Lanaʻi (140-square miles.)

Lava covered all, or most, of what are now Mauna Loa Estates, Royal Hawaiian Estates, Hawaiian Orchid Island Estates, Fern Forest Vacation Estates, Eden Rock Estates, Crescent Acres, Hawaiian Acres, Orchid Land Estates, ʻAinaloa, Hawaiian Paradise Park and Hawaiian Beaches.

The pahoehoe flows did leave rather large kipuka south of Keaʻau and in the forest southwest of ʻAinaloa, as well as small kipuka in Hawaiian Paradise Park and elsewhere.

This eruption and lava flow may be described in the Pele-Hiʻiaka chant. Hiʻiaka, late on returning to Kilauea from Kauai with Lohiau, sees that Pele has broken her promise and set afire Hiʻiaka’s treasured ʻohiʻa lehua forest in Puna.

Hiʻiaka is furious, and this leads to her love-making with Lohiau, his subsequent death at the hands of Pele, and Hiʻiaka’s frantic digging to recover the body.

The ʻAilaʻau flows seem to be the most likely candidate to have covered so much of Puna that they were worthy of commemoration in the chant.

The timing seems right, too – after the Pele clan arrived from Kahiki, before the caldera formed (Hiʻiaka’s frantic digging may record this), and before the encounters with Kamapuaʻa, some of which probably deal with explosive eruptions between about 1500 and 1790. (USGS)

Reminders of past eruptions are lava tubes. Lava tubes are natural conduits through which lava travels beneath the surface of a lava flow. Tubes form by the crusting over of lava channels and pāhoehoe flows.

When the supply of lava stops at the end of an eruption or lava is diverted elsewhere, lava in the tube system drains downslope and leaves partially empty conduits beneath the ground. (USGS)

One such, as a result of the ʻAilaʻau eruption, is Kazumura Cave – it has been called the longest (over 40-miles) and (to some) deepest lava tube in the world and the deepest cave in the US. (Cultural Surveys)

According the Hawaiian Government Surveyors in 1891 (related to ‘The New Puna Road:’) “An interesting feature of this locality is the large number of lava caverns and long subterranean passages abounding upon it, especially between the 9th and 11th miles, in fact this whole tract is so thoroughly penetrated by caverns that hollow sounds are often heard beneath ones footsteps when traversing the region.”

“These subterranean passages are generally entered through some opening made by the falling in of the roof and prove to be regular arched ways, ranging as much as 25 feet in width and 15 feet high and extending for long distances.”

“The floors have that corrugated ropy appearance such as are seen on any viscid mass if drawn out as it hardens. The roofs and sides are covered with stalactites, the whole producing a wonderful effect when lit up.”

“These caverns evidently served as burial places in ancient and comparatively modern times in view of the fact that the benches here and there were covered in human remains.” (Cultural Surveys)

“Its average inclination was found to be 1.75 degrees, less in its lower section and considerably more in the upper sections. Passage cross-sections also were found to be different in the different areas.”

“While considerable local variation exists, its lower end tends to be wide and comparatively low while the upper section tends to be high and narrow. Locally, slip slopes and cut banks were found at sharp bends. Lavafalls up to about 15 m are numerous, especially in the upper sections.” (Halliday)

I have asked everyone who I thought should know who Kazumura was (the apparent namesake of the cave/lava tube.) Any insight into who Kazumura was is appreciated.

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by Peter T Young 1 Comment

Kaʻohe

Looking at land divisions on the Island of Hawaiʻi, “the common ahupuaʻa is found to be a strip say 1,000-feet average width, and running from the seashore, not by any means to the top of the mountains, but to the zone of timber land that is generally exists between 1,700 and 5,000-feet line of elevation. The ordinary ahupuaʻa extends from half a mile to a mile into this belt.”

“Then there are the large ahupuaʻa which are wider in the open country than the others, and on entering the woods expand laterally so as to cut off the smaller ones, and extend toward the mountain till they emerge into the open interior country not however to converge to a point at the tops of the respective mountains.”

“Only a rare few reach those elevations, sweeping past the upper ends of all the others, and by virtue of some privilege in bird-catching, or some analogous right, taking the whole mountain to themselves.”

“Thus Mauna Loa is shared by three great lands, Kapapala and Kahuku from Kaʻū, and Humuʻula from Hilo. Possibly Keauhou from Kona may yet be proved to have had a fourth share.”

“The whole main body of Mauna Kea belongs to one land from Hāmākua, viz., Kaʻohe, to whose owners belonged the sole privilege of capturing the ʻuaʻu, a mountain-inhabiting but sea-fishing bird.” (Kaʻohe translates to ‘bamboo;’ the name may relate to a bamboo water carrier.)

“High up on its eastern flank, however, stretched the already mentioned land of Humuʻula, whose upper limits coincide with those of the māmane, a valuable mountain acacia, and which, starting from the shore near Laupāhoehoe, extends across the upper ends of all other Hilo lands to the crater of Mokuʻāweoweo.”

“These same lands generally had the more extended sea privileges. While the smaller ahupuaʻa had to content themselves with the immediate shore fishery extending out not further than a man could touch bottom with his toes …”

“… the larger ones swept around outside of these, taking to themselves the main fisheries much in the same way as that in which the forests were appropriated.”

“Concerning the latter, it should here be remarked that it was by virtue of some valuable product of said forests that the extension of territory took place.”

“For instance, out of a dozen lands, only one possessed the right to kalai waʻa, hew out canoes from the koa forest. Another land embraced the wauke and olona grounds, the former for kapa, the latter for fish line.” (Lyons, The Islands, July 9, 1875)

“From the mass of evidence taken we find that in ancient time the main value of the land of Kaʻohe was the uwaʻo, a sea-bird, whose habitat was the dry, rocky and elevated portion of the mountain.” (Appeal from Boundary Commissioner, May 31, 1892)

Kaʻohe is an irregular ahupua‘a because it only occupies a narrow (and relatively resource-poor) band along the coast where most of the residents would have lived.

But as Kaʻohe ascends the eastern slope of Mauna Kea and emerges above the forest near 6,000-feet in elevation, it expands to occupy the entire summit region. The uplands of Kaʻohe would have contained few food resources beyond ground-nesting birds.

The primary evidence of pre-contact human utilization of Kaʻohe’s vast mountain region is the adze quarry, which would have provided Kaʻohe with a valuable resource to exchange with other ahupua‘a. (Mills)

The adze quarry area was “the largest workshops in the world for making of stone tools.” (Kenneth Emory) It covers an area of roughly 7 ½-square miles on the south slope of Mauna Kea. The main activity was concentrated in a zone that is 1-to-1½ miles wide between the 11,000 and 12,400 ft. elevation.

The landscape is dotted with numerous cinder cones, the principal one of which in the quarry area is Puʻu Koʻokoʻolau. The upper slopes of Mauna Kea have been described as a stony alpine desert. There is little vegetation and the ground surface has the appearance of a desert pavement.

Kaʻohe effectively crosses and includes all regions going from the sea to the summits of Mauna Kea and Mauna Loa. Some of the general regions include (from top to bottom:)

Kuahiwi – the mountain top, which is too high in elevation for heavy vegetation to grow. It has strong winds and extreme climates (sometimes very hot and sometimes very cold.)

Kualono – the region near the mountain top. Likewise, very few plants and animals live here. Māmane and naio (hardwoods) are the only hardy trees to grow at this height.

Waomaʻukele – the region named for the wet, soggy ground. The main trees that live in this area are the koa and ʻōhiʻa. This area was located in the rain belt of the island, especially on the koʻolau side of each island.

Waoakua – the forested region, the realm of the god and where the rain forest begins. This sacred area was kapu to most kānaka.

Waokānaka – where kānaka live and farm the land. Wood was harvested for tools, weapons and canoes; many other useful things for everyday living were gathered here.

Kula – the upland plain or open country. Pili was harvested and used mostly for thatching hale (houses).

Kahakai – the edge of the ocean. Here ʻākulikuli, with succulent green leaves, resists wind and salt water. Its leaves contain a special chemical that acts like a natural steroid.

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