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February 28, 2024 by Peter T Young Leave a Comment

Waiʻaleʻale

“Aloha Waiʻaleʻale
Ka Kuahiwi o Kauai”

“Such is the beginning of the ancient mele which pilgrims were formerly accustomed to sing on reaching the highest peak of the mountain, which is Waiʻaleʻale proper; at its foot lies the fabulous lake from which it takes its name.  “Rippling Water,” the origin of many a wild tale, lay before us; it proved to be a very small pool.”  (Dole, The Garden Island, October 21, 1913)

“As droplets in a cloud approach the mountain, small vertical wind shear constrains their horizontal motion, while upward motion stops at the trade wind inversion or stable layer. Thus entrainment is limited and droplets grow rapidly.  Over the sea and along the coast, drops falling from the cloud usually evaporate.”

“At the mountain face, lifting cools the air. Increased condensation and turbulence accelerate drop growth through collision, as flow becomes constrained between mountain and the trade wind inversion. At the cloud-covered mountaintop, mechanical uplift stops and most of the accumulated moisture precipitates as prolonged light or moderate continuous rain.”  (Ramage)

“Hawaii now claims the wettest spots on earth.  From records covering a long period, Cherrapunji, a village at the elevation of about 4,800 feet in the Khasi hills of India, has established a rainfall average of 426 inches a year …”

“Short period observations show that Mount Waiʻaleʻale, the central peak of the island of Kauai, with a height of 5,080 feet, has a yearly average of 476 inches.  Other parts of Hawaii are scarcely less damp.  Puʻu Kukui, 5,000 feet high on the island of Maui, has had a seven-year average of 396-inches.  (The Times, Arkansas, July 9, 1920)

“You all know, more or less definitely, that there is a swampy region on the top of Waiʻaleʻale – but perhaps you do not realize that this swamp extends from Waiʻaleʻale clear back to Nāpali district, comprising a great table land of some 30 or 35 square miles, lying at an elevation varying from 4,000 to 5,000 ft. No such table land is found, at this elevation on any other island.”  (The Garden Island, December 14, 1914)

In 1913, The Garden Island published a letter from George H Dole, a resident of Kauai, to Judge Jacob Hardy, describing the “first ascent of the highest mountain on Kauai by white men.” (1862)  The following are excerpts from that letter and article written 100-years ago (in a lot of respects, I suspect it remains much the same.)

“Permit me merely to premise that the mountain of Waiʻaleʻale, although in former times frequently visited by the natives, had never until our visit been trod by the foot of a haole.”

They left from Waimea, riding on horseback “through the cocoanut groves of the valley until we reached Kalaeokaua, where we turned off into the Makaweli valley.”

“Our general course through this valley was about northeast; as we proceeded, the road, – to use an expression from St. Paul, – waxed worse and worse; the sides of the valley became higher and more precipitous, till they reached a degree of rugged sublimity which made them worthy objects of contemplation.”

“The narrow path led us on up it winding course, now across the pure, cool waters of the brook, and now into the deep shade of a Kukui grove, from whose airy branches the brilliantly dyed little songster whistled a merry “God-speed,” or the awkward Aukuʻu (black-crowned night heron) gazed with wonderment in his yellow eyes.”

“The sides of the valley gradually approached each other and increased in height. Ever and anon we paused to take breath, and as we look upon the immense perpendicular walls almost surrounding us where ‘time had notched his centuries in the eternal rock,’ our souls would be filled with astonishment and awe.”

“After a march of an hour or two the trees, which hitherto had appeared only in isolated groves, formed a dense forest, with a wild tangled undergrowth of bushes and vines and heavy grass; the hillsides became less steep than before and green with vegetation.”

“A walk of about five miles brought us to the pretty water-fall of Waikakaa, which is perhaps one hundred and fifty feet in height, – we could only give its arrow-like flakes of white foam a passing glance as they descended with a quiet roar to the dark, deep waters of the round basin beneath, and then hastened up the steep hill, richly robed in a many-tined dress of green.”

“We … lunged into the labyrinths of the primeval forest with which these high table-lands are covered, and from which we only emerged when within a short distance of Waiʻaleʻale’s summit.”

“The trees consist chiefly of Lehua, although the Kauila, ʻŌhia, Koa, and many other varieties are frequently met with. The trees throughout this forest are often covered to the depth of two or three inches with gray moss, and the ground is at frequent intervals heavily carpeted with the same material.”

“The forest became wilder, and the country more broken than ever; not far from the cave we descended into a deep ravine and traveled in the bed of the stream for about a mile, sometimes jumping from one moss-covered stone to another at an imminent risk of slipping heels over head into the chilly water, and sometimes wading with complete abandon through the sparking fluid, where it was not over our knees in depth, to the inevitable deterioration of shoe leather.”

“The smooth sloping sides of Waiʻaleʻale soon greeted our delighted eyes, and in a short time, in crossing the Wainiha stream, we said “au revoir” to the old woods, and found ourselves on an open plain, which had a gentle inclination to the west, and was covered with coarse grass; here and there were clumps of bushes, – principally lehua and ohelo”.

“(S)cattering everywhere were wild flowers, some of them vying in beauty and delicacy with the rarest gems of the garden. In low and swamp spots a small variety of silver sword was growing in such profusion that the ground seemed almost covered with a mantle of snow. This whole vicinity would be, as was remarked by one of the company, an interesting field for the explorations of a botanist.”

Waialeale lake “is of a regular, elliptical shape, its two diameters being respectively forty-seven and forty-two feet;–in short, it appears much like an ordinary fish-pond. The chief outlet is the Wainiha stream at the north-west end; the ground is so extremely level along the course of this stream that it flows for a long distance without any perceptible current, and the water would apparently flow just as well the other way.”

“There is another outlet at the south-east end of the pond; it consist of a ditch, said to have been dug by the natives in some former generation, and conducts the water east to the edge of the tremendous pali, from which the pond is distant but a few rods. This little stream trickle down among the fern and grass is the Wailua River in embryo.”

“Thus this crystal lake in miniature is the source of two large streams which empty themselves into the ocean on opposite sides of the island.”

“If we looked off from the brink of the eastern precipice, whose perpendicular height is several thousand feet, nothing was to be seen but an ocean of cloud, so illuminated by the sun as to appear like a boundless field of the whitest snow beneath our feet. It was a very fine spectacle”.

“The whole of Puna was spread out like a map before us, and an exquisitely beautiful landscape it was. As perfect a combination of dark forests, and shimmering streams, and smooth plains, and verdant hills, and blue ocean, is rarely seen; everything was in harmony, – there was nothing to offend the taste.”

“But although the eastern view was invisible, the western was still unclouded and magnificent; the whole of the western portion of the island lay spread out in quiet grandeur, rugged and for the most part densely wooded. At the northeast was the Wainiha valley, with its blue precipitous sides, forming a yawning gulf so deep that no bottom could be seen from our point of observation.”

“Many miles away in the west the mighty pali of Puʻukapele and Halemanu was strikingly apparent, stretching like a stern impassable barrier across the island, from sea to sea.”

“About four o’clock we struck our tent and set out for the lower regions … We arrived at Waimea a little after noon the next day, feeling richly repaid for the toil of the journey, but satisfied that much remained yet unseen, and determining that we would try it again next season.

© 2024 Hoʻokuleana LLC

Filed Under: Place Names Tagged With: Hawaii, Kauai, Waialeale

February 27, 2024 by Peter T Young Leave a Comment

ʻOheʻo

Although the canoe was a principal means of travel in ancient Hawaiʻi, extensive cross-country trail networks enabled gathering, harvesting other necessities for survival.

Famed for his energy and intelligence, King Piʻilani and his son Kiha constructed the legendary Alaloa or long trail known as the King’s Highway.

It was built about the time Christopher Columbus was crossing the Atlantic, before there were roads in Hawaiʻi.  Back then, they were trails and Piʻilani was ruler of Maui.

According to oral tradition, Piʻilani unified the entire island of Maui, bringing together under one rule the formerly-competing eastern (Hāna) and western (Wailuku) multi-district kingdoms of the Island.   Piʻilani ruled in peace and prosperity.

Four to six feet wide and 138-miles long, this rock-paved path facilitated both peace and war.  It simplified local and regional travel and communication, and allowed the chief’s messengers to quickly get from one part of the island to another.  The trail was used for the annual harvest festival of Makahiki and to collect taxes, promote production, enforce order and move armies.

The southeastern section of the island of Maui, comprising the districts of Hāna, Kīpahulu, Kaupo and Kahikinui, was at one time a Royal Center and central point of kingly and priestly power – Piʻilani ruled from here (he built Hale O Piʻilani – near Hāna.)  This section of the island was also prominent in the later reign of Kekaulike.

Royal Centers were where the aliʻi resided; aliʻi often moved between several residences throughout the year. The Royal Centers were selected for their abundance of resources and recreation opportunities, with good surfing and canoe-landing sites being favored.

Long before the first Europeans arrived on Maui, Kīpahulu was prized by the Hawaiian aliʻi for its fertile land and abundant ocean.  The first written description of the region was made by La Pérouse in 1786 while sailing along the southeast coast of Maui in search of a place to drop anchor:

“I coasted along its shore at a distance of a league (three miles) …. The aspect of the island of Mowee was delightful.  We beheld water falling in cascades from the mountains,  and running in streams to the sea,  after having watered the habitations of the natives,  which  are  so numerous  that a  space of  three or four leagues (9 – 12 miles, about the distance from Hāna to Kaupō) may be  taken for  a single village.” (La Pérouse, 1786; Bushnell)

“But all the huts are on the seacoast, and the mountains are so near, that the habitable part of the island appeared to be less than half a league in depth.  The trees which crowned the mountains, and the verdure of the banana plants that surrounded the habitations, produced inexpressible charms to our senses…”

“… but the sea beat upon the coast with the utmost violence, and kept us in the situation of Tantalus, desiring and devouring with our eyes what it was impossible for us to attain … After passing Kaupō no more waterfalls are seen, and villages are fewer.” (La Pérouse, 1786; Bushnell)

With the development of the whaling industry on the island in 1880s the southeastern Maui population started to decline as people moved to main whaling ports, such as Lāhainā.  In the early-1900s, one of the regular ports of call for the Inter-Island Steam Navigation Company was here at Kīpahulu. Steamships provided passenger service around Maui and between the islands.

Kīpahulu Landing also provided a way for growers and ranchers to ship their goods to markets. (Today the land where Kīpahulu Landing existed is private but protected with a conservation easement, overseen by the Maui Coastal Land Trust (now part of the Hawaiian Islands Land Trust.))

The Hāna Sugar Plantation, formed in 1864, gradually increased production by expanding cane plantings toward Kīpahulu Valley.  (Cusick)

However, shortly after World War II, Paul I Fagan, an entrepreneur from San Francisco, bought the Hāna Sugar Co, formed a ranch and started tourism on this part of Maui.

It had been only 20-years since Hāna was linked to the outside world by a rough dirt road, and it would be almost two decades more before it was paved.

In 1946, Fagan built a small six-room inn, called Kaʻuiki Inn (it was later expanded). Fagan’s guests consisted of his friends as well as sportswriters, one of which gave Hana the current name of “Heavenly Hana.”  (Maui College)

Near here was ʻOheʻo; here was a succession of several waterfalls tumbling from one pool into another and so on up the gulch.  (One interpretation of the name Oheo is “moving origin” – suggesting all pools as one (Yardley.))

In order to entertain guests and promote tourism in East Maui, employees at Fagan’s Inn crafted a legend that these pools had been reserved exclusively for Hawaiian Royalty and, therefore, were considered a sacred site.  (Cusick)

Billed as Hawaiʻi’s “Seven Sacred Pools” to attract tourists, ʻOheʻo Gulch actually has a series of 24 bowls that carry water down the slopes of 10,023-foot Mount Haleakalā to the sea.  (NY Times)

Then in the 1960s, Kīpahulu residents Charles Lindbergh and Sam Pryor, and philanthropist Laurance Rockefeller, concerned that public use of this area may be lost, worked to protect it.  Through their efforts, Kīpahulu Valley and ʻOheʻo Gulch became the Kīpahulu District of Haleakala National Park on January 10, 1969.  (NPS)

This part of the Park is located about 15-minutes past Hāna town, near mile marker 42 on the Hāna Highway (Road to Hana) after it turns into Highway 31. 

© 2024 Hoʻokuleana LLC

Filed Under: Place Names, Economy Tagged With: Maui, Piilani, Paul Fagan, Seven Sacred Pools, Haleakala National Park, Hotel Hana, Kipahulu, Kaupo, Oheo, Hawaii, Hana, Haleakala

February 21, 2024 by Peter T Young Leave a Comment

Great Crack

The Great Crack is one of the most conspicuous features of the Southwest Rift Zone of Hawaii’s Kilauea Volcano. (Halliday) It is an extensive network of cracks, fissures and cones. It spans 8 miles in length, measures 50 feet in width and plunges down to a depth of 66 feet.

Hawaiian Volcano Observatory geologists believe that the crack formed as magma intruded into the rift zone causing the surface to spread, not from the island falling apart. While the exact time of its formation remains uncertain, research indicates that it might have occurred gradually over time. (NPS)

In 1823, an eruption caused lava to surge out from the lower section of the Great Crack and flow for about 6 miles into the ocean, destroying one small coastal village at Mahuka Bay.

English missionary William Ellis witnessed the aftermath of the eruption. “Messrs (William) Ellis, (Asa) Thurston, (Artemas) Bishop and (Joseph) Goodrich made a tour round the island of Hawai‘i, examining its various districts, conversing with the natives, and preaching the gospel 130 different times.”  (History of ABCFM) They were looking for suitable sites for mission stations.

Of this, Ellis wrote, “The people of Kearakomo also told us, that, no longer than five moons ago, Pele had issued from a subterranean cavern, and overflowed the low land of Kearaara, and the southern part of Kapapala.”

“The inundation was sudden and violent, burnt one canoe, and carried four more into the sea. At Mahuka, the deep torrent of lava bore into the sea a large rock, according to their account, near a hundred feet high, which, a short period before, had been separated by an earth quake from the main pile in the neighbourhood ….”

“We exceedingly regretted our ignorance of this inundation at the time we passed through the inland parts of the above-mentioned districts, for, had we known of it then, we should certainly have descended to the shore, and examined its extent and appearance.”

“We now felt convinced that the chasms we had visited at Ponahohoa, and the smoking fissures we afterwards saw nearer Kirauea, marked the course of a stream of lava, and thought it probable, that though the lava had burst out five months ago, it was still flowing in a smaller and less rapid stream.” (Ellis)

A hundred years later, geologist Harold Stearns officially named it the ‘Keaiwa Flow,’ which was a name the residents of Ka‘ū had been using informally back then. (NPS)

“The Keaiwa flow of 1823 from Kilauea welled up in the Great Crack and spread out seaward as a thin flow, in places only a few inches thick. The absence of cinders or driblet cones in or along the crack indicates that the usual fire fountains of Hawaii did not play during this eruption.”

“Lining the Great Crack in many places are lava balls that appear to be bombs, but that do not owe their form to projection.” (Stearns)

Beginning at roughly 2,300 feet in elevation, the lower extent of the Southwest Rift Zone is quite unlike any other on the island. Faulting activity here has consolidated into a feature named The Great Crack. It is just that, a single large crack that runs unbroken for more than 10 miles before finally reaching the coastline. (Coons)

“The Great Crack is one of a number of open cracks that fissure the southwest rift zone, a belt 1-2 miles wide extending southwestward from Kilauea to the sea.”

“Throughout most of its length the Great Crack has the general appearance of a steep-sided trench 20 to 30 feet wide. A few yards north of the head of the Keaiwa flow the crack breaks up into many smaller ones.”

“There are also graben areas [an elongated block of the earth’s crust lying between two faults and displaced downward] which seem to have been produced by the separation of the fissure into two cracks for a short distance and the later collapse of the narrow slices thus formed, with the subsidence of the magma.”

“In other places the graben is due to the collapse along the walls bordering the fissure when the region settled down after the extrusion of the lava.  In a few places, especially near the sea, the Great Crack decreases in width to about 2 feet, and it finally dies out in echelon fashion at the coast. The cracks beyond the area of extravasation are only a few inches wide.”

“The Great Crack … differs from the others only in its continuity; it can be traced continuously for about 8 miles, and before it was buried by the flow of 1920 it must have been traceable still farther toward Halemaumau.”

“However, the mere fact that the Great Crack is continuous does not necessarily indicate that it was all opened at one time. There is ample evidence to show that it belongs to a system of fissures from which lava has poured out again and again.” (Stearns)

The Great Crack “is the result of crustal dilation from magmatic intrusions into the rift zone and not from the seaward movement of the south flank. There is no evidence that the Great Crack is getting bigger at this time or that the island is tearing apart along this seam.”

“Where the crack is narrow enough that opposing walls can be compared, matching features fit together like pieces of a jigsaw puzzle. This suggests that a simple widening caused the crack. Opposite walls also have no vertical offset, so south flank subsidence did not influence the formation of the crack.”

“The total breakaway of the south flank block of Kīlauea … is not taking place at this time.” (USGS)

Notable features in the Great Crack are caves.  Most of the floor of the open crack is littered with breakdown, but there are occasional gaps where cave entrances and pit craters lead to greater depths within the Great Crack System. It is believed there are more than 20 of these.

“The National Park Service has acquired a nearly 2,000-acre Big Island property containing a chasm known as ‘The Great Crack.’ The oceanfront property adjacent to Hawaii Volcanoes National Park was purchased for $1.95 million in a recent foreclosure sale”.

“The park has been interested in the property northeast of Pahala for more than five decades, said Ben Hayes, the park’s director of interpretation.” (Associated Press, 2018)

The National Park is working to create a long-term plan for managing the Great Crack area. The park is exploring future public use options for these areas, with a community meeting in Fall 2023 to learn from local residents about the site’s resources and past uses. (NPS)

© 2024 Ho‘okuleana LLC

Filed Under: General, Place Names Tagged With: Hawaii, Volcano, Great Crack, Crack

February 11, 2024 by Peter T Young Leave a Comment

Halfway House

The way is long, the way is steep,
the road is crooked, the holes are deep;
on the Half Way House a blessing be?
Lord bless this house, and the thoroughbred flea,
For man may swear, and woman may weep.
But the cursed flea won’t let you sleep;
In the early morn, arise and go
The remaining way to the Lava flow
To the brink of the Pit of fiery depth
The Volcano House upon its width. …
(Max Pracht, San Francisco, 16 May 16, 1884)
(NPS, Volcano House Register)

In the 1800s, tourism was already developing as an important part of Hawaii’s economy. Honolulu was the principal destination and excursions to Kilauea crater were the main drawing card of the island of Hawai’i. Only hardy souls braved the “discomforts of the journey from Honolulu to the Volcano [which] were often vexatious and always considerable.” (Manning)

Two routes may be taken to the crater Kilauea, on the slope of Mauna Loa, one by Puna, the other by Ola‘a. Time being an object, the trip to and from the crater via Olaa can be accomplished in three days, which will give one day and two nights at the volcano house. (Manning)

The most traveled route between Hilo and Kīlauea was the Volcano Trail, which we now refer to as the “Old Volcano Trail” (at the time called “the Volcano Road”). (McEldowney)

The alignment of the Old Volcano Trail was mapped as early as 1874 by John M. Lydgate who referred to the Old Volcano Trail as “Road to Hilo”. The trail appears as a meandering line that straddled the ahupua‘a of ʻŌlaʻa and Keaʻau and strays in and out of the boundaries between the two. (ASM)

A critical step toward developing agriculture in ʻŌlaʻa was the creation of a new road between Hilo and Kīlauea located mauka of the Old Volcano Trail. As the new Volcano Road through ʻŌlaʻa was being built, the Crown made a large portion of potential agricultural lands (Ola‘a Reservation) available for lease and homesteading. (ASM)

The old trail effectively adjoins and runs mauka of the mauka lots in the mass of lots subdivided in Puna in the 1950s-70s (Hawaiian Acres to Fern Forest).

“Fifteen miles from Hilo Olaa is reached, the half-way stopping place. The intermediate territory is covered with ti plant and ferns, while the road consists mostly of pahoehoe lava, scantily covered with bunch grass and occasional bushes and trees.”

“‘The Half-way House’ at Olaa is merely a cluster of grass houses, a passable rest for travelers, who wish to spend the night, and obtain pasturage for horses.” (Whitney, 1875)

“There were at least two different structures over the years. The first probably existed as early as 1867, certainly by 1870. This structure was a one-room grass house with a wooden porch or lanai.”

“The interior was ‘divided in half by a curtain; in one half … a large four-poster bed, rough table and chairs, and in the other … a thick layer of grass covered with mats, on which … the whole family sleep.’”

“Those stopping during the day often used a mattress stuffed with pulu fiber from tree fern fronds laid on the floor instead of the four-poster bed.  Around 1880, Hawelu [the operator] built a hale la‘au, a substantial frame house with glass windows.”

“The new halfway house is mentioned in a promotional brochure, ‘The Great Volcano of Kilauea,’ designed by the publishers, Wilder’s Steamship Company, to attract tourists to ‘that extraordinary wonder of nature,’ Kilauea crater.”

“During the Hilo-Volcano horseback trip, the writer suggests a stop to rest at the halfway house, saying, “This house of accommodation has five bedrooms and the usual conveniences of a stopping place. …’” (Manning)

“Here several orange trees display their rich fruit in sight of the road. Although this point is 1138 feet above the sea level, and ten miles from Keaau, (the nearest point on the sea shore) the roar of the sea may be distinctly heard during a heavy surf.”

“Leaving Ola‘a, the route is over pahoehoe in all its varieties, thickly covered with wild grass, straggling ferns, creeping vines, and that vegetation which in tropical lands seeks only water to become impenetrable.” (Whitney, 1875)

“For more than 20 years, Hawelu and Lipeka operated a rest stop or halfway house on the Hilo-Kilauea crater trail. This horseback trip was said to ‘try the patience of most travelers.’”

“Tired and weary travelers could turn off the trail near ‘Kalehuapuaa . . . where there is a mauka road which goes to Hawelu’s.’ Over the years, halfway houses were variously situated along the trail.”

“Hawelu’s house was on the Hilo side of Mahiki. Visitors record that Hawelu’s was anywhere between 13 and 15 miles from Hilo, at an elevation of 1,138 or 1,150 feet. [“A comparison of the many descriptions places Hawelu’s near a point parallel with the Hilo end of present-day Mountain View, but on the Kea’au-‘Ola’a border”.]

“A visitor might rest at Hawelu’s for a few hours or overnight. Heavy rains occasionally stranded people at the halfway house for one or two days.”

“Each service was independently priced, but the price was the same regardless of the service. Horseshoeing was a dollar, food was a dollar, and lodging was a dollar. Lipeka was a full partner. The profits were divided in half, with Lipeka acting as banker.”  (Manning)

“Travelers variously reported the accommodations as beautiful and clean or dreary and dirty! Male travelers complained more  than females. Women seem to have expected rough ‘camp’ conditions. … Travelers throughout the Kingdom reported their tortures.” (Manning)

As noted by one in the Volcano House Register, “The undersigned left Hilo Friday morning June 7th at 6:30 a.m. Jo Puni as guide. Directly after leaving Hilo they received a moderate wetting down with a sun shower, wh. awakened them to the realities of Hawaiian travelling.”

“It was quite sultry until they arrived at the Half-way House, when a very distinct change in temperature was experienced. Showers of rain kept ahead of them from there to the Volcano House.”

“At the Half-way House a very good meal was heartily enjoyed, and a rest of two hours taken. They arrived at the Volcano House at 3:55 p.m. June 7.”

“The volcano was apparently quite active during the night, but the ride had fatigued your humble servants sufficiently to enable them to sleep soundly. They started for the crater at 7:45 a.m. and traveled down at a jog trot.” (Godwin McNeil, Sacramento, Cal., June 8, 1878; NPS, Volcano House Register)

With the new road, in May 1891 the Kilauea Volcano House began offering a package tour. It included steamer passage from Honolulu, a carriage ride from Hilo to the end of the half-finished road, and saddle horses supplied by Volcano Stables for the remaining ride. Accommodations were provided at the Volcano House.

In the same year, JR Wilson built Mountain View House as a rest stop on the new road. Little, if any, business would have been left to Hawelu’s independent halfway house by 1891 and he stopped his operation about that time. (Manning)

© 2024 Ho‘okuleana LLC

Filed Under: General, Place Names, Economy Tagged With: Hawaii, Volcano, Halfway House

February 10, 2024 by Peter T Young Leave a Comment

Mānā – Laumai‘a – Keanakolu Trail/Road

This is about a trail and a subsequent road on the east side of Mauna Kea.  Today, we call the Waimea end (and up Mauna Kea) the Mānā Road and the Saddle Road side of this road we call the Keanakolu Road,.  At least part of this trail/road was called Laumai‘a Trail.

Here is some of the background about the need for mauka access in this area of the Island of Hawai‘i, as well as some history on the trails/roads there.

Although the canoe was a principal means of travel in ancient Hawai`i, extensive cross-country trail networks enabled gathering of food and water and harvesting of materials for shelter, clothing, medicine, religious observances and other necessities for survival.

Trails and roads connected the coast with the uplands, probably easing travel through the upland forests. Boundary Commission records document numerous trails from the coast to the upper edge of the forest.

Most trails seem to have followed ahupua‘a boundaries (although this could be a factor of the Commission’s purpose, which was to define boundaries). (Tuggle)

Early accounts date back to the 1500s, at the time that ‘Umi-a-Līloa fell into a disagreement with the chief of Hilo over a whale

tooth (ivory) pendant. Traveling from Waipi‘o, across Mauna Kea, ‘Umi and his warriors camped in the uplands of Kaūmana.

Samuel Kamakau wrote that ‘Umi-a-Līloa “conferred with his chiefs and his father’s old war leaders. It was decided to make war on the chiefs of Hilo and to go without delay by way of Mauna Kea.”

“From back of Ka‘umana they were to descend to Hilo. It was shorter to go by way of the mountain to the trail of Poli‘ahu and Poli‘ahu’s spring at the top of Mauna Kea, and then down toward Hilo.  It was an ancient trail used by those of Hamakua, Kohala, and Waimea to go to Hilo.”

“They made ready to go with their fighting parties to Mauna Kea, descended back of Hilo, and encamped just above the stream of Waianuenue without the knowledge of Hilo’s people that war was coming from the upland. Hilo’s chiefs were unprepared.” (Kamakau, Ruling Chiefs)

In the period leading up to the mid-1800s, travel to Mauna Kea was done on foot along a system of trails that crossed the mountain lands.

Native ala hele (trails), which had been used for centuries and often provided the “path of least resistance,” to travel around and across the island, proved inadequate for the new methods of travel with horses, wagons and team animals.

By 1847, Kamehameha III had instructed island governors to undertake the survey of routes and construction of new roads, which became known as the Alanui Aupuni (Government Roads). Construction was to be paid for through taxation and “labor days” of the residents of the lands through which the roads would pass.  (ASM)

In 1862, the Commission of Boundaries (Boundary Commission) was established in the Hawaiian Kingdom to legally set the boundaries of all the ahupua‘a that had been awarded as a part of the Māhele.

Subsequently, in 1874, the Commissioners of Boundaries were authorized to certify the boundaries for lands brought before them. The primary informants for the boundary descriptions were old native residents of the lands, many of which had also been claimants for kuleana during the Māhele. (ASM)

An informant, Kalaualoha, stated that “in olden times the birdcatchers used to go up the Honohina and Pīhā roads, they could not go up Nanue as the road was so bad.”

“The canoe road of Nanue ran to mauka of Kaahiwa [Ka‘ahina stream], there it ended. But the roads on Honohina and Pīhā ran way mauka.” (Koa logs were selected, prepared in the forest and then hauled down canoe roads.) (Tuggle)

Puuhaula’s testimony for Pāpa‘ikou stated that “the old Alakahi road ran up the boundary to Palauolelo and was said to be the boundary between Makahanaloa and Papaikou.”

Coastal-inland travel in all likelihood extended beyond the limits of any particular ahupua‘a. But McEldowney suggests that paths in the upper subalpine region were not defined; rather, travelers followed “prominent landmarks rather than set or distinct trails.” (Tuggle)

It was not until the second half of the 1800s that specific routes up the mountain were established, probably related to the building and use of ranch establishments at ‘Umikoa (Kukaiau Ranch) and Humu‘ula (Humuula Sheep Station) as base camps.

A major cross-island trail crossed the upper edge of the Hakalau Forest area. In the 19th century, it was called the Laumai‘a road, but it likely originated in earlier times.  The present Keanakolu Road probably roughly follows the Laumai‘a alignment.  (Tuggle)

Cordy describes a trail on the east flank of Mauna Kea that connected Kohala, Waimea, and Hāmākua with Hilo. This could be the trail that was used by the high chief ‘Umi in his conquest of Hilo. (Kamakau, Tuggle)

“It was shorter to go by way of the mountain [Mauna Kea] to the trail of Poli‘ahu and Poli‘ahu’s spring at the top of Mauna Kea, and then down toward Hilo. It was an ancient trail used by those of Hamakua, Kohala, and Waimea to go to Hilo.”

Nineteenth century accounts document travel between Kawaihae and Hilo using a mountain route, although the specific alignment of the road may have varied somewhat from the earlier traditional trail.

Although this road probably follows the general alignment of earlier routes, there was a different path for what was alternatively referred to as the Laumai‘a road, the Laumai‘a-Hopuwai road, the Laumai‘a-Hope-a trail, or the connection to the Mānā (Waimea) road. (Tuggle)

The Kalai‘eha-Laumai‘a Trail, was paved with stones in the late 1800s to facilitate transportation of goods around the mountain. (ASM)  (Kalai‘eha is the large pu‘u (cinder cone) near Saddle Road on DHHL property, Hilo side of the Mauna Kea Access Road.)

Formal surveys of the Hilo-Kalai‘eha-Waimea government road via Waiki‘i (the early Saddle Road) were begun in 1862. The Kalai‘eha-Waiki‘i alignment remained basically the same until after the outbreak of World War II, and the paving of the “Saddle Road” in the 1940s.

In the area from Kilohana (on the north side of the present-day Girl Scout Camp) to Waiki‘i proper, the route is almost as it was finally laid out in 1869 (overlaying one of the ancient trails through the area), except for widening.

The Kalai‘eha-Hilo section of the route remained basically as constructed in 1869, but because of the dense forest vegetation and the difficulty encountered in traveling through the region, the route received little maintenance and use by travelers other than those on foot or horseback, generally on their way to one of the ranch stations or the summit of Mauna Kea. (Kumu Pono)

The Waimea-Mānā-Kula‘imano-Hilo route along the upper forest line of Hāmākua and Hilo, was developed in 1854, with subsequent modifications in 1877, and again in the 1890s, as a part of the Humu‘ula Sheep Station operation.

Further modifications to the Kalai‘eha-Keanakolu-Mānā route were made as a part of the tenure of Parker Ranch-Humu‘ula Sheep Station, the Civilian Conservation Corps (CCC), and Territorial Forestry tenure of the land. (Kumu Pono)

Access along the eastern side of Mauna Kea was by the old Waimea-Laumai‘a road, which was greatly improved by the CCC; “a truck trail has been cleared along the old horse trails on this mountain so that now one may negotiate the trip completely around Mauna Kea at the general elevation of 7,000 feet in an automobile.” (Judd, Tuggle)

In the 1930s, the CCC, under the direction of L Bill Bryan, undertook improvements on the mountain roads, particularly the section between Kalai‘eha and Keanakolu.

In 1942, following the outbreak of World War II, the US Army began realignment and improvements of the route that became known as the Saddle Road. Territorial ownership of the road was assumed on June 30, 1947.  (Kumu Pono)

Construction on the Alanui Aupuni from coastal Kona to the saddle lands was actually begun in 1849, and ten miles of the road, completed by 1850. The route was cut off by the lava flow of 1859, and all but abandoned by public use; though it remained in use by ranchers and those traveling between Kona, the saddle region, and Waimea until the early 1900s. (Kumu Pono)

© 2024 Ho‘okuleana LLC

Filed Under: General, Hawaiian Traditions, Place Names, Economy Tagged With: Hakalau, Laumaia, Hawaii, Keanakolu, Mana

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