Place Names | Page 25 | Images of Old Hawaiʻi

August 25, 2024 by Peter T Young Leave a Comment

Kahului Landing

It is believed that initial Polynesian discovery and settlement of the Hawaiian Islands occurred between approximately AD 1000 and 1200. (Kirch) This effectively started the ‘Settlement’ phase.

For generations, the small, slowly growing population clustered around shore sites near streams that supplied them with water. Such sites are best for inshore fishing.

The food plants of Hawaiʻi can be divided into three groups: those known as staple foods (the principal starchy foods – kalo (taro,) ʻuala (sweet potato,) ʻulu (breadfruit,) etc;) those of less importance (to add nutrients and variety to the diet;) and those known as famine foods. (Krauss)

Kamakau states that there were no chiefs in the earliest period of settlement but that they came “several hundred years afterward … when men became numerous.” The communities shared familial relations and there was an occupational focus on collection of marine resources.

By the 14th century, inland elevations to around the 4,000 foot level were being turned into cultivated fields of the early dryland Kona Field System.

By the 15th century, residency in the dry uplands was becoming permanent, and there was an increasing separation of chiefly class from commoners. In the 16th century the population stabilized and the ahupua‘a land management system was established as a socio-economic unit. (Kepā Maly)

“The sweet potato and gourd were suitable for cultivation in the drier areas of the islands. The cult of Lono was important in those areas, particularly in Kona on Hawaii and ‘Ulupalakua on Maui . At both of these places there were temples dedicated to Lono. The sweet potato was particularly the food of the common people.” (Handy Handy & Pukui)

In the later Hawaiian period (c. 1600-1800), leading to the eventual rise of Kamehameha I to power (c.1791 A.D.), the ko kula kai and ko kula uka (coastal and upland-slopes) of this area came to be extensively cultivated with important staple and supplemental crops suited to dryland planting techniques and the Kona environment. (Kepa Maly)

“Not the smallest piece of Ground was left uncultivated. By their accounts it is hardly possible that this Country can be better cultivated or made to yield a greater sustenance for the inhabitants; they passed thro fields of hay, with which they cover the young Tarro Grounds, to prevent the suns drying it up.”

“In their walk through the Villages they met with real hospitality, every one was desirous of entertaining them, & used enticing arts to prevail upon them to stay some time amongst them; these Villages were never found farther than 4 or 5 miles from the sea side”. (Journals of Captain James Cook, Beaglehole)

“Small bays generally had a cluster of houses where the families of fishermen lived-as in Kona, Hawaii, in the specific localities of Kailua, Holualoa, Kahalu‘u, Keauhou, Napo‘opo‘o, Honaunau, Kealakekua, and Ho‘okena. … Wherever a ruling ali‘i had his establishment there was a large aggregation of domiciles.” (Handy, Handy & Pukui)

Of significance to the land of Kahului, is the fact that a number of early historians record that the area between modern day Kailua Town to Keauhou, was favored by the ali‘i nui (high ranking chiefs) of the island of Hawai‘i as a residence. (Maly)

Kahului is a ili within the ahupua‘a of Holualoa. (Ili, ahupua‘a and moku are Hawaiian terms that refer to land divisions. A moku is a large section of an island, while an ahupua‘a is a portion of a moku that is typically somewhat pie-shaped, and runs from the mountains to the ocean, and an ili is a portion of an ahupua‘a.) (NPS, Henderson House) (Others suggest Kahului is an ahupua‘a.)

Kahului is a part of this larger district that was a significant political seat and population center. (Maly) On the makai side, at Kahului Bay, was a canoe landing.

“Look at all the ulu niu [coconut grove]. This is about 1890, it’s Kahului Bay, there are canoes at the landing, the sand was up. Look where all the people are standing. And there are thatched house here. This is where the Kona Tiki Hotel is now.” (Kepā Maly)

“You know, the shore was very different here, even when I was young. The beach came up with sand and rocks into the yard, and there used to be an old canoe and boat landing in front here. You know Kahului was an important landing, before days.”

“Over there [pointing to a thatched house in the picture on the north side of the landing] that’s where the Kona Tiki Hotel is now. You see, they’ve filled all this in to make the road and hotel. The landing is all changed now.”

“But look, there are so many people, all Hawaiians down on the shore. Now almost all the families are gone. Our house would be just off the picture here. Now, all these walls and house sites are all gone too.” (Luciana Ka‘ailehua Makuakâne-Tripp, Interview with Kepa Maly)

August 23, 2024 by Peter T Young Leave a Comment

DLNR’s Roles at the Ala Wai

During the 1920s, the Waikīkī landscape would be transformed when the construction of the Ala Wai Drainage Canal, begun in 1921 and completed in 1928, resulted in the draining and filling in of the remaining ponds and irrigated fields of Waikīkī.

“Over the decades, all sorts of pollution – pesticides, heavy metals, sediments and even raw sewage – has flowed into the canal. As Honolulu’s upstream population mushroomed, contamination in the canal has steadily increased …”

“… and over the years levels of pollution have tested well above limits considered safe. One local man died from bacterial infections he picked up after falling in the water.” (Civil Beat)

One role DLNR plays is dealing with the trash that floats down the respective drainage ditches up mauka that make their way into the Ala Wai.

Ala Wai small boat harbor is particularly prone to collecting trash that heavy rains, such as has been experienced this summer, wash down from watershed areas of Manoa, Makiki and Palolo streams.

Trash then flows down the Ala Wai canal, where a portion is captured in a debris trap, or amid the harbor front row piers and boats that is visible to the public.

“The trap utilizes a floating boom on the makai side of the bridge span next to Ala Wai Marine boatyard that captures tons of refuse after every rainstorm. But, like any trap, once it’s filled it must be emptied before it can function again.” (Pendleton)

DLNR Division of Boating and Ocean Recreation (DOBOR) is responsible for removing this mess from the traps. (DLNR) The trap is normally cleaned three to four times a year. The expense is paid through the Boating Special Fund (paid by boaters), not from General Funds from tax revenues.

That responsibility became more profound when, in 2006, “the city dumped 48 million gallons of untreated sewage into the canal – which flowed out into the ocean and polluted Waikiki beaches – in order to keep the waste from backing up into hotels, homes and businesses.” (Civil Beat)

“This spill is such a large magnitude. We have never seen this before,” said state Health Department spokesman Kurt Tsue. “It’s pretty bad.”

“More than 100 warning signs to stay out of the water were posted along a 1 ½-mile stretch covering 18 beaches from Waikiki to downtown Honolulu.” (LA Times)

“Oliver Johnson, a 34-year-old mortgage broker, died April 6 from a bacterial infection after falling or being pushed into the sewage-contaminated Ala Wai Harbor on March 31.” (Star Bulletin, April 15, 2006)

DLNR had to clean up the debris trap and we viewed it as a biological hazardous waste removal/treatment and “Workers in protective gear will begin cleaning the sewage-polluted Ala Wai Boat Harbor today, under a $50,000 state contract.” (Star Bulletin, April 15, 2006)

Some may recall the ‘black noodle’ in and around the Ala Wai. “The 5,135-foot sewage pipe that juts out of the water near community gardens on the mauka bank of the canal, has been a constant reminder of that environmental disaster.” (Civil Beat)

It took the City seven years to remove the large black sewage pipe that snaked along the bottom of the Ala Wai Canal and out toward the mouth of the boat harbor, adjacent to Waikiki’s famous beaches.

In addition to the surface collection of debris, DLNR is also responsible for periodic dredging of the Ala Wai Canal. Just as debris comes downstream, accumulated silt and sediments come down and collect in the Ala Wai.

The Ala Wai Canal serves as an essential drainageway and sediment basin for the Ala Wai watershed. Over time, the build-up of sediments into the Ala Wai Canal has affected the canal’s sediment- and water-holding capacity, reducing the canal’s ability to temporarily contain and then release storm water when there are heavy storm events. (Army Corps)

At times, “some areas are only 4 to 6 feet deep at high tide and canoes ply inches-deep water at low tide” (Honolulu); dredging is targeted to get water levels closer to “12-6 feet below the mean lower low water mark”. (DLNR)

As reported in 2003, “The dredging is a state-financed, $7.4 million effort to restore a measure of health and self-respect to the Ala Wai, which began filling with sediment almost as soon as the Army Corps of Engineers dug it in 1927 to control floods and mosquitoes and to provide landfill for the swampland that was then Waikiki.”

“The canal, which collects runoff from streams and storm drains on the densely populated mountain slopes above Waikiki, has been dredged periodically, most recently in 1979.” (NY Times, March 3, 2003)

A challenge was that Hawaiian Electric has underground electrical cable crossing under the Ala Wai (first installed in 1956 replaced in 1990 with higher capacity cables). “DLNR encountered Hawaiian Electric’s cables during routine maintenance dredging of the Ala Wai Canal” and “it was determined the cables were at risk of damage from dredging”.

“As a temporary solution, sections of the active cables on the makai side of the canal were covered with twelve 20-foot by 8-foot pre-cast concrete panels. The panels provided protection and allowed the dredging operations to continue in areas upstream of the cables.” (Belt Collins)

Later, “Hawaiian Electric relocated underground sub-transmission line cables that connect to HECO’s Waikiki Substation located on Kai‘olu Street.” This also shifted the alignment of the cable to the west of the existing route. New technology allowed for horizontal directional drilling to cross under the Ala Wai Canal.

In part, HECO’s action supported the Department of Land and Natural Resources’ efforts to provide continuous maintenance dredging of the Ala Wai Canal. The replacement cables also help maintain the reliability of the electrical distribution system. (Belt Collins)

DLNR Chief Engineer Carty Chang said, “The long-term benefits of this project include maintaining the ability of the canal to efficiently convey storm water flows to the ocean to reduce the risk of flooding, and to improve the aesthetics and safe use of the canal for recreational users.”

August 22, 2024 by Peter T Young Leave a Comment

Henrik Christian L’Orange

L’Orange is a Norwegian family of French origin. The family were Huguenots (Protestants), and after the repeal of the Edict of Nantes in 1685, members of the family had to leave France.

The first known man of the family, Jean L’Orange, who according to tradition came from St.-Quentin in Gascogne , probably came to Copenhagen at the end of the 17th century. His son Johan Gerhard L’orange (1696–1772) came to Norway and settled in Vestfold. (Norwegian Encyclopedia)

Fast forward to the end of the American Civil War in 1865; emigration from Norway to the US increased rapidly. But there were some who chose other destinations.

In 1877, Hendrik Christian (Christian) L’Orange (born in Fredrikshald in 1843) married Caroline Faye (born in Drammen in 1856), daughter of merchant Hans Peter Faye and his wife Karen Sophie Knudsen in Drammen. (Emigrantforlaget)

Following their wedding Christian and Caroline sailed for the islands of Hawai‘i in 1877. Her cousin, Anton Faye, also sailed with them to Kauai in 1877. Caroline’s uncle, Valdemar Knudsen, had already settled there in 1856.

Knudsen, Faye and L’Orange got involved in the operation of a sugar plantation on Kauai. (Scandinavian Club of Hawai‘i) Knudsen had acquired a 30-year lease on crown lands in the Waimea district where he established a ranch. Using an old Hawaiian ditch at Waiele, he drained and reclaimed about 50 acres on which he and L‘Orange planted sugar cane in 1878. (HSPA)

In 1879 Christian purchased his own plantation on Maui. He named it Lilikoi. He later sold the plantation and moved to Kauai. There he became the director of a sugar plantation, which was also given the name Lilikoi. (Norwegian Heritage)

As early as July 7, 1878, Captain L’Orange proposed to the Bureau of Immigration of the Hawaiian Kingdom to bring Scandinavian laborers to the Islands. By mid-June of 1880 he was involved in plans to go to Norway for contract workers to fill the needs of plantations represented by the sugar factors, Castle and Cooke. (Satrum)

By July 20, 1880, he had received his letter of appointment as agent of the Bureau of Immigration, and a few weeks later was on his way to Norway with a letter of credit for $20,000 from the firm of Castle and Cooke for expenses and advances.

Captain L’Orange had Instructions to hire not more than 400 adult workers, in a ratio of 35 to 40 women to each 100 men. These people were to be of ‘proper class’ and good workers, and no family was to bring more than two children. (Satrum)

A long depression from the mid-1870s to the early 1890s hit the Norwegian economy severely. Signs of the stagnation could be found in the large-scale immigration from Norway to North America during the 1880s. In the long-run, immigration was basically a result of increased labor productivity in the primary sector, causing surplus labor to find jobs in the New World. (Grytten)

Thousands were leaving Norway for other lands. This occurred at a time when there was actually a demand for more farm laborers in Hawai‘i. These circumstances partially determined who would be in the mix of people signing contracts as Hawaiian plantation workers. (Satrum)

L’Orange placed an advertisement in Drammen, Norway newspapers, stating, in part, “To the Emigrants for the Sandwich Islands Contracts with those who will go to the Sandwich Islands, are drawn up and signed on Wednesday, Sept. 23 … The parties must be provided with good recommendations, and attestations for good and faultless behaviour.”

“The conditions are now regulated, and thus fixed: laborers over 20 years, 9 dollars; under 20 years, somewhat less, per month, with free board, or board-money and free lodgings, families may bring two children with them. Free passage and board, which Is not to be worked out afterwards. Chr. L’Orange, Agent for the Hawaiian Bureau of Immigration, Sandwich Islands”.

The idea of a paid voyage and an opportunity to make their fortunes in a new land had an irresistible appeal to many Drammen folk that difficult year of 1880. Norwegians by the thousands were flocking to the US in response to promises of free land or jobs.

However, some were unable to raise the passage money, or unwilling to risk their savings on the gamble of a better life in a new country. To these the phrase, ‘free passage and board, which Is not to be worked out afterwards,’ had a special attraction. (Davis)

The planters were eager for the new laborers to arrive quickly, though Captain L’Orange warned that it would be impossible to find suitable ones in a hurry. The great need in Hawai‘i was for men to work in the fields. (Davis)

When L’Orange began hiring he found men with farm experience difficult to obtain. But there were plenty of artisans and industrial workers from the towns eager to sign his contracts, and from these came most of the recruits for Hawai‘i. (Davis)

Most of the recruits were from the town of Drammen or from nearby areas; but there were a few Swedes as well. The Norwegian bark Beta, commanded by Captain Kasper Rist Christensen, was first to weigh anchor (October 27, 1880). Almost 400 people made up the passenger list – 327 adults, Including 49 married couples, and 69 children 12 years and younger. (Davis)

The ship stopped briefly at Lahaina to take on board Captain L’Orange, who had traveled by a quicker route than the emigrants, and then went on to Ma‘alaea Landing. On February 18, 1881, it let down Its anchor.

On arrival, “The physician of the Board of Health pronounces them the most healthy company of men, women, and children he has ever seen and affirms that they are without the slightest taint of infectious diseases. The planters, who are so fortunate to obtain these laborers, highly value their adaptability by skill, as well as by physical strength, for almost every kind of work of plantations.”

“There are amongst them carpenters, blacksmiths, upholsterers, harness makers, printers, and engineers, while many of the women are admirably adapted for housekeepers.” (Hawaiian Gazette, March 2, 1881)

Two hundred and twenty eight adults with their children drew numbers assigning them to Maul. Passengers not included among this number remained on board to be trans-shipped at the end of the week to Hilo by the steamer Llkelike for work on the Hitchcock plantation is Pāpa’ikou. (Davis)

The German bark, ‘Musca’ sailed from Drammen for Hawai‘i, November 23, 1880. Its master was Captain DW Oltman, and it carried 237 passengers, including 29 married and 57 children 12 and under. Arriving in Honolulu on the island of O‘ahu, most of the workers were assigned to a variety of plantations. (Satrum)

The German bark, ‘Cedar’ arrived in Hawai‘i on July 18, 1881, primarily with Germans hired to work in the plantations of Hawai‘i, although there were ten Norwegians and four Swedes on the ship as well. One child was also born during the voyage. (Satrum)

So far, it is good news for the Hawai‘i sugar planters and the Norwegian workers. However, things soon soured …

On both Maui and the Big Island, the Scandinavians had begun complaining almost immediately: They didn’t like the food, they didn’t like their houses, they didn’t like their wages, they felt their employers violated their contracts, they found field work difficult, the Hawaiian sun burned their flesh unmercifully.

Many of the new immigrants declared, flatout, that they’d become slaves. By the time the Musca landed in Honolulu, the folks at Castle & Cooke wanted to scatter the latest contingent of Scandinavians as widely as possible so that they couldn’t band together in their complaints. … But the complaints continued. (Bowman)

For most of the Scandinavians, Hawai‘i was a place to leave as soon as it was possible. It is estimated that about 50 of the immigrants who came to the Islands aboard the Beta and the Musca remained in Hawai‘i.

Some of them stayed on the plantations and moved rapidly out of field work and into positions that took advantage of their industrial skills. Some became integrated into the fabric of Hawai‘i and led successful lives. Christian L’Orange found himself decidedly unpopular with his fellow sugar planters and disbanded his activities on Maui. (Bowman)

Around 1885 the family moved to Florida. One of the reasons that they left Hawai‘i was, without a doubt, all the criticism he had received for having brought such ill-suited laborers to work on the plantations there.

He bought property in Florida and became a tobacco farmer. Christian died in Florida in 1916. Caroline was buried in Hawai‘i in 1935. Their oldest son, Hans Peter Faye L’Orange (born in 1892 in Florida), became one of the administrators of O‘ahu Sugar Company. (Norwegian Heritage)

August 16, 2024 by Peter T Young Leave a Comment

Hot Spot

Kupuna means elder, grandparent or ancestor. The islands to the northwest of the main Hawaiian Islands have been referred to as the Kupuna Islands. The Hawaiian chain is made up of volcanic islands.

Kilauea Volcano has been erupting since 1983. Mauna Loa is also an active volcano. Off the coast, to the southeast, Kamaʻehuakanaloa Seamount (previously known as Loʻihi) is forming. (It is currently about 3,000-feet below sea level and is estimated to emerge above sea level in the next 10,000 to 100,000 years.)

Some of the other recent eruptions include Hualālai that last erupted in 1801; Haleakala that last erupted in about 1790 and Mauna Kea that last erupted about 4,000 years ago. (SOEST) (The first three volcanoes are considered ‘active’ and the latter three ‘dormant.’)

Hawaiʻi sits over a ‘hot spot,’ the Hawaiian hot spot.

It’s one hot spot, but lots of volcanoes have formed over it. The Islands are above a moving sea floor of the North Pacific Ocean (the Pacific Ocean is mostly floored by a single tectonic plate known as the “Pacific Plate.”)

The Pacific Plate is moving over the layer in the Earth known as the Asthenosphere. This movement takes it to the northwest. As the plate moves over a fixed spot deeper in the Earth where magma (molten lava) forms, a new volcano can punch through this plate and create an island.

As the plate moves away, the volcano stops erupting and a new one is formed in its place. With time, the volcanoes keep drifting westward and getting older relative to the one active volcano that is over the hot spot.

As they age, the crust that they sit on cools and subsides. This, combined with erosion of the islands, once active volcanism stops, leads to a shrinking of the islands with age and their eventual submergence below the ocean surface.

Each island is made up of at least one primary volcano, although many islands are composites of more than one. The Big Island, for instance, is constructed of 5 major volcanoes: Kilauea, Mauna Loa, Mauna Kea, Hualālai and Kohala (the island is still growing, but is basically about 400,000-years old.)

Maui is made up of two volcanoes, Haleʻākala and West Maui (about 1.32-million years ago.) Kahoʻolawe and Lānaʻi were each formed by a single volcano of their respective names.

Molokai was formed by East and West Molokai volcanoes (about 1.8-million years ago.) Oʻahu is also formed by two, Koʻolau and Waianae (about 3-million years ago.) Kauai and Niʻihau were formed by volcanoes of their respective Island names (about 5.1-million years ago.)

They are all part of the Hawaiian-Emperor Volcanic Chain. About 40-million years ago, the Pacific Plate changed direction from north to northwest – so the Emperor Seamounts run more north-south, the Hawaiian Ridge north-westerly.

Midway Island is 27.7-million years old; Meiji Seamount the northern part of the Emperor Seamount (near the end of the Aleutian chain) is about 80-million years old.

All of these are still youngsters, when you look at the perspective, say, of the dinosaurs. The Islands weren’t even a glimmer in anyone’s eyes when dinosaurs walked the Earth; sixty-five million years ago the last of the non-avian dinosaurs went extinct, after living on Earth for about 165-million years. (USGS)

If all of Earth time from the very beginning of the dinosaurs to today were compressed into 365 days (1 calendar year), the dinosaurs appeared January 1 and became extinct the third week of September.

Using this same time scale, the Earth would have formed approximately 18.5-years earlier. By comparison, people have been on earth only since December 31 (New Year’s eve.) (USGS)

When I was at DLNR, President George W Bush created the Northwestern Hawaiian Islands Marine National Monument on June 15, 2006. Seeking a more appropriate Hawaiian name for the monument, suggestions for a name change were submitted.

We selected the name Papahanaumokuakea; it was submitted by Pua Kanahele. Pua and the First Lady, Laura Bush, attended the ceremony announcing the new name (March 2, 2007.)

The Kumulipo, the creation chant, tells of the history of how all life forms came and evolved from Papahanaumokuakea, beginning with the coral polyp – the building block for all life.

Papahanaumoku is a mother figure personified by the earth and Wakea is a father figure personified in the expansive sky; the two are honored and highly recognized ancestors of Native Hawaiian people.

Their union resulted in the creation, or birthing, of the entire Hawaiian archipelago. The naming of the monument is to honor and preserve these names, to strengthen Hawaii’s cultural foundation and to ground Hawaiians to an important part of their history.

Thus, the genealogy of Papahanaumokuakea tells the story of Native Hawaiians’ ancestral connection with the gods who created those coral polyps, the Northwestern Hawaiian Islands or Kūpuna Islands, and everything else in the archipelago. (Lots of information here from the UH-Manoa SOEST, USGS and Papahanaumokuakea.)

Hawaiian Ridge – Emperor Seamounts

NWHI_Map-noting Kure

Loihi-compared to Hawaii Island

Papahanaumokuakea-Marine-National-Monument-Map

hawaiimap-loihi-SOEST

Hawaiian Islands – Emperor Seamounts

Hawaiian Archipelago

Age of Islands-map

Hawaiian- Emperor Seamounts

3D of Kamaʻehuakanaloa (Lo’ihi)

Papahanaumokuakea Naming Ceremony-postcard-signed by Pua Kanahele-03-02-2007

TectonicPlates

Plates

Hawaiian Islands for space-NASA

August 13, 2024 by Peter T Young Leave a Comment

Waihī Nui

“Manoa valley ends in what is called ‘the pen.’ It has walls with a trail into Pauoa valley.” (Towse) “Rocky, wooded ridges enclose it to right and left, and straight ahead is the black, sheer face of Konahuanui.” (Loomis)

Translated “his large seeds (testicles,)” the name Kōnāhuanui is said to come from a story summarized by T Kelsey: “when a man, probably a giant, chased a woman who escaped into a cave, he tore off his testes and threw them at her”. (Kawaharada)

Kōnāhuanui is the highest peak in the Koʻolau Mountains and is the northwest corner of the Mānoa Ahupua‘a boundary. It was the home of the gods Kāne and Kanaloa.

It is also home to a moʻo goddess, a large mythic lizard that lives in freshwater pools and streams. Rain clouds gather around its peak, and its Kona side, often ribboned with waterfalls, is the wettest area of Honolulu: here is the source of the waters of Mānoa and Nuʻuanu valleys.

“[T]his cul-de-sac at its makai, or southern, angle, along the stream called ‘Aihualama. The trail into Nu‘uanu opened at its upper left, or northwestern, angle. Here was a good path for a kama‘aina going alone from valley to valley”. (Loomis)

In an 1882 map of Manoa prepared by Baldwin, there are several waterfalls back in the valley, including, Waiihi-nui (Waihī Nui), Waihii-iki (Waihī Iki), Luaaulaea and Naniuapo.

“[T]he ground rises rapidly for a few rods, to a thicket of hibiscus and eugenia, at the foot of a magnificent mountain, exhibiting from the base to its summit a perpendicular height of a thousand feet – as rich a variety of projecting cliff and wild recess, of dripping rocks and mantling foliage, of graceful creeper, pendant shrub, and splendid flower, as Arcadia itself can boast.” (Stewart)

“On the curve of high cliffs at the mauka boundary of Manoa sheer white splashes of waterfall filled pools hidden from the casual eye in recesses where Kaahumanu herself loved to bathe among cool winds and soft air laden with fragrance of awapuhi and maile.” (Damon)

The water from these falls converge into Manoa Stream. Mānoa Valley formerly supported a large population with scores of lo‘i kalo that were watered by the many freshwater streams. (ASM)

“When we had seen the piece of land appropriated by Kalaimoku or Mr. Pitt to our use, and had given directions to the natives who cultivated the taro on the land, we indulged ourselves with a pleasant bath in a cooling stream that waters the valley, and we returned across a part of the mountain which lies between that place and Honoruru valley.” (Missionaries Chamberlain, Loomis, Blatchely and Bingham; Damon)

“The taro patches that followed the stream bed down the center of the valley were now either vegetable gardens, pasture land, or abandoned. … AIso much of the stream’s water had been diverted for the use of the island’s increasing population. The taro farms that were in the valley from the time the first foreign observer stepped into it were gone for good.” (DeLeon)

“In 1919 the Hawaii Sugar Planters’ Association established an experimental substation in the rear of the valley. Here sugar cane was raised for experimental purposes. Trees from all over the Pacific were also brought to the substation to see how they would adapt to the Hawaiian environment. The substation became Lyon Arboretum, which is part of the University of Hawaii.” (DeLeon)

There is something about falling water that fascinates a human being.

As noted above, here is Waihī Nui (‘trickling water’), Mānoa Falls. It’s in the backyard of Hawai‘i’s largest population and visitor destination. A bus line takes you within walking distance to the trailhead.

It is one of the most popular trail destinations on O‘ahu; Mānoa Falls sees an average of 200,000 visitors annually. (DLNR) The Mānoa Falls Trail is part of DLNR’s Na Ala Hele Trail & Access Program.

The video (done by DLNR) shows people down by the falls. Don’t go there; rather, there is a viewing area contained by a rock wall at the falls – heed all warning and other signs, do not go beyond the rock wall.

The State does not charge a fee to hike this trail. The Mānoa Falls Trail is open seven days a week – sunup to sundown. The parking lot is managed by Paradise Park and is not associated with the management of the state trail.

The beginning of the trail goes through a shipping container into a big open lush field used as a location for many movies. The trail continues past the field, then crosses over a natural wood footbridge through a grove of Eucalyptus trees.

The 0.8-mile trail (each way) gradually ascends through a rainforest that eventually transitions into bamboo. There is a low-lying rest area on the right of the trail with benches, interpretive sign and tree arch throne.

Continue up ascending gravel terrace steps until you round the corner that reveals the water fall from a distance. On the left you will another rest stop with a bench and interpretive sign. There is one more short section of terrace steps that leads up to a nice flat section of trail that gently takes all the way to small section of cement steps.

Ascend up the steps and now you are at the falls viewing area. On your left is a bench and viewing area is straight ahead. The viewing area is contained by a rock wall.

Signs are posted indicating to not go beyond that point, and of the potential danger of landslide. Do not go beyond the rock wall viewing area, closed area signs or into pool area or to upper pools. (DLNR)