Images of Old Hawaiʻi

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Wailau

“The glimpses of Molokai which one obtains from a steamer’s deck while passing to Honolulu from San Francisco or in passing to and from Maui (along its south shore,) give the impression that the island is bleak, mountainous and desolate.”

“Skirting its (north) shores on the Hālawa, Wailua and Pelekunu sides on Wilder’s fine steamer Likelike, gives a far different picture. For miles sheer precipices rise from the sea and tower 1,500 feet into the air.”

“Now and then, and sometimes in groups, beautiful waterfalls are seen on the face of the cliff, now falling in clear view for a couple of hundred feet, now hidden under denses masses of foliage, only to reappear further down, another silvery link in the watery thread which ends In a splash and scintillating mist in the breakers below.” (Hawaiian Gazette, March 31, 1905)

“Early the next morning, with a pleasant breeze from the NE, we stood over towards the east point of Mororoi (Molokai.) … we sailed to the westward … In this the land rises rather abruptly from the sea, towards the lofty mountains in the center of the east part of Morotoi …”

“… and though the acclivity was great, yet the face of the country, diversified by eminences and vallies, bore a verdant and fertile appearance. It seemed to be well inhabited, in a high state of cultivation, and presented not only a rich but a romantic prospect.” (Captain George Vancouver, March 19, 1793)

The windward valleys developed into areas of intensive irrigated taro cultivation and seasonal migrations took place to stock up on fish and precious salt for the rest of the year. Kalaupapa was well known for its bountiful ʻuala (sweet potato) crops and its fine-grained, white salt which was preferred over that from the salt ponds of Kawela and Kaunakakai. (Strazar)

The large windward valleys – Pelekunu, Wailau and Halawa – and Papalaua, along with all of Kalaupapa comprise the old Hawaiian Koʻolau Moku (district) of Molokai.

Wailau Valley (“many waters” – the largest along the coast) on Molokai’s North Shore has some interesting history.

The sea cliffs that surround Wailau on the island’s north shore were formed by the ‘Wailau Slide,’ in which a portion of the volcano collapsed into the ocean, leaving a swath of debris strewn across the ocean floor.

The sea cliffs represent the scar left by the collapse and Wailau and the other windward valleys were cut into the scar after the slide.

The Kalaupapa Peninsula, in north central Molokai, was formed later by volcanic rejuvenation.

Molokai’s North Shore Cliffs were designated a National Natural Landmark in December 1972. The Landmark includes 27,100 acres located along 17 miles of the northeast coast between Hālawa and Kalaupapa.

Four major valleys span the coastline, from Hālawa (at the east end of the island of Molokai) westward toward Kalaupapa: from east to west they are Pāpalaua, Wailau, Pelekunu and Waikolu.

This area is accessible by boat and trails into the valleys; there are no roads through North Shore Molokai.

Wailau is made up of a smaller broad valley on the east and a deeper valley on the west, with two major streams flowing down through them – Kahawai‘iki Stream and Wailau Stream.

The Wailau stream, which runs the entire length of the valley, is said to have received its name “because it began in many brooks that flowed from the palis on every side.”

Wailau was a major area of taro production from the pre-contact era until the 1930s, when the valley was abandoned due to a combination of factors, including flooding and unfavorable economic conditions.

A series of intact lo‘i, or taro terraces, forms an agricultural system distributed across almost the entire valley.

There are extensive terraces in the seaward lowlands and back in the lower valleys of streams. Approximately 80 acres were planted in taro. The banks of the numerous taro patches in the lowlands can still be seen from the air.

They say Wailau also has high terracing of valley sides comparable to that on the Napali coast of Kaua‘i.

The cliffs just beyond Pāpalaua Valley are home to Kahiwa Falls, the longest waterfall in the state (over 1,700-feet.) (Lots of the information and images come from reports by Windy K McElroy.)

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Wailau (Windy K McElroy)
Wailau (Windy K McElroy)
Wailau (Windy K McElroy)
Wailau (Windy K McElroy)
Wailau (Windy K McElroy)
Wailau (Windy K McElroy)
Wailau
Wailau
Wailau (Windy K McElroy)
Wailau (Windy K McElroy)
Wailau (Windy K McElroy)
Wailau (Windy K McElroy)
Wailau (Windy K McElroy)
Wailau (Windy K McElroy)

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Hālawa

“Early the next morning, with a pleasant breeze from the NE, we stood over towards the east point of Mororoi (Molokai.) … we sailed to the westward … In this the land rises rather abruptly from the sea, towards the lofty mountains in the center of the east part of Morotoi …”

“… and though the acclivity was great, yet the face of the country, diversified by eminences and vallies, bore a verdant and fertile appearance. It seemed to be well inhabited, in a high state of cultivation, and presented not only a rich but a romantic prospect.” (Captain George Vancouver, March 19, 1793)

“… a beautiful deep valley….watered by a large and delightful stream of fresh water which falls from the mountains…in two grand and beautiful cataracts one of which rushes over a perpendicular decent of more than five hundred feet into a deep…and crystal lake”.

“The stream which issues from the lake … is so situated as to be easily drawn off by sluices into the taro plots…. the valley is principally laid out in these small rectangular plots …” (Hitchcock, 1833; NPS)

In 1877, a native Hawaiian described Hālawa “as a very fertile valley, with wild fruits, mountain shrimps, and much water in the streams…. There were nine hundred and thirteen taro patches and with the hundred and nine others that I hadn’t counted, they totaled a thousand and thirty-two patches. Most of the land is covered in taro”. (NPS)

“The glimpses of Molokai which one obtains from a steamer’s deck while passing to Honolulu from San Francisco or in passing to and from Maui (along its south shore,) give the impression that the island is bleak, mountainous and desolate.”

“Skirting its (north) shores on the Hālawa, Wailua and Pelekunu sides on Wilder’s fine steamer Likelike, gives a far different picture. For miles sheer precipices rise from the sea and tower 1,500 feet into the air.”

“Now and then, and sometimes in groups, beautiful waterfalls are seen on the face of the cliff, now falling in clear view for a couple of hundred feet, now hidden under denses masses of foliage, only to reappear further down, another silvery link In the watery thread which ends In a splash and scintillating mist in the breakers below.” (Hawaiian Gazette, March 31, 1905)

The windward valleys developed into areas of intensive irrigated taro cultivation and seasonal migrations took place to stock up on fish and precious salt for the rest of the year. Kalaupapa was well known for its bountiful ʻuala (sweet potato) crops and its fine-grained, white salt which was preferred over that from the salt ponds of Kawela and Kaunakakai. (Strazar)

John FG Stokes, who was Curator of Polynesian Ethnology at Bishop Museum, was sent to Molokai in 1909 to survey the remains of the ancient Hawaiian temples (heiau) found there. Stokes recorded thirteen medium-sized heiau distributed along the lower slopes and two large luakini heiau.

Molokai used to be referred to as ʻAina Momona (the bountiful land,) reflecting the great productivity of the island and its surrounding ocean.

It is about 38-miles long and 10-miles wide, an area of 260-square miles, making it the 5th largest of the main Hawaiian Islands (and the 27th largest island in the US.)

The island was formed by two volcanoes, East and West, emerging about 1.5-2-million years ago. The cliffs on the north-eastern part of the island are the result of subsidence and the “Wailua Slump” (a giant submarine landslide – about 25-miles long that tumbled about 120-miles offshore – about 1.4-million years ago.)

Hālawa Valley is the easternmost valley at the edge of Molokai’s north shore; four other major valleys span the coastline, from Hālawa westward toward Kalaupapa: from east to west they are Papalaua, Wailau, Pelekunu and Waikolu.

Archeological surveys indicate that by the 1300s, Hālawa Valley’s population had expanded inland, and small irrigation systems were developed along the streams.

By the 1600s, an extensive taro irrigation system dominated the valley’s settlement pattern. At that time, the lower valley was entirely covered in large rectangular fields watered by long irrigation ditches (taro loʻi made up about 55-acres of land.)

Hitchcock who established the first permanent Mission Station at Kaluaʻaha in 1832, gave a census figure of 6,000 for the island. (Strazar)

These early counts were generally taken in the field by both native school teachers and missionaries. During this period, the Reverends Hitchcock and Smith preached once a week at seven different stations from Kamaloʻo to Hālawa, and in 1833 they estimated the population of the entire island to be about 3,300. (Strazar)

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Halawa Valley shoreline and cove
Halawa Valley shoreline and cove
Halawa Stream at the lower end of the valley
Halawa Stream at the lower end of the valley
Halawa_Molokai
Halawa_Molokai
Halawa-Bay
Halawa-Bay
Poi_making_out_of_doors._A_scene_at_Halawa,_Molokai,_in_1888,_Memoirs_Bishop_Museum,_Vol._II,_Fig._100
Poi_making_out_of_doors._A_scene_at_Halawa,_Molokai,_in_1888,_Memoirs_Bishop_Museum,_Vol._II,_Fig._100
Hawaiian woman seated in front of a grass house, Halawa, Molokai-Baker-PP-32-3-010
Hawaiian woman seated in front of a grass house, Halawa, Molokai-Baker-PP-32-3-010
Moa'ula Falls-alohafrom808
Moa’ula Falls-alohafrom808
Aerial-of-Halawa-Bay-North-Shore-Molokai
Aerial-of-Halawa-Bay-North-Shore-Molokai
Halawa Valley
Halawa Valley
Halawa waterfalls
Halawa waterfalls
Falls at the end of Halawa Valley
Falls at the end of Halawa Valley
Halawa Park
Halawa Park
Halawa selfie
Halawa selfie
Halawa Selfie
Halawa Selfie
Halawa-Settlement-Map-Kirch
Halawa-Settlement-Map-Kirch

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Hālawa Naval Cemetery

As a result of the December 7, 1941 attack on Pearl Harbor, there were 2,403 people killed and 1,178 wounded. Among the deceased were 2,008 Navy personnel, 109 Marine, 218 Army and 68 civilians.  (navy-mil)

World War II brought death to more than 300,000 Americans who were serving their country overseas.  While the war was on, most of these honored dead were buried in temporary US military cemeteries.

(Punchbowl was not a cemetery at that time.  In 1943, the governor of Hawaiʻi offered the Punchbowl for use as a national memorial cemetery; in February 1948 Congress approved funding and construction began.  The first interment at Punchbowl was made January 4, 1949.)

(Initially, the graves at National Memorial Cemetery of the Pacific were marked with white wooden crosses and Stars of David; however, in 1951, these were replaced by permanent flat granite markers.)

After the attack on Pearl Harbor December 7, 1941, the Navy selected Oʻahu Cemetery to bury the dead. At the time, only 300 plots at the cemetery were available for use.  Burials began there on December 8, 1941. (navy-mil)

“Historical records show that the Navy originally purchased plots in the cemetery October 9, 1919, and additional land was acquired in 1931. The current cemetery site was acquired April, 13, 1932.”  (NAVFAC)

Several temporary cemeteries were constructed – one was in lower Hālawa Valley, overlooking Pearl Harbor.

“On Dec. 9 it became evident that sufficient land was not available in Oʻahu Cemetery for this purpose.  By direction of the commandant (of the 14th Naval District), a site for a new cemetery was selected by the public works department. This site (Hālawa) was approved by the district medical officer and remaining burials were made in this new cemetery.”  (US Naval Hospital; Cole)

Over the course of about 4-years, about 1,500 graves were prepared (some containing multiple sets of remains.)  All bodies, except those of identified officers, were placed in plain wooden caskets. “Bodies of officers were placed in standard Navy caskets in order that they might later be disinterred and shipped home if desired.”

Two officers of the Chaplain Corps and two civilian priests from Honolulu rendered proper religious rites at the hospital and at the funeral ceremonies held each afternoon in the Oʻahu and Hālawa Cemeteries. The brief military ceremony held at the burial grounds included a salute fired by a Marine guard and the blowing of taps by a Marine bugler.  (navy-mil)

Following the war, Congress passed, and the President signed, a bill that authorized the War Department to take steps to provide a reverent final burial for those who gave the last full measure of devotion.

“A first step in determining the final resting place for Americans who died outside the continental United States during World War II will be taken this week, Col George E Hartman, commanding officer of the Schenectady General depot, US Army, announced yesterday. … letters will be sent to more than 20,000 next-of-kin of American dead now in 15 of 207 temporary cemeteries overseas.”

“Next-of-kin may choose to have remains of WWII armed forces personnel who dies overseas returned to the US for burial in a private cemetery; returned to the US for burial in a National Cemetery; buried in a permanent US military cemetery overseas; or buried in a private cemetery in a foreign country which is a homeland of the deceased or next-of-kin.”    (Schenectady Gazette, March 5, 1947)

In September 1947, the American Graves Registration Service (AGRS) disinterred and moved the remains to the Schofield Barracks Central Identification Laboratory (Schofield CIL), located at the AGRS Pacific Zone Headquarters, in order to effect or confirm identifications and return the men to their next of kin for burial.

Between August and September 1947, the US military exhumed 18 remains at Kāneʻohe Bay, 339 from Oʻahu Cemetery, and 1,516 at Hālawa, according to a 1957 government report.  (Cole)

What was the Hālawa Naval Cemetery is the vicinity of the Animal Quarantine and Hālawa Industrial Park.  (Currently, there are 135 Sailors, Marines and spouses interred in Oʻahu Cemetery.)

The image shows Hālawa Naval Cemetery.  (Babcock)  In addition, I have added other images in a folder of like name in the Photos section on my Facebook and Google+ pages.

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Hālawa Shaft

The Hawaiian Islands are made up of one or more shield volcanoes that are composed primarily of extremely permeable, thin basaltic lava flows (within the flows are a few ash beds.)  Ordinarily, basalts are among the most permeable rocks on earth.

When rain falls on the Islands, it does one of three things: (1) wets the land surface, shallow infiltration saturates the uppermost soil layer and replaces soil moisture used by plants and then is absorbed by the vegetation and/or evaporates (evapotranspiration;) (2) runs off, eroding the land, forming valleys and gouges in the mountain slopes (and also creates some spectacular periodic waterfalls;) or (3) percolates into the ground (slowly sinks into the ground and becomes groundwater.)

The latter contributes to the groundwater recharge of the area (in the Koʻolau, it takes about 9-months for the rain, now groundwater, to seep down through cracks and permeable materials in the mountain.) Other recharge components include cloud drip (moisture condenses on the trees and leaves as clouds/fog drift through) and irrigation of an area helps add to the recharge.

Rainfall percolating through the ground may accumulate in three principal types of groundwater bodies: (1) high-level bodies perched on relatively impervious soil, ash or lava layers; (2) high-level bodies impounded within compartments formed by impermeable dikes that have intruded the lava flows; and (3) basal water bodies floating on and displacing salt water.

The principal source of fresh ground water in the Hawaiian Islands is the roughly lens-shaped basal water body floating on and displacing denser sea water.  (It varies by area, sometimes there is high-level confined water.)  Recharge of the basal water body results directly from percolating rain water or by underground leakage from perched-water bodies and bodies impounded by dikes.

The Ghyben-Herzberg principle applies to this basal water that suggests the top of fresh water above sea level should be balanced by a thickness of fresh water below sea level about 40 times as great.  That generally means, for every foot of fresh water above sea level, there is 40-feet of fresh water below it.)

Water resources were becoming a challenge in the growing Honolulu community. “From the outset it was the Board’s major problem to supply the City of Honolulu with water from sources within its own boundaries as long as that remained possible.”

“The Board’s long range plan, however, contemplated the eventual necessity of going outside the boundaries of the District of Honolulu for additional artesian water but it had been thought that the time when this would have to be done was far in the future. However, when the emergency arose it was possible to advance this phase of the program by deferring the infiltration projects.”

“Bond moneys that would have been applied to infiltration were transferred to a new project through which additional artesian water will be brought into the city from a 284-foot inclined shaft and electrically-operated underground pumping station in North Hālawa Valley.”

“War has delayed the completion of the North Hālawa project and has greatly increased its cost. Army and Navy authorities have given us splendid cooperation on this project, and, although we cannot be certain how soon all the materials and equipment required for completion of the installation will reach us, progress on its construction has been satisfactory, and it should be completed within the year 1943.”  (Report of the Board of Water Supply, Ohrt’s Report, January 28, 1943)

North Hālawa Valley overlies the Pearl Harbor aquifer, an important source of potable water for the island of Oʻahu. Freshwater in the Pearl Harbor aquifer is part of a large, lens-shaped body of ground water that is thickest in the central part of Oahu and thins toward the coastline.

This lens of freshwater, known as the ‘basal lens,’ floats on saltwater that penetrates from the ocean into the basalt flows of which the island is composed.  (Izuka, USGS)

In some early installations, vertical wells were drilled in the tunnels to develop additional water.  Hālawa was different; it is referred to as a skimming tunnel.  It’s commonly called the Hālawa Shaft.

Skimming tunnels consist essentially of a vertical or inclined shaft constructed from the ground surface down to about the water table and one or more horizontal, or nearly horizontal, tunnels constructed laterally at, or just below, the water level to collect water.  (Peterson)

The fundamental advantage of the skimming tunnels over conventional wells is their capability to produce large quantities of fresh water from lenses so thin that drilled wells would recover only brackish water.

For this reason, skimming tunnels are especially useful in some of the dry leeward coastal areas of Hawaiʻi, as well as on many small oceanic islands with extremely thin fresh-water lenses.

Owing primarily to economic considerations and also to the greater flexibility of modern deep-well pumping stations, no new major skimming tunnels have been constructed in Hawaiʻi since the early 1950s. (Peterson)

The Hālawa Shaft facility is at an elevation of 165 feet above sea level; it’s one of five main shafts operated by the Honolulu Board of Water Supply. (The other main shafts include Wai’alae, Kalihi, Makaha and Pearl City.)

Approximately 15-million gallons of pure water is pumped every day from the Hālawa shaft by three pumping units which have a capacity of 18 to 20-million gallons per day.

The water pool is a ‘hole’ at the top of a 919-foot long water development tunnel below. The Hālawa Shaft was put in operation on August 22, 1944.  (Papacostas)

The completion of the Hālawa Shaft made possible the importation of water from the Pearl Harbor area to Honolulu permitting a reduction in draft from the Honolulu aquifer.

This change in draft has raised the water levels in Honolulu to the extent that this aquifer now appears to be functioning well within the limits of its safe yield. (Ground Water Development, 1958)

While I was at DLNR, I had the opportunity to have a private tour of the Hālawa Shaft.  The lack of a key to unlock a gate on the stairs leading down the shaft caused quite an embarrassment to the Water staff.

Rather than turn back, we climbed over the gate and were able to view the shaft and water pool.  (Check the photos in the album.)

The image shows a simple water level gauge at the water pool at the Hālawa Shaft.  In addition, I have included other related images in a folder of like name in the Photos section on my Facebook and Google+ pages.

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Pelekunu, Molokai

“The glimpses of Molokai which one obtains from a steamer’s deck while passing to Honolulu from San Francisco or in passing to and from Maul (along its south shore,) give the impression that the island is bleak, mountainous and desolate.”

“Skirting its (north) shores on the Hālawa, Wailua and Pelekunu sides on Wilder’s fine steamer Likelike, gives a far different picture.  For miles sheer precipices rise from the sea and tower 1,500 feet into the air.”

“Now and then, and sometimes in groups, beautiful waterfalls are seen on the face of the cliff, now falling in clear view for a couple of hundred feet, now hidden under denses masses of foliage, only to reappear further down, another silvery link In the watery thread which ends In a splash and scintillating mist in the breakers below.”  (Hawaiian Gazette, March 31, 1905)

The large windward valleys – Pelekunu, Wailau and Halawa – and Papalaua, along with all of Kalaupapa comprise the old Hawaiian Koʻolau Moku (district) of Molokai.

Literally defined, the word Pelekunu means “smelly for lack of sunshine.” (Pukui)   Being that it is such a tall and narrow valley, the sun is out for only about seven hours a day. Short days, coupled with the windward tendency for rain, creates a generally damp condition in Pelekunu.

Marion Kelly gives an alternate possibility suggesting the name Pelekunu relates to Pele, the goddess of the volcano. The area is said to be sensitive to very light earthquakes that are felt by the folks in the area, thus the name, Pelekunu, “coughing” or “grumbling” Pele.

Archaeological evidence suggests this area of Molokai was traditionally the home of the majority of early Hawaiians. The water supply was ample; ʻauwai (irrigation ditches,) loʻi kalo (wetland taro ponds) and habitation sites were found here.

“Every possible square yard was utilized for growing taro as the patches go nearly to the beach and even up the small ravines which cut the sides of the valleys. … In the matter of food, the emphasis which has been placed upon taro should not obscure the importance of fish whether from deep water or from other places and of fruits and other plant products.”

“The depth of the sea off this region prohibited the development of fish-ponds … but fishing with hook and line or with nets found rich opportunities.”  (Phelps, NPS)

The “narrowness of the gulches and their steep slopes result in the patches being no more than 12-feet on a side and the down-slope retaining wall may have to be seven-feet high.  The stream flows on one side of the gulch and is tapped at the highest placed patch, the water running successively into the lower ones.” (Phelps (1937,) NPS)

Pelekunu is an unusual ahupua‘a for several reasons. Within the Pelekunu ahupua‘a are three lele (disconnected portions of associated land) that belong to ahupua‘a on the other side of the island in the Kona District. Another unusual feature is that the ahupua‘a of Kawela actually extends up and over the mountains at the back of Pelekunu and runs into the valley.

Additionally, the ahupua‘a of Pelekunu includes not only most of the valley itself (less the extension of Kawela at the back and the lele within), but also the land of Honokaʻupu to the west as well as the small valley of Waiahoʻokalo just beyond.  (Eminger/McElroy)

The windward valleys developed into areas of intensive irrigated taro cultivation and seasonal migrations took place to stock up on fish and precious salt for the rest of the year. Kalaupapa was well known for its bountiful ʻuala (sewwt potato) crops and its fine-grained, white salt which was preferred over that from the salt ponds of Kawela and Kaunakakai.  (Strazar)

Emory (1916) describes Pelekunu Valley as the “most densely populated area of the ahupuaʻa … where we found miles and miles of huge stone terraces, witnesses of a once thriving population that must have run into the thousands.”  Taro was grown on the flat land and in the steep ravines of the valley.  (NPS)

The earliest recorded population figures we have for Molokai are those of visiting missionaries in 1823. A loose estimate of three to four thousand inhabitants in 1823 was published by Claudius S. Stewart in 1830. The Reverend Harvey Rexford Hitchcock who established the first permanent Mission Station at Kaluaʻaha in 1832, gave a census figure of 6,000 for the island.  (Strazar)

These early counts were generally taken in the field by both native school teachers and missionaries. During this period, the Reverends Hitchcock and Smith preached once a week at seven different stations from Kamaloʻo to Hālawa, and in 1833 they estimated the population of the entire island to be about 3,300.  (Strazar)

During the years around 1854, taro was raised extensively in the windward valleys and shipped as far away as Maui. Everywhere the inhabitants (of Pelekunu) were busy making baskets of ki (ti) leaves …., which they used to pack and transport … the product of their oasis, taro reduced to paʻiʻai (dry poi.)  (Strazar)

In 1898, Johnny Wilson (later Mayor of Honolulu) looked into living in Pelekunu and farming there.  Wilson’s parents’ friends included John and Lydia Dominus (Queen Liliʻuokalani) and King Kalākaua.

“We had known Mr. Wilson quite well as a young man when he was courting his wife. My husband and myself had warmly favored his suit; and, with his wife, he naturally became a retainer of the household, and from time to time they took up their residence with us.”  (Liliʻuokalani)

During her imprisonment, Queen Liliʻuokalani was denied any visitors other than one lady in waiting (Mrs. Eveline Wilson – Johnny’s mother.)  Johnny would bring newspapers hidden in flowers from the Queen’s garden; reportedly, Liliʻuokalani’s famous song Kuʻu Pua I Paoakalani (written while imprisoned,) was dedicated to him (it speaks of the flowers at her Waikiki home, Paoakalani.)

Johnny Wilson brought his wife Jennie Kini Kapahu to Pelekunu to live in 1902. The entry in Johnny’s diary for Tuesday, April 8, 1902, reads, “Arrived Pelekunu & occupied Koehana’s house”   According to Bob Krauss, Kini was “one of Hawai‘i’s premier hula dancers” and not used to country life; the Hawaiians in the valley wondered how long Kini would stick it out.

In the beginning Johnny and Kini lived at the shore, but sometime after the 1903 tsunami Johnny built Kini a house farther back in the valley.  Later, Johnny bought Kini a piano, the only one in Pelekunu.  (Krauss)

Kini did stick it out for quite a while. She helped teach the children in Pelekunu and ran their taro operation while Johnny was away. Eventually, however, Kini did leave the valley; in the summer of 1914, Kini finally got tired of the rain. She staged a one-woman mutiny and moved to a drier place on Molokai at Kamalō, where Johnny had a cattle ranch.

Wilson tried to aid the small native Hawaiian farmers by arranging for a steamer schedule to remote taro- and rice-producing areas.   When his plans for a commercial line fell through Wilson convinced the federal administration to place a post office in Pelekunu, guaranteeing regular steamer visits to deliver the mail. (Cook)

However, when his wife left (she was postmistress,) no one filled the post and the post office closed.  The steamships tried to keep regular schedules to Pelekunu to support the valley’s residents.  However, they were not regular enough and eventually others abandoned Pelekunu valley, deeming it as too isolated to remain viable in a cash economy. (Cook)

(Johnny Wilson served three times as mayor of Honolulu: from 1920 to 1927, 1929 to 1931 and from 1946 to 1954.)

In 1986, The Nature Conservancy purchased nearly 5,800-acres of Pelekunu Valley from Molokai Ranch to create a preserve to protect its natural and cultural resources.  (It contains nearly all the native Hawaiian aquatic fish, crustacean and mollusk species; in addition, 27-rare plant, 5-endemic forest bird and 2-endemic land snail species have been reported in the area.)  (TNC)

The Pelekunu Preserve is managed in partnership with the State Department of Land & Natural Resources through the Natural Area Partnership Program; due to its remote, rugged location, Pelekunu Preserve is not open to the public.

Pelekunu Preserve is bordered by four other managed natural resource areas: state-owned Pu‘u Ali‘i and Oloku‘i Natural Reserve Areas (NARs), Kalaupapa National Historic Park and the Conservancy’s Kamakou Preserve.

It is a part of the East Molokai Watershed Partnership (EMoWP); (a public-private partnership that protects more than 30,000 acres of contiguous ecosystems that range from sea level to 4,970 feet in elevation.)

The image shows an image of Pelekunu Village (Stokes, Bishop Museum – 1909.)  In addition, I have added other images in a folder of like name in the Photos section on my Facebook and Google+ pages.

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