Images of Old Hawaiʻi

by Peter T Young 2 Comments

Hilo Railroad Company – Hawaiian Consolidated Railway

The Treaty of Reciprocity (1875) between the United States and the Kingdom of Hawai‘i eliminated the major trade barrier to Hawai‘i’s closest and major market.  Through the treaty and its amendments, the US obtained Pearl Harbor and Hawai‘i’s sugar planters received duty-free entry into US markets for their sugar.

At the industry’s peak in the 1930s, Hawaiʻi’s sugar plantations employed more than 50,000 workers and produced more than 1-million tons of sugar a year; over 254,500-acres were planted in sugar.

Sugar cultivation exploded on the Big Island.  As a means to transport sugar and other goods, railroading was introduced to the Islands in 1879.

On March 28, 1899, Dillingham received a charter to build the original eight miles of the Hilo Railroad that connected the Olaʻa sugar mill to Waiākea, that was soon to become the location of Hilo’s deep water port.

Rail line extensions continued.  Extensions were soon built to Pāhoa, where the Pahoa Lumber Company was manufacturing ʻōhia and koa railroad ties for export to the Santa Fe Railroad.

Although not the first railway on the Big Island, the Hilo Railroad was arguably the most ambitious.  The Olaʻa line was completed in 1900, immediately followed by a seventeen mile extension to Kapoho, home of the Puna Sugar Company plantation.

Immediately after that two branch lines were constructed (also to sugar plantations,) and then the railroad was extended north into Hilo itself.

All the sugar grown in East Hawaiʻi, in Puna and on the Hāmākua Coast, was transported by rail to Hilo Harbor, where it was loaded onto ships bound for the continent.

An early account stated that the rail line crossed over 12,000 feet in bridges, 211 water openings under the tracks, and individual steel spans up to 1,006 feet long and 230 feet in height.

Some of the most notable were those over Maulua and Honoliʻi gulches, the Wailuku River and Laupāhoehoe.  Over 3,100 feet of tunnels were constructed, one of which, the Maulua Tunnel, was over half a mile in length.

While the main business of the railroad remained the transport of raw sugar and other products to and from the mills,  it also provided passenger service.

A chiefly tourist line, branching from Olaʻa, was built inland 12.5 miles up the mountain to Glenwood where visitors to the Volcano House near Kilauea Volcano would then transfer to buses. Due to stiff competition from motor vehicles, the Glenwood extension was scaled back to Mountain View in 1932.

Between 1909 and 1913, the Hāmākua Division of the railroad was constructed to service the sugar mills north of Hilo. Unfortunately, the cost of building the Hāmākua extension essentially destroyed the Hilo Railroad, which was sold in 1916 and reorganized as the Hawaiʻi Consolidated Railway.

Targeting tourists to augment local passenger and raw sugar transport, the Hawaiʻi Consolidated Railway ran sightseeing specials under the name “Scenic Express.”

Not for the faint of heart, these trips included a stop on the trestles, where passengers disembarked to admire the outstanding scenery.

The Great Depression saw a decrease in business, but business picked up in the 1940s, when thousands of battle-weary troops packed the passenger cars en route to Camp Tarawa, in Waimea, to rest, recuperate and prepare for another campaign.

But the end was near for the Hawaiʻi Consolidated Railway. Early in the morning of April 1, 1946, a massive tsunami struck Hawaiʻi. The railroad line between Hilo and Paʻauilo suffered massive damage; bridges collapsed, trestles tumbled and one engine was literally swept off the tracks.

The expensive option of rebuilding the railway was rejected. Hawaiʻi Consolidated offered the rights-of-way, tracks and remaining bridges, trestles and tunnels to the Territory of Hawaiʻi, but the offer was refused, and finally the company sold the entire works to the Gilmore Steel and Supply Company.

Shortly thereafter, realizing its error, the Territory bought it all back.  Much of the current highway along the coast follows the route of the old railroad; five original railroad trestles have been converted into highway bridges.  (This route averaged better than one bridge per mile over its 40-mile length.)

At the time of the tsunami, plantations were already phasing out rail in favor of trucking cane from the field to the mill. It was inevitable that trucking would also replace rail as the primary means of transporting sugar to the harbor. The tsunami accelerated that transition.

Most sugar from Hāmākua was trucked to Hilo Harbor, although the Hāmākua Sugar Company continued to use its offshore cable landing at Honokaʻa until 1948.

A few remnants of the railway are still visible. Hawaiʻi Consolidated’s yards were in the Waiākea district of Hilo, where the roundhouse still stands today, next to the county swimming pool on Kalanikoa Street.

In Laupāhoehoe, a concrete platform remains where Hula dancers once performed for tourists. And the Laupāhoehoe Train Museum is housed in the former home of Mr. Stanley, the superintendent of maintenance.

Today, the Laupāhoehoe Train Museum and Visitors Center keeps the memory of Hawaiʻi Consolidated Railway alive.  Although the Laupāhoehoe Train Museum is among the state’s smallest museums, it attracts an estimated 5,000 visitors a year. The admission fee is $4 for adults, $3 for seniors, and $2 for students. Special rates for tours are also offered.

The museum is open weekdays from 9 am to 4:30 pm and on weekends from 10 am to 2 pm. The address is 36-2377 Māmalahoa Highway, Laupāhoehoe, Hawaiʻi 96764.  (Lots of information here for Laupāhoehoe Train Museum and Ian Birnie.)

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Island Summits

He ‘Ohu Ke Aloha; ‘A‘ohe Kuahiwi Kau ‘Ole
Love is like mist; there is no mountaintop that it does not settle upon

“… as the sun shining in his strength dissipated the clouds, we had a more impressive view of the stupendous pyramidal Mauna Kea, having a base of some thirty miles, and a height of nearly three miles.  Its several terminal peaks rise so near each other, as scarcely to be distinguished at a distance.”

“These, resting on the shoulders of this vast Atlas of the Pacific, prove their great elevation by having their bases environed with ice, and their summits covered with snow, in this tropical region, and heighten the grandeur and beauty of the scene, by exhibiting in miniature, a northern winter, in contrast with the perpetual summer of the temperate and torrid zones below the snow and ice.”

“The shores along this coast appeared very bold, rising almost perpendicularly, several hundred feet, being furrowed with many ravines and streams. From these bluffs, the country rises gradually, for a few miles, presenting a grassy appearance, with a sprinkling of trees and shrubs.”

“Then, midway from the sea to the summit of the mountain, appeared a dark forest, principally of the koa and ʻōhia, forming a sort of belt, some ten miles in breadth-the temperate zone of the mountain.”  (Bingham at first sight of the Islands, 1820)

And when you think about high elevation places in the Hawaiian islands, of course you have to talk about that basic dichotomy between the lower elevation places where people live.

And in old times, the lower elevations would have been called the Wao Kanaka. Wao being a word that means “zone” and “Kanaka” being a person. So the Wao Kanaka is a zone in which people belong.

When you rise above that zone, you enter into a realm in which all of the living things there are not there because of human activity. They flourish as the result of the activity of the gods, or the Akua. And so that zone is called the Wao Akua. And the transition from Wao Kanaka to Wao Akua is not taken lightly.  (Gon)

The Islands’ peaks are considered the piko (summit or center of the land) and are considered sacred.  The places upon which clouds nestle are considered wao akua, the realm of the gods.  Clouds cover the actions of the gods while they walk the earth. The higher the piko, the closer to heaven, and the greater the success of prayers. (Maly)

Let’s look at Hawaiʻi’s peaks, the highest point on each Island as we move down the Island chain.

Niʻihau – Pānīʻau (1,281-feet)

Ni‘ihau was formed from a single shield volcano approximately 4.89-million years ago, making it slightly younger in age than Kaua‘i. It is approximately 70-square miles or 44,800-acres.  It’s about 17-miles west of Kauaʻi.

Pānīʻau, the island’s highest point, is 1,281-feet; approximately 78% of the island is below 500-feet in elevation.   Located inside Kauai’s rain shadow, Ni‘ihau receives only about 20 to 40-inches of rain per year.  Ni‘ihau has no perennial streams.  (DLNR)

Kauai – Kawaikini (5,243-feet)

Geologically, Kauai is the oldest of the main inhabited islands in the chain. It is also the northwestern-most island, with Oʻahu separated by the Kaʻieʻie Channel, which is about 70-miles long. In centuries past, Kauai’s isolation from the other islands kept it safe from outside invasion and unwarranted conflict.

Near the summit (Kawaikini) is Waiʻaleʻale; in 1920 it passed Cherrapunji, a village in the Khasi hills of India, as the wettest spot on Earth (recording a yearly average of 476-inches of rain.)

Oʻahu – Kaʻala (4,025-feet)

The Waiʻanae Mountains, formed by volcanic eruptions nearly four-million years ago, have seen centuries of wind and rain, cutting huge valleys and sharp ridges into the extinct volcano.  Mount Kaʻala, the highest peak on the island of Oʻahu, rises to 4,025-feet.

Today, only a small remnant of the mountain’s original flat summit remains, surrounded by cliffs and narrow ridges. It’s often hidden by clouds.

Molokai – Kamakou (4,961-feet)

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.)

Kamakou is part of the extinct East Molokai shield volcano, which comprises the east side of the island.   It and much of the surrounding area is part of the East Maui Watershed partnership and the Kamakou Preserve.  A boardwalk covers part of the rainforest and bog to protect the hundreds of native plants, birds, insects and other species there.

Lānai – Lānaihale (3,337-feet)

The island of Lānai was made by a single shield volcano between 1- and 1.5-million years ago, forming a classic example of a Hawaiian shield volcano with a gently sloping profile.  (SOEST)  The island of Lānai is about 13-miles long and 13-miles wide; with an overall land area of approximately 90,000-acres, it is the sixth largest of the eight major Hawaiian Islands.

“At the very summit of the island, which is generally shrouded in mist, we came upon what Gibson (an early (1861) Mormon missionary to the islands) called his lake – a little shallow pond, about the size of a dining table.  In the driest times there was always water here, and one of the regular summer duties of the Chinese cook was to take a pack mule and a couple of kegs and go up to the lake for water.”  (Lydgate, Thrum)

Maui – Haleakalā (10,023-feet)

Haleakalā was thought to have been known to the ancient Hawaiians by any one of five names: “Haleakalā,” “Haleokalā,” “Heleakalā,” “Aheleakalā” and “Halekalā.” (Hawaiʻi National Park Superintendent Monthly Report, December 1939)

Haleakalā is best known in stories related of the demi-god Māui; he is best known for his tricks and supernatural powers. In Hawaiʻi, he is best known for snaring the sun, lifting the sky, discovering the secrets of fire, fishing up the islands and so forth.  (Fredericksen)

Kahoʻolawe – Lua Makika (1,477-feet)

Kahoʻolawe is the smallest of the eight Main Hawaiian Islands, 11-miles long and 7-miles wide (approximately 28,800-acres;) it is seven miles southwest of Maui.  The highest point on Kahoʻolawe is the crater of Lua Makika at the summit of Puʻu Moaulanui, which is about 1,477 feet above sea level.

Located in the “rain shadow” of Maui’s Haleakalā, rainfall has been in short supply on Kahoʻolawe.  However, nineteenth century forestry reports mentioned a “dense forest” at the top of Kahoʻolawe.  Historically, a “cloud bridge” connected the island to the slopes of Haleakalā.  The Naulu winds brought the Naulu rains that are associated with Kahoʻolawe (a heavy mist and shower of fine rain that would cover the island.)

Hawaiʻi – Mauna Kea (13,796-feet)

Nani Wale ʻO Mauna Kea, Kuahiwi Kūhaʻo I Ka Mālie (Beautiful is Mauna Kea, standing alone in the calm) expresses the feeling that Mauna Kea is a source of awe and inspiration for the Hawaiian people. The mountain is a respected elder, a spiritual connection to one’s gods.   (Maly)

A significant pattern archaeologists note in their investigations is the virtual absence of archaeological sites at the very top of the mountain. McCoy states that the “top of the mountain was clearly a sacred precinct that must, moreover, have been under a kapu and accessible to only the highest chiefs or priests.”  (Maly)

ʻĀina mauna, or mountain lands, reflects a term used affectionately by elder Hawaiians to describe the upper regions of all mountain lands surrounding and including Mauna Kea.  (Maly)

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Kailua-Kona in 1819

The expedition sailed from Toulon on the 17th of September 1817 … “Finally, (they) arrived at Havre on the 15th, (November 1820) … The duration of the voyage was therefore three years and two months nearly”.

“The principal object of the expedition commanded by Captain Freycinet, was the investigation of the figure of the earth, and of the elements of terrestrial magnetism; several questions of meteorology had also been suggested by the Academy as worthy of attention.”

“Although geography certainly formed but a secondary object in the voyage, it was natural to anticipate that so many experienced and zealous officers, well provided with excellent instruments, would not circumnavigate the globe without making some valuable additions to the existing tables of latitude and longitude.” They came to the Islands in August 1819.

“On the 5th of April 1819, the Uranie sailed from Guam; she cast anchor at Owhyhee, the largest of the Sandwich Islands, on the 8th of August: on the 16th she touched at Mowhee; on the 26th at Woahoo; and on the 30th, finally quitted that Archipelago for Port Jackson”. (Arago)

“It was on the 6th of August that we discovered the island of Owhyhee: we were only a short distance from it; and the land, which we expected to see of a prodigious height, appeared to us as of very moderate elevation.”

“An island which recalled so many unpleasant recollections, necessarily excited our attention; and every one fixed his eye on it. On a sudden, the thick clouds separating, which covered its regularly formed sides and enormous base; Mowna Kah stood, majestically before us ….”

“Karakakooa harbour is spacious and safe; the high mountains which protect it from the winds which blow most generally, namely, Cape Kovvrovva to the north, and Cape – to the south, prevent the sea from ever being very rough. The beach is good, and some buildings, and two considerably projecting piers, offer a secure shelter for shipping.”

“Kayerooa is the largest, most important, and most populous town of Owhyhee … The town of Kayerooa is of considerable extent; but the houses, or rather the huts, are at such distances from each other …”

“… particularly on the descent of the hill, as not to be at all connected with the part in the plain, in which there are some small beaten paths, which may pass as tolerable representations of streets and alleys.”

“There are some houses built of stone, cemented with mortar; the others are made of thin deals, with mats or leaves of palm-trees, closely tied together and made impenetrable to wind and rain.”

“The roofs are in general covered with sea-weed, which makes them wonderfully strong; while they are also very durable, owing to a few beams closely fitted and fastened with cords of the plantain tree.”

“The huts of Owhyhee appear to me the best that we have seen since we have been in these semi-barbarous regions. Almost the whole of them have only one apartment, ornamented with mats, calebashes, and some country cloths.”

“In that room fathers, mothers, boys, girls, and sometimes even hogs and dogs, all sleep together pele-mele: there the mothers offer their daughters to strangers; there the children learn, almost as soon as they are born, what they ought scarcely to know when they are grown up …”

“Two or three buildings, as seen from the roads (anchorage), have a good appearance, and make one rather regret that they are, as it were, solitary in the midst of ruins.”

“The most considerable is a storehouse distinguished by its white front from the other huts; it belongs to the King, who uses it as a sort of repository, without venturing to confide his treasures to its keeping; these he buries in cellars.”

“The second edifice is a morai, situated at the end of a jetty, projecting into the sea; the third is a house belonging to one of the principal chiefs of Riouriou, who had address enough, when he quitted the town, to get it consecrated (tabooed) in order to protect it from intruders and thieves.”

“I was given to understand, that whoever should endeavour to enter it, would be instantly put to death, and that the owner of the house was a very cruel and powerful man. The northern part of the town may perhaps consist of a hundred huts, most of which are only about three or four feet high, and six long ….”

“On reaching the shore, there is a large dock-yard directly opposite, in which a vessel was building, of forty tons burden. Near it are some sheds, which shelter from the rain and wind a prodigious number of canoes, both single and double, remarkably handsome and well finished.”

“They are made by means of an instrument called in this country toe, which may be compared to a carpenter’s adze, though much smaller, and fit to be used by one hand.”

“Our cabinet-makers do not polish the most costly furniture better; and without planes or any of the tools employed by our workmen, those of Owhyhee are capable of competing with the best artisans of Europe.”

“The inside of the bottom of their boats, as far as the thwarts, is painted black, and polished till it becomes very bright, by means of a yellow flower which is found all over the island.”

“The largest canoe was a single one, seventy-two feet long, and three in its greatest breadth. The threads with which the planks were sewed o=together and with which the other parts of the canoes and their outriggers were connected, were twisted and fastened with wonderful skill.”

“After visiting a great number of the houses of Kayerooa, where these people, whose existence is so monotonous and so peaceful, repose from their indolent toils, I directed my steps towards the Governor’s hut, as he had asked me to visit him.”

“It is small, but very clean, and tolerably well furnished; containing rather a handsome bed, two wicker chairs, some Indian cushions, and a great number of mats. …”

“The town of Kayerooa is situated at the foot of a high mountain which protects the anchorage from the North and North-West winds. From this mountain, particularly from the nearest declivity, the inhabitants derive the greater part of their subsistence.”

“It is really melancholy to see the extensive plain which surrounds it on both sides, uncultivated and despised. I cannot conceive how a people so characteristically idle and indifferent can neglect so fertile a spot, which would at once enrich and save them great fatigue and suffering …”

“… a few days’ labour would provide them subsistence for several months; and two years’ perseverance would secure to them for ever those valuable gifts, of which, on the summit of mountains, a violent storm or some other catastrophe may so easily deprive them. …”

“Our botanist, whose zeal augments with the difficulty and fatigue he encounters, has walked over the best part of the heights above the town.”

“He assures us, that vegetation was very powerful there, and that it would be very easy to conduct into the plain, by means of shallow canals, the waters which fertilize these summits, and are entirely lost to the inhabitants, whose means of subsistence are entirely derived from the lands which adjoin the sea. …”

“We left Owhyhee on the 15th of August, at four in the morning, with a very light breeze, which, however, freshened up during the morning.”

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Kamilo Beach

 

Kamilo Beach (milo tree; the twisting (of ocean currents) (Pukui)) on the Kaʻū coast of the Big Island of Hawaiʻi expectedly has a stand of milo trees. But that is not the only wood here.

Two places here were called Ka-milo-pae-aliʻi (Ka-milo landing (of) chiefs) and Ka-milo-pae-kānaka (Ka-milo landing (of) commoners.) Drowned commoners washed in at the latter, chiefs at the former.

Kaʻū people traveling to Puna cast lei tied with loincloths and pandanus clusters into the sea at Puna; when the lei drifted back to Ka-milo, the Kaʻū people knew that the travelers had reached Puna. (Pukui)

Native Hawaiians, seeking wood for dugout canoes, used to go to Kamilo Beach at the southernmost tip of the Big Island to collect enormous logs that had drifted from the Pacific Northwest. (LATimes)

True to its name, ocean currents, actually two currents – one coming up from South Point and the other coming down from Cape Kumukahi – combined with fierce onshore winds to make this rocky stretch of shoreline the final resting place for plenty of natural debris – it was known as a magnet for driftwood.

However “the strangest thing about Kamilo is that it’s covered with plastic trash — things that we use every day. I find shoes, combs, laundry baskets, Styrofoam, toothbrushes and countless water bottles.”

“There are even toys like LEGO blocks and a little green army man. Beneath the recognizable things are millions of tiny, colorful plastic pieces — the fragments of broken-down larger objects. They look like confetti.” (Marinez, ScienceNews)

This plastic sand is coming from all around the Pacific rim, swirling into a vortex which eventually brings it to these shores. This is the place where Hawaiians came to find bodies of people who were lost at sea. Nowadays, this beach is where we come to find what our throw-away society has done to the environment. (HawaiiNewswNow)

Algalita Research Foundation founder Charles Moore estimates that more than 90% of the trash on Hawai‘i beaches is not generated in the Islands. Kamilo Beach on the Big Island, gets the worst of the debris influx, with trash over a foot deep in some areas. (HonoluluMagazine)

“Our exploration brought us no answers but inspired more questions and speculations. We confirmed that some debris on Kamilo Beach has travelled in the Pacific subtropical gyre from far away East Asia and from the North American West Coast.” (Maximenko, IPRC)

“The current meters tell us that the waves and the tides provide the energy, pushing the debris to shore like a broom. The rather long shore break may contribute to debris accumulation.”

“But, we still need to understand the interaction between large-scale currents collecting debris from the entire North Pacific and the coastal dynamics that move the debris over the reef.” (Maximenko, IPRC)

Finds range from everyday items like shampoo bottles, combs and toothbrushes; fishing industry items like buoys, hagfish eel traps and glowsticks; mariculture leftovers like oyster spaces; children’s items like army toys; and a remarkable number of unidentifiable bits and pieces, broken fragments and resin pellets (aka “nurdles.”)

Some of the more interesting debris items include a full-size refrigerator with Japanese kanji, a military box with Soviet Union tags, and a select few glass floats made in Norway, Korea or Japan. (NPS)

Some debris is generated in Hawaiʻi. But much of the debris comes to Kamilo from much farther away. One piece of plastic had Japanese writing. Ropes were sprinkled with a species of barnacle found commonly in the Pacific Northwest. (CivilBeat)

Volunteers regularly pickup and dispose of the trash. Of the over 130-tons taken out, glass gets recycled, plastic garbage ends up in the landfill and old fishing nets are barged to Oʻahu, where they’re burned in H-POWER to provide some of Honolulu’s electricity. For every truckload of garbage that comes out, more comes in from the ocean. (Gilmartin, Hawaiʻi Wildlife Fund (HWF))

HWF co-founder Bill Gilmartin and colleagues estimate that approximately 15 – 20 tons of debris wash ashore here annually. About every other month, HWF coordinates a community-based cleanup effort at the “dirtiest” section of this coastline.

On average, they bag and remove about 3,600 lbs. of marine debris in a single day’s effort. By weight, about 62% (199,600 lbs.) of the total debris removed has been derelict fishing net bundles. (NPS)

The debris from the North Pacific Garbage Patch occasionally escapes and the model shows it floats towards the Hawaiian Islands, making windward shores of the islands trashcans for marine debris.

Kamilo Beach near South Point on the Big Island is arguably the most famous beach for the enormous amount of marine debris sweeping up on it. A BBC video labeled it as “The Dirtiest Beach in the World.” (iprc)

Lessons can be learned from HWF’s experience, and have been. Volunteers now see the relationship between beach litter and our own daily reliance on single-use, throw-away plastics.

Imagine if we each made a commitment to reduce the amount of single-use plastics we personally consume and dispose of on a daily basis; this would make a difference to the marine ecosystem. (NPS)

 

by Peter T Young 2 Comments

Hawaiʻi Preparatory Academy

Marines and Sailors trained for what has been referred to as the toughest marine offensive of WWII. 1,300 miles northeast of Guadalcanal, the Japanese had constructed a centralized stronghold force in a 20-island group called Tarawa in the Gilbert Islands.

The Marines would reconstitute at Camp Tarawa at Waimea, on the Island of Hawaiʻi.  Originally an Army camp named Camp Waimea, when the population in town was about 400, it became the largest Marine training facility in the Pacific following the battle of Tarawa.

Huge tent cities were built on Parker Ranch land; the public school and the hotel across the road from it were turned into a 400-bed hospital. At first the school children attended classes in garages and on lanais, but by fall of 1944, Waimea School was housed in new buildings built by Seabees on the property behind St. James’ church.

Over 50,000-servicemen trained there between 1942 and 1945; it closed in November 1945. The new roads, reservoirs and buildings were left to the town. The public school children returned to Waimea School, and the buildings behind St. James’ stood empty … but not for long.

At the end of World War II, the Right Reverend Harry S Kennedy arrived. He was a builder of congregations and of schools, and when he saw the empty buildings at St. James’, he immediately saw possibilities.

March 12, 1949, Bishop Kennedy and a group of local businessmen turned the buildings into a church-sponsored boarding school for boys, Hawaiʻi Episcopal Academy.  The Episcopal priest was both headmaster of the school and vicar of St. James’ Mission.

The early school struggled with facilities and financing. A turning point came in 1954, when James Monroe Taylor left Choate School in Connecticut to become HPA headmaster.

Three years later, substantial financial pledges came in and the church surrendered its direction to a new governing board. The school was then independently incorporated and the name changed to Hawai‘i Preparatory Academy.

In January 1958, the board of governors purchased 55-acres of land in the foothills mauka of the Kawaihae-Kohala junction and announced plans to build a campus there. Within a year, two dorms opened on the new campus and another was cut and moved from the town campus.

Old Air Force buses driven by faculty members made daily runs between the new campus, where boarders ate and slept, and the old campus, where classes were held. The last class to graduate on the town campus was the Class of 1959.

Honolulu architect Vladimir N Ossipoff was retained to design the campus buildings – five classroom buildings, two residence halls, a chapel, a library, an administration building and a dining commons.

In 1976, HPA acquired the buildings of the former Waimea Village Inn in town. Growing out of the “Little School” founded in 1958 by Mrs T to accommodate children of HPA faculty in the lower grades, the Village Campus today houses HPA’s Lower and Middle Schools, encompassing kindergarten through eighth grade.

In the 1980s, 30-acres of Parker Ranch land were added to the Upper Campus. Besides the Village Campus, the school added the Institute for English Studies and a campus in Kailua-Kona for grades K-5. (The Kona campus became the independent Hualālai Academy, but it closed effective May 30, 2014.)

Building projects expanding the HPA facilities included Atherton House, the headmaster’s residence, Gates Performing Arts Center, Dowsett Pool, Gerry Clark Art Center, Davenport Music Center, Kō Kākou Student Union, faculty housing and the Energy Lab.

Starting with five boarding students in a World War II building, today, there are 600 students (approximate annual enrollment) – 200 in Lower and Middle Schools (100% day students) – 400 in Upper School (50% day, 50% boarding) ; Boarding students: 60% U.S., 40% international.

HPA is fully accredited by the Western Association of Schools and Colleges and is a member of 12 educational organizations including the Council for the Advancement and Support of Education, College Entrance Examination Board, Council for Spiritual and Ethical Education, Cum Laude Society, National Association of College Admission Counselors, Hawaii Association of Independent Schools, and National Association of Independent Schools.  (Information here from HPA and St James.)

I am one of the fortunate boys-turned-to-young-men under the leadership and guidance of headmaster Jim Taylor.

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