Hawaii | Page 377 | Images of Old Hawaiʻi

November 2, 2018 by Peter T Young Leave a Comment

Pineapple Pier

Although sugarcane was ‘king’ in Hawai‘i, untilled government land was in pasture rather than sugarcane because it was too dry for unirrigated sugarcane and the elevation was too high for irrigated cane.

Several events occurred in 1898 that facilitated the development of the new pineapple canning industry. First, the annexation of Hawaii in that year resulted in the revocation of the 35% duty on Hawaiian canned pineapple.

Second, the Republic of Hawaii legislature passed a law that made some 1,300-acres of government land near Wahiawa available for homesteading once a pasture lease expired (13 southern California families came to Wahiawa to homestead the land made available under the new law.)

These early migrants and James Dole, who arrived in 1899, formed the nucleus of what would eventually become the largest pineapple industry in the world. (Bartholomew et al)

Homesteaders cleared land, built homes, and at first planted food and fodder crops. Byron O. Clark had obtained a small pineapple farm planted with ‘Smooth Cayenne’ plants near Pearl City in 1898 before the prospective homesteaders had left California.

Clark’s farm provided the first pineapple plants grown on the homesteaded lands near Wahiawa and they grew so well that other homesteaders followed suit. James Dole established the Hawaiian Pineapple Company in 1901 and is “usually considered to have produced the first commercial pack of 1,893 cases of canned pineapple in 1903”.

The pineapple plantation concept quickly spread to Kauai and Maui, perhaps because the already well-established sugar industry provided the near-ideal plantation model for those to whom it was not initially obvious. (Bartholomew et al)

In the early 1900s, to help with the burgeoning plantation population, government lands were auctioned off as town lots in Kapa‘a.

The first pineapple company on the island of Kauai was established in 1906. In 1913, Hawaiian Canneries Company, Ltd opened in Kapa‘a at the site now occupied by Pono Kai Resort. Through the Hawaiian Organic Act, Hawaiian Canneries purchased land they were leasing, approximately 8.75 acres, in 1923.

A 1923 sketch of the cannery shows only four structures, one very large structure assumed to be the actual cannery and three small structures makai of the cannery. (Bartholomew etal)

On August 21, 1929, a US trademark registration was filed for ‘Pono’ by Hawaiian Canneries. The description provided to the trademark for Pono is ‘canned sliced and crushed pineapple and pineapple juice used for food-flavoring purposes’. (Trademarkia)

By 1956, the cannery was producing 1.5 million cases of pineapple. By 1960, 3,400 acres were in pineapple and there were 250 full time employees and 1,000 seasonal employees. (Exploration)

Until the 1960s, the Hawaiian Canneries canning plant used to produce canned sliced and crushed pineapple and pineapple juice used for food-flavoring purposes.

Factory by-products – the crowns & skins from the processed pineapples – were loaded onto train carts and hauled up the coast to a pier. The pineapple rubbish was then dumped into the ocean from the end of the pier. (Kauai Path)

As canned pineapple from other countries began filling the market, Hawaiian canneries began to close and plantations, once located on Maui, Oahu, Molokai, Lanai, and Kauai, began to shrink.

In 1962, Hawaiian Canneries went out of business due to foreign competition. (Exploration) Other smaller Kauai and Maui pineapple companies closed in the late-1960s.

In 1969, Hawaiian Fruit Packers (which was formed in 1937 by the reorganization of a company initially started by a group of ethnic Japanese growers) on Kauai, the last cannery remaining there, announced plans to cease planting. The cannery was closed in Oct. 1973. (Bartholomew etal)

Del Monte cannery closed in 1985, and Dole cannery in Iwilei closed in 1991. The Kahului cannery of Maui Land and Pineapple Company was the last remaining pineapple cannery in Hawai‘i. During the end of the 1990s and into the 21st century the value of fresh Hawaiian pineapple overtook the value of canned Hawaiian pineapple.

The Hawaiian pineapple industry has gone from its early days as a primarily fresh product, through most of the 20th century as principally a canned product and a major supplier of the worlds canned pineapple market, to the 21st century when it is once again grown mostly for fresh consumption. (HAER)

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Pineapple Dump Pier

Pono Pineapple

Pono – Hawaiian Canneries Company, Ltd

Hawaiian_Canneries (Kapaa)-Sanborn Fire Map

Sugar_Plantation-Fire_maps-Index-Kauai-Oahu-Hawaiian Canneries Company, Ltd-noted

November 1, 2018 by Peter T Young Leave a Comment

The Islands in 1856

“On Owhyhee, two enormous mountains rise to 14,000 feet above the level of the sea, and rest crowned with perpetual snow. Many craters of extinct volcanoes, and extensive plains covered with the rude debris of earlier or later eruptions, exist everywhere; and Kilauea, on the mountain of Mouna Kea, is the largest active volcano in the known world.”

“In a country thus formed, and, doubtless, at a date comparatively so recent, we cannot be surprised that no metals have been found, and no minerals save the varieties of the lava, and some limestone which has been lately discovered lying in a remarkable and raised bed at Kahuku, in the island of Woahoo.”

“In this island there is also a salt-lake, a little elevated above the surface of the sea. Soils formed of such materials as those which thus compose the entire bed of the islands, could not be expected to be very fertile, save upon some of the lower or little elevated lands, and in the valleys long formed in situations exposed to the winter rains.”

“The climate generally of the islands is remarkable for its salubrity and its even temperature. Near the sea, the highest elevation of the thermometer is 86° Fahrenheit, and the lowest 62°. The greatest heat occurs during the month of July, and the least in January.”

“Thus the extreme range during the year, does not exceed 24°, but the variation is rarely more than 8°. The inhabitants may, however, by ascending to the higher lands, live in any temperature between that of these tropical latitudes and that of the frigid zone.”

“But, notwithstanding the general healthiness of the climate, at the time that the trade-winds are irregular, which happens during the winter months …”

“… when the wind is commonly from the south, rains and storms occur, attended by diseases not differing much from those which prevail in the southern parts of Europe, at the same season — such as headaches, rheumatism, and others, arising from imprudent exposure to the night air, in damp and chilly weather.”

“According to the reports of naturalists who have visited the islands, the spontaneous productions of their soil are much more varied than the evidently recent formation of the group would lead us to expect. It will suffice to mention, that those of the family of Rubiaceae, Con tor tee, and Urticae, predominate.”

“From the last of these, as well as from the Broussonetia papyrifera, or the paper mulberry, are made cordage and cloths. The acacia also abounds in the mountain districts, and is employed by the natives in the construction of their canoes.”

“The sandal-wood was also once very abundant, and lately afforded an article of commerce with the Chinese, by whom it is chiefly used for cabinet purposes. It is now, however, save some young, and, for the present, useless trees, quite destroyed.”

“The more familiar plants and useful productions for domestic purposes are, the banana-tree, the sugar-cane, the yam, the bread-fruit, and the taro-root (Arum esculentum), all of which are indigenous.”

“Such were these islands after they first raised their towering heads above the waters of the mighty ocean which surrounds them, and such the earliest productions of the vegetable world which sprung from the soil first formed.”

“Several important plants have been lately introduced, such as the coffee, cotton, rice, tobacco, the melon and water-melon, indigo, and even the vine, of which, however, though it flourishes in the mountain districts, little use is likely to be made, on account of the necessity of discouraging the growth of everything from which alcohol may be distilled.”

“Several of our ordinary vegetables have also been introduced with success, as well as some of the fruits of the tropical and temperate latitudes which were not indigenous, such as pine-apples, oranges, grapes, peaches, figs, tamarinds, and guavas. The bread-corns will also flourish on the higher lands.”

“With respect to the animal kingdom, it seems that at the discovery of the islands nothing was observed save hogs and dogs, the importation, without doubt, of the first inhabitants, and such of Nature’s earlier productions as may be considered habitants rather of the sea than of the land …”

“… but all our domestic animals, including such as we use for food, for beasts of burden, and for companions of our sports, have been since introduced.” (All here is from Hill.)

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Hawaiian Islands from Hill-1856

October 30, 2018 by Peter T Young Leave a Comment

The Lost Battalion

The War Department announced that it was forming an all-Nisei combat team. (Nisei are the second-generation Japanese in Hawaiʻi and the first generation of Japanese descent to be born and receive their entire education in America, learning Western values and holding US citizenship).

The call for volunteers for the 442nd Regimental Combat Team was made. The Territory of Hawaiʻi raised a total of 10,000-volunteers and so its quota was increased to 2,900 while the mainland quota was lowered proportionately to 1,500.

The 442nd Regimental Combat Team was activated on February 1, 1943 at Camp Shelby Mississippi; the Honolulu Chamber of Commerce held a Farewell Ceremony for Hawaiʻi 442nd soldiers on March 28, 1943, at ʻIolani Palace. By April 1943, the recruits arrived for training at Camp Shelby, Mississippi. Following their training, on April 22, 1944, the 442d packed up and were bound for Europe.

As the soldiers of the 36th Infantry Division, including the 100th/442nd Regimental Combat Team (RCT), pushed toward Germany in late-1944, they faced some of their heaviest resistance and harshest terrain in the Vosges Mountains of eastern France.

“It was in this dense forest and mountainous landscape that the 1st Battalion of the 141st Regiment, 36th Division, became ‘The Lost Battalion.’”

“On the front lines of the Allied assault, Major General John E. Dahlquist, commander of the 36th Division, pushed the unit – which was made up primarily of soldiers from Texas – forward to liberate more French territory.”

“The men of the 141st moved quickly through the trees taking advantage of significant gains made by the Allies during the previous days and weeks of fighting.”

“In their haste to recapture more territory, they unknowingly separated themselves from their fellow soldiers and became surrounded by German units.”

“The 1st Battalion, under the leadership of Lt. Marty Higgins, lost contact with headquarters and the 2nd and 3rd Battalions made little headway in their attempts to reach their comrades.”

“Members of the 405th Fighter Squadron of the 371st Fighter Group dropped supplies and food to the men, but as temperatures fell, rations decreased and the wounded deteriorated; the situation grew desperate for the men of the 1st Battalion.”

“Members of the 1st Battalion of 141st Texas Regiment found themselves cut off and surrounded behind enemy lines with limited food and water.”

“General Dahlquist recalled the Japanese American soldiers of the 100th /442nd RCT from their rest behind the lines and they attempted to reach the surrounded unit, slogging through rain and mud for miles towards the Texans.”

“The 100th Infantry and the 2nd and 3rd Battalions of the 442nd RCT fought diligently for five days with the help of the 522nd Field Artillery Battalion to break through or surround the Germans who entrapped the Texans.”

“Pvt. George Sakato reported that the lines were often so close that when the American artillery was active, ‘we jumped into any hole that was open to keep from getting hit.’”

“Members of their Antitank units joined in the effort as did soldiers from the 232nd Combat Engineer Company, all of whom hoped to break the stalemate that encircled the men of the 36th.”

“Despite their best efforts and teamwork, the fighting was difficult, forcing the Nisei to fight tenaciously for every yard of ground gained. The men would later learn that Adolf Hitler himself had heard of the trapped unit and ordered that they not be rescued no matter what the cost on the German side.” (Grubb)

“Moving quickly, the 3d and 100th Battalions pushed off from Belmont in pitch darkness at 0400, 27 October. By 1000 hours they had passed through the remainder of the 141st, which had been trying to break through to its besieged troops. The 442d launched its attack, battalions abreast, with the 100th on the right.”

“Progress was slow on the 27th. The terrain was next to impossible, heavily forested and carpeted with a dense growth of underbrush. Fighting went back to the days of America’s Indian wars; every tree and every bush were carefully investigated before the troops passed on.” (442)

“Ordered to rescue them, the 100th/442nd RCT, engaged in nearly nonstop combat for six days, eventually reaching the Lost Battalion on October 30. The 442nd suffered hundreds of casualties in rescuing 211 men.”

“Finally, six days after the Texans were surrounded, the Nisei approached from two sides, pushed back the German troops, and drew near the Lost Battalion.”

“At some points during the battle the Nisei had been outnumbered by as many as four to one; one particular hill that witnessed a fierce bayonet charge led by Private Barney Hajiro came to be known as ‘Suicide Hill’ due to the casualty rate of the advancing troops.”

“According to Pfc. Ichigi Kashiwagi of K Company, ‘We yelled our heads off and charged and shot the head off everything that moved… we didn’t care anymore… we acted like a bunch of savages.’”

“Companies I and K of the 3rd Battalion emerged with only seventeen and eight infantrymen respectively and both were led by sergeants because all higher ranking officers and non-commissioned officers had been killed or wounded.”

“Following the strenuous hand-to-hand combat of October 29 and an artillery bombardment the morning of October 30, the battles finally eased for the 100th/442nd RCT, but the situation was still tense for the trapped Texans.”

“As the rescuers came closer, the German artillery focused more on the Lost Battalion itself, which was already lacking supplies and losing soldiers every day. By midafternoon the Nisei were able to penetrate the German lines and caught sight of soldiers in American uniforms.”

“In what has become a famous exchange, Mutt Sakumoto, the first Japanese American to reach the trapped soldiers, offered a cigarette to the men of the 36th when he found them. Ed Guy, one of the rescued soldiers recalled, ‘I might have hugged [Sakumoto], I don’t know… I was just excited to get out of there.’” (Grubb)

“On the 30th, although the back of the German resistance had been broken and infantry action was sporadic, the artillery kept pouring in.”

“Finally, at 1500 hours that day, with the 3d and 100th Battalions moving as much abreast as possible, a patrol from I Company, led by Technical Sergeant Takeo Senzaki, made contact with the ‘Lost Battalion.’ Shortly thereafter, the main bodies linked up.”

“The impossible had been accomplished.” (442)

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442nd taking part in rescuing the Lost Battalion

October 29, 2018 by Peter T Young 1 Comment

Palaoa

O kane ia Waiʻoloi, O ka wahine ia Waiʻololā
Hanau ka Palaoa noho i kai
Kiaʻi ia e ka ʻAoa noho i uka

Male the narrow waters, female for the broad waters
Born is the Palaoa (whale) living in the ocean
Guarded by the ʻAoa (sandlewood) that grew in the forest

O ke kaʻina a palaoa e kaʻi nei
E kuwili O haʻahaʻa i ka moana

The procession of whales leading forward
To spin to the depths of the sea.
(Kumulipo)

The Hawaiian Chant of Creation, known as the Kumulipo, is a genealogical creation chant composed in Hawaii for the chief, Ka-’I-i-mamao, about the eighteenth century, comprising more than 2,000 lines.

It contains 2,000 names representing 812 generations the sum of linear time in that history is about 22,300 years, or roughly one precession of the equinoxes dating back to around 21,000 BC. (Rubellite Kawena Kinney Johnson)

The koholā or whale was formerly called the palaoa. (Malo) “The whale is the largest ocean creature and a majestic manifestation of Kanaloa.

From the ivory of this creature. The highly prized ‘Palaoa’ or whale-tooth pendant is carved. This palaoa was only worn by ali‘i of highest rank.” (Kanahele)

The scarcity of the palaoa and its connection to Kanaloa brought mana to the carver, to the pendant itself and eventually to the wearer of the pendant.

The aliʻi who possessed this kinolau or body form of the great God would himself/herself acquire the characteristics, intelligence and knowledge of the God. Therefore it would be advantageous for any aliʻi to secure the ivory whale-tooth of this Kanaloa body form. (KIRC)

In the ocean, outside lay a belt called kai-kohola, where swim the whales, monsters of the sea; beyond this lay the deep ocean, moana.

If any large fish – such as a whale – or a log strapped with iron, should be cast ashore, it was to be offered to the gods, (ie, it was to be given to the priests for the use of the king). The whale was not taken by Hawaiian fishermen. (Malo)

The whale species hunted in the 19th century were primarily the North Pacific right, the humpback, the fin and the gray whale; they also caught blue and sperm whale. The right and humpback are baleen species; rather than teeth, baleen plates filter food from water.

Whaling was an integral part of the development of many countries in the early nineteenth century. Whale blubber produced oil that lit the lamps and greased the machines of many of the most “modern” inventions of the time. It was said that whale oil was the illumination and lubrication of the Industrial Revolution. (Bishop Museum)

As the traditional hunting grounds of the Atlantic began to be fished out, whalers turned to the plentiful waters of the Pacific. Some of the most bountiful harvesting grounds were found off the coast of Japan.

Japan’s ports however, were closed to foreign vessels; Hawai‘i became a perfect destination for these whaling fleets needing a place to dock, replenish supplies, repair the ships and rest the crews,.

Whalers began arriving in Hawai‘i in 1819, and by 1822 over sixty ships were docking annually. Honolulu, Lāhainā and Kōloa were the primary anchorage areas for the whalers. By 1846, the number of whaling ships arriving in Hawai‘i had reached 596-ships.

The sailors, and their ships needed supplies, food, tools, liquor and many more commodities that often newly arrived “businessmen” were ready to supply. Hawai‘i became a “gold rush” town that attracted people of all types.

Some of the most influential businesses in modern Hawaiian history got their start from the capitalist opportunities of this period. Hawai‘i also saw the loss of young Hawaiian men who traveled aboard these ships to the northwest coast of America and other destinations. (Bishop Museum)

The whale at Bishop Museum, unlike those that were caught for their oil, is actually a sperm whale. It was the first specimen installed in Hawaiian Hall in December of 1901 and has hung there ever since. It is over 55 feet long and weighs over two tons. (Bishop Museum)

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WLA_haa_Lei_Niho_Palaoa_Neck_Ornament-Carved sperm whale tooth, braided human hair, olona cordage

October 28, 2018 by Peter T Young 2 Comments

Koʻolau Volcano

O‘ahu used to be nearly twice as big as it is now. (Thompson) The Island consists of two major shield volcanoes: Waiʻanae and Koʻolau; the eroded remnants of which are the Waiʻanae Range and the Koʻolau Range.

Waiʻanae is the older of the two (breaking the ocean surface ~3.9 to ~2.8 million-years ago) and makes up the western part of O‘ahu. Koʻolau volcano started as a seamount above the Hawaiian hotspot around 4-million years ago. It broke sea level some time prior to 2.9-million years ago.

Koʻolaupoko, one of O‘ahu’s six ancient moku (districts,) is bounded by Kalaeoka‘ō‘io, which is a point near the center of the northeast coast at Kualoa; the crest of the Koʻolau Range to the west; and Makapuʻu Point on the southeastern tip of the island.

This expanse also generally delineates the extent of Koʻolau Volcano – effectively from and including Kāne‘ohe to Kailua to Waimānalo. A significant landslide and ongoing erosion reshaped the volcano.

About 2-million years ago, much of the northeast flank of Koʻolau volcano was sheared off and material was swept onto the ocean floor (named the Nuʻuanu Avalanche) – one of the largest landslides on Earth.

The Pali is the remaining edge of the giant basin, or caldera, formed by the volcano. At its base are the towns of Kāne’ohe, Kailua and Waimānalo – beyond that, open ocean. The other half of the caldera, an area the size of Brooklyn, tore away and tumbled into the ocean. (Sullivan)

Material swept more than 140-miles north of O‘ahu and Molokai. For the last 85-miles of its journey, the avalanche traveled uphill by about 1000 feet, leaving jumbled blocks – once part of O‘ahu – scattered over more than 9,000-square miles of seafloor. (Sinton)

Residual ridges, remnants of the old Koʻolau volcano, extend northeast from the Pali. These include the Mokulua islands, Olomana, Kapaʻa (where the quarry is,) Mahinui (Oneawa, Kalaheo) and Keolu Hills.

Mōkapu Peninsula (where Marine Corps Base Hawai‘i is situated) is evidence of subsequent secondary volcanic eruptions that formed Ulupaʻu Crater (the large hill on the Kailua side of the peninsula,) Pu‘u Hawaiiloa (the central hill that originally had the base control tower, now has radar (‘the hill’,)) Pyramid Rock and the nearby Moku Manu (Bird Island.)

Following a period of dormancy, Koʻolau erupted about 1-million years ago (known as the Honolulu Volcanic Series) and created landmarks such as Lēʻahi (Diamond Head,) Hanauma Bay, Pūowaina (Punchbowl Crater) and Āliapaʻakai (Salt Lake.) Another tuff cone is Mānana Island (Rabbit Island.)

Pounded by the tradewind and rains, the windward side of O‘ahu is more weathered than the leeward areas of the island, and now this vast caldera wall is reduced to a line of sheer cliffs stretching from Makapuʻu to Kualoa and beyond.

The flat valley floors are extensively eroded, and are now mostly joined, studded here and there with isolated remnant peaks and ridges connected to the central range. (Klieger)

Coral reefs and marine terraces were formed at different elevations due to the changing sea levels over time. There are some broad lowland areas in the lower reaches of deeply alluvial valleys. (Moberly)

It was the broadness of this coastal plain (which included swampy areas near the shore) that distinguished Koʻolaupoko from other areas of O‘ahu, and most likely helped account for the intensity and productiveness of agriculture.

The abundant rainfall produces constantly flowing streams that supported the vast expanse of wetland kalo (taro) lo‘i (pondfields) that once extended throughout Koʻolaupoko. (Klieger)

Because Kāne’ohe Bay has a deep lagoon between an outer reef and the shore, the reef is considered by some geologists to be a barrier reef, the only example in Hawaii. Several fishponds lined the bay.

Mokoliʻi (Chinaman’s Hat) and Mokuoloe (Coconut Island) are erosional remnants of the bedrock Koʻolau basalt; Kapapa and Kekepa (Turtleback) Islands are of limestone; and Ahu O Laka Island is a sand bar that is uncovered at low tide. (Moberly)

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