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April 16, 2023 by Peter T Young Leave a Comment

St Peter’s Chapel

“There are a few, very small fishing villages, Alae, Alika and Papa, which are reached by poor trails from the mauka road. It is necessary to travel from Hookena mauka to the main road to Papa, and thence by either road or trail to Hoopuloa, the last steamship landing in Kona.”

“This is another village which is dwindling in population, only a few Hawaiians and a couple of Chinese storekeepers remaining. A fair road leads across a barren a-a flow to Miloli‘i, the largest and best specimen of an exclusively Hawaiian village on the Island, which is seldom visited.”

“It is splendidly situated by a sand beach, the sea coming right up to the yard wall, and is inhabited by a rather large population of Hawaiians, who prosper through the fishing which is almost phenomenally good…”

“This region is seldom visited. Its chief points of interest are the remains of a heiau, mauka of the Catholic church at Milolii, some fine papa konane at the south end of the same village a well preserved kuula (still used) where fishermen offer offerings of fruit to insure a good catch, by the beach south of Milolii, where the Honomalino Ranch fence crosses the trail; while all along the trail are smaller kuulas, and at many points the foundations of villages, where old implements may still be found.” (Kinney, 1913)

“Hoopuloa was one of the few typically Hawaiian villages remaining in Hawaii. It comprised of a cluster of 10 to 15 homes of old Hawaiian style and boasted a population of approximately 100 persons … The wharf was a port of call for the Inter-Island steamers”. (Honolulu Star Bulletin, April 19, 1926)

Then … “The number of earthquakes recorded for April [1926] was 671 (compared with monthly average of 52 for the preceding 3 months. … The maximum daily frequency of earthquakes in the 1926 eruption was on April 15 (86 shock), the first day of free-flowing flank eruption …” (Jaggar)

Edward G Wingate, USGS topographical engineer, was mapping the summit of Mauna Loa in 1926, changing campsites as the work progressed. On April 10 his camp was along the 11,400-foot elevation, well into the desolate upland above the Kau District.

An earthquake wakened the campers about 0145; as they drifted back to sleep, a further series of quakes had them sitting up, talking, and wondering. About 0330 Wingate braved the cold and wind; with a blanket wrapped around him, he went outside and stood bathed in reddish light.  (USGS)

There was a brief summit eruption, followed by 14 days of eruption on the southwest rift zone.  “About 3 am April 10 (1926,) glowing lava spouted along the upper 3 miles of cones and pits of the Mauna Loa rift belt, immediately south of Mokuʻāweoweo, the summit crater.  … The actual beginning shown at Kilauea by seismographic tremor was 1:36 am, followed by two pronounced earthquakes.”    (Jaggar)

For three days the HVO party surveyed the sources of the eruption; then they descended and moved into Kona District, where roads, houses, and other property were threatened by the flows. Wingate and his crew stayed behind. Much of the area already mapped was under fresh lava, and there was a lot of remapping to do.  (USGS)

“A crack only 1 to 3 feet wide opened southward from a point tangent to the ease edge of the bottom of the south pit of Mokuʻāweoweo, vomited out pumiceous silvery pāhoehoe froth lava, and extended itself S.30oW. past the next two pits and over the brow of the mountain down to an elevation of 12,400 feet.”  (Jaggar)

“Fortunately the main gushing of this first phase ceased about 5 am the same forenoon, after flowing 5 hours. … (Then,) The vent crack was splitting itself open downhill. The source pāhoehoe changed itself by stirring into scoriaceous aa half a mile from the vents”. (Jaggar)

“When it got close to the upland of Hoʻopuloa, the flow of lava separated into two, and one of the flows went straight for the village of Hoʻopuloa and the harbor, and the second flow went towards the village of Miloliʻi.”  (Hoku o Hawaii, April 20, 1926)  

“(T)he Honomalino flow to the west finally dominated, … This was also aa. … It crossed the belt road at 12:22 pm April 16, 3 miles above Hoʻopuloa village.” (Jaggar)

On April 16, Jaggar scratched marks about a foot apart across the rutted, gravel road (the only road) between the Kona and Kau Districts. A lava flow was approaching, and Jaggar wanted to measure the flow’s speed as it crossed the road.

St Peter’s Chapel, sometimes referred to as Ho‘opuloa Catholic Church, was on the makai side of the road.  Perhaps a hundred people were waiting around the Hoʻopuloa Church, on the uphill side of the road, and at the Kana‘ana house opposite, on the downhill side of the road.

They had seen and heard the flow, 15-20 feet high and more than 500 feet wide, as it moved through the forest uphill.  When it neared the road, people who lived on the Kona side of the flow moved off to the north, and those who lived on the Ka‘u side moved to the south, so they could go home after the road was closed.  (USGS)

Jaggar recorded that it reached the uphill, inland side of the road at 12:22 at an estimated speed of about 7 feet/minute; within two minutes the road was crossed. Jaggar and his assistant, HS Palmer, stayed on the Ka‘u side.  (USGS)  St Peter’s Chapel, sometimes referred to as Ho‘opuloa Catholic Church, was on the makai side of the road.

“The Catholic church, where many Hawaiians worshipped, was one of the first building to be destroyed in the flow which buried Hoopuloa.”  (The Star, NZ, May 21, 1926)

“It is true that I saw the church destroyed by the lava tide, which moved onward with irrevocable majesty, entering the house of worship by way of the open front door.”

“Through the windows I observed the red mass proceed to the alter as the whole structure, capable of seating 20 worshipers, burst into flames.”

“Most dramatic of all was the moment when the slow moving red-hot deluge, pressed on by the mass of lava from the rear, tipped the church from its foundations and set it careening upon the molten river.”

“Straightaway, the bell, which hung in an open steeple, began ringing. It pealed above the roar of the flames and the grinding of the blazing substance surging onward.”

“A dozen doleful strokes of the iron tongue echoed farewell before it fell from the cross beam ringing its own requiem.”  (Father Eugene Oehman, Honolulu Advertiser, July 31, 1932)

A memorial to the church was erected; the plaque on the monument reads “1926 Hoopuloa Catholic Church.” “Under the cross, 25 feet below the surface is all that remains of a small Catholic church, over which the lava flowed without a moment’s halt.” (Honolulu Advertiser, July 31, 1932)

“The fiery lava engulfed the harbor and village of Hoʻopuloa, and now they are but a heap of pāhoehoe lava.” (Hoku o Hawaii, April 20, 1926)

“Families of Ho‘opuloa were forced out of their homes by the flow, and many eventually settles in Miloli‘i on state land.  The displace families remained on the land although they had no legal title to the property.” (Hawaii Tribune Herald, July 10, 1985)

In 1932, St. Peter’s Catholic Church at Miloli‘i was built by Father Steffen to replace an earlier St. Peterʻs destroyed by the 1926 lava flow. (PaaPonoMilolii)

In 1982, the State Legislature passed Act 62 which designated 52.6 acres of state land to be leased to the refugees and the descendants of the Ho‘opuloa lava flow.”

The Act also created the criteria by which people could qualify fo5 65-year leases”  Initial implementation of the Act took place July 12, 1985 with the signing of 12 long-term leases for families living on the designated property.  (Hawaii Tribune Herald, July 10, 1985)

© 2023 Ho‘okuleana LLC

Filed Under: General, Missionaries / Churches / Religious Buildings Tagged With: Hawaii, Eruption, Mauna Loa, Hoopuloa, South Kona, St Peter's Chapel, Hoopuloa Catholic Church, 1926

April 15, 2023 by Peter T Young Leave a Comment

Wind, Wings and Waves

Hawaiʻi is the world’s most-isolated, populated-place, we are about: 2,500-miles from the US mainland, Samoa & Alaska; 4,000-miles from Tokyo, New Zealand & Guam, and 5,000-miles from Australia, the Philippines & Korea.
 
We are surrounded by a vast ocean and sometimes naively feel isolated, separated and protected from outside threats and negative impacts.  Unfortunately, we take too much for granted.
 
Formation of Hawaiian Island chain started more than 70 million years ago.  Yet despite millions of years of isolation, plants, animals and insects found their way to Hawaiʻi … on Wind, Wings and Waves.
 
Some seeds, spores and insects arrived on the wind.  A few birds flew or were blown off course; in them or stuck to their feathers were more seeds.  Some seeds managed to float here on ocean currents or waves.  Ocean currents also carried larval forms of fish, invertebrates, algae and even our freshwater stream species.
 
It is estimated that one plant or animal arrived and successfully colonized every 30,000 years.  Over millions of years in isolation, these original plant and animal species changed, forming into our native species.
 
The first alien species arrived with Polynesians in the year 300 A.D. or so. In 1778, Hawaiʻi was placed on the world map; and so started new invasive species pathways.
 
It is estimated that in the last 230+ years, as many as 10,000 plants have been introduced: 343 new marine/brackish water species; Hawaiʻi went from 0 native land reptiles to 40; 0 amphibians to 6 (including coqui) and there is a new insect in Hawaiʻi every day.
 
The greatest threat to Hawaiʻi’s native species is invasive species.
 
Hawaiʻi has the dubious distinction of being called the endangered species capital of the world and unfortunately leads the nation in endangered species listings with 354 federally listed threatened or endangered listed species.
 
With only 0.2% of the land area of the United States, nearly 75% of the nation’s historically documented plant and bird extinctions are from Hawaiʻi.  We have more endangered species per square mile on these islands than any other place on Earth.
 
Impacts from invasive species are real and diverse: Tourism and agriculture-based economy; Forests’ ability to channel rainwater into our watersheds; Survival of native species found nowhere else; Health of residents and visitors; and Quality of life that makes Hawaiʻi a special place.
 
Today, the pathways to paradise are diverse, including: air & ship cargo; ship hulls & ballast water; hand-carry/luggage; mail & freight forwarders; forestry activities; horticulture trade; aquaculture; pet trade; botanical gardens and agriculture experiment stations (or simply on you and your clothing.)
 
While I was at DLNR, we formed and I co-chaired the Hawai‘i Invasive Species Council, a multi-jurisdictional agency, established to provide policy level direction, coordination, and planning among state departments, federal agencies, and international and local initiatives.
 
Our focus was primarily on two actions: the control and eradication of harmful invasive species infestations throughout the State; and prevention the introduction of other invasive species that may be potentially harmful.
 
We must continue to be vigilant in stopping new pests from coming in and eradicating those that have already made it to our shores.
 
We share a common goal.  Whether your concern is in having enough water, healthy reefs, diverse forests, a healthy economy or a healthy family, we all want the same thing:  To make and keep Hawaiʻi a great place to live.
 
© 2023 Ho‘okuleana LLC
 

Filed Under: General Tagged With: Hawaii Invasive Species Council, Hawaii, Invasive Species, Native Species, HISC

April 12, 2023 by Peter T Young 1 Comment

Threes and Eights

No, it’s not a typo (I don’t mean black Aces and Eights, Wild Bill Hickock’s “dead man’s hand”;) this relates to Noah Webster, Henry ʻŌpūkahaʻia, and Hawaiian grammar and spelling.

How in the world are these in common? … Let’s look.

Noah Webster (1758-1843) was the man of words in early 19th-century America. He compiled a dictionary which became the standard for American English; he also compiled The American Spelling Book, which was the basic textbook for young readers in early 19th-century America.

ʻŌpūkahaʻia, in 1809, boarded a sailing ship anchored in Kealakekua Bay and sailed to the continent.  ʻŌpūkahaʻia latched upon the Christian religion, converted to Christianity in 1815 and studied at the Foreign Mission School in Cornwall, Connecticut (founded in 1817) – he wanted to become a missionary and teach the Christian faith to people back home in Hawaiʻi.

A story of his life was written (“Memoirs of Henry Obookiah” (the spelling of his name prior to establishment of the formal Hawaiian alphabet, based on its sound.))  This book was put together by Edwin Dwight (after ʻŌpūkahaʻia died.)  It was an edited collection of ʻŌpūkahaʻia’s letters and journals/diaries.

This book inspired the New England missionaries to volunteer to carry his message to the Sandwich Islands.

On October 23, 1819, the pioneer Company of missionaries from the northeast United States, set sail on the Thaddeus for the Sandwich Islands (now known as Hawai‘i) – they first landed at Kailua-Kona on April 4, 1820.  (Unfortunately, ʻŌpūkahaʻia died suddenly (of typhus fever on February 17, 1818) and never made it back to Hawaiʻi.)

OK, so what about the 3s and 8s – and Hawaiian grammar and spelling?

It turns out that a manuscript was found among Queen Emma’s private papers (titled, “A Short Elementary Grammar of the Owhihe Language;”) a note written on the manuscript said, “Believed to be Obookiah’s grammar”.

Some believe this manuscript is the first grammar book on the Hawaiian language. However, when reading the document, many of the words are not recognizable.  Here’s a sampling of a few of the words: 3-o-le; k3-n3-k3; l8-n3 and; 8-8-k8.

No these aren’t typos, either.  … Let’s look a little closer.

In his journal, ʻŌpūkahaʻia first mentions grammar in his account of the summer of 1813: “A part of the time [I] was trying to translate a few verses of the Scriptures into my own language, and in making a kind of spelling-book, taking the English alphabet and giving different names and different sounds. I spent time in making a kind of spelling-book, dictionary, grammar.”  (Schutz)

So, where does Noah Webster fit into this picture?

As initially noted, Webster’s works were the standard for American English.  References to his “Spelling” book appear in the accounts by folks at the New England mission school.

As you know, English letters have different sounds for the same letter.  For instance, the letter “a” has a different sound when used in words like: late, hall and father.

Noah Webster devised a method to help differentiate between the sounds and assigned numbers to various letter sounds – and used these in his Speller.  (Webster did not substitute the numbers corresponding to a letter’s sound into words in his spelling or dictionary book; it was used as an explanation of the difference in the sounds of letters.)

The following is a chart for some of the letters related to the numbers assigned, depending on the sound they represent.

Long Vowels in English (Webster)
..1……..2…….3………4……….5…….6………7……….8
..a……..a…….a………e……….i……..o………o……….u
late, ask, hall, here, sight, note, move, truth

Using ʻŌpūkahaʻia’s odd-looking words mentioned above, we can decipher what they represent by substituting the code and pronounce the words accordingly (for the “3,” substitute with “a”(that sounds like “hall”) and replace the “8” with “u,” (that sounds like “truth”) – so, 3-o-le transforms to ʻaʻole (no;) k3-n3-k3 transforms to kanaka (man;); l8-n3 transforms to luna (upper) and 8-8-k8 transforms to ʻuʻuku (small.)

It seems Henry ʻŌpūkahaʻia used Webster’s Speller in his writings and substituted the numbers assigned to the various sounds and incorporated them into the words of his grammar book (essentially putting the corresponding number into the spelling of the word.)

“Once we know how the vowel letters and numbers were used, ʻŌpūkahaʻia’s short grammar becomes more than just a curiosity; it is a serious work that is probably the first example of the Hawaiian language recorded in a systematic way. Its alphabet is a good deal more consistent than those used by any of the explorers who attempted to record Hawaiian words.” (Schutz)

“It might be said that the first formal writing system for the Hawaiian language, meaning alphabet, spelling rules and grammar, was created in Connecticut by a Hawaiian named Henry ʻŌpūkahaʻia.  He began work as early as 1814 and left much unfinished at his death in 1818.” (Rumford)

“His work served as the basis for the foreign language materials prepared by American and Hawaiian students at the Foreign Mission School in Cornwall, Connecticut, in the months prior to the departure of the first company of missionaries to Hawai’i in October 1819.”  (Rumford)

It is believed ʻŌpūkahaʻia classmates (and future missionaries,) Samuel Ruggles and James Ely, after ʻŌpūkahaʻia’s death, went over his papers and began to prepare material on the Hawaiian language to be taken to Hawaiʻi and used in missionary work (the work was written by Ruggles and assembled into a book – by Herman Daggett, principal of the Foreign Mission School – and credit for the work goes to ʻŌpūkahaʻia.)

Lots of information here from Rumford (Hawaiian Historical Society) and Schutz (Honolulu and The Voices of Eden: A History of Hawaiian Language Studies.)

I encourage you to review the images in the folder; I had the opportunity to review and photograph the several pages of ʻŌpūkahaʻia’s grammar book.

© 2023 Hoʻokuleana LLC

 

Filed Under: General, Missionaries / Churches / Religious Buildings Tagged With: Hawaii, Noah Webster, Henry Opukahaia, Hawaiian Mission Houses Historic Site and Archives, Hawaiian Language, Hawaiian

April 11, 2023 by Peter T Young Leave a Comment

Whose Footprints Are These?

Geologic evidence suggests that the modern caldera of Kīlauea formed shortly before 1500 AD. Repeated small collapses may have affected parts of the caldera floor, possibly as late as 1790. For over 300-400 years, the caldera was below the water table.

Kilauea can be an explosive volcano; several phreatic eruptions have occurred in the past 1,200 years.  (Phreatic eruptions, also called phreatic explosions, occur when magma heats ground or surface water.)

The extreme temperature of the magma (from 932 to 2,138 °F) causes near-instantaneous evaporation to steam, resulting in an explosion of steam, water, ash and rock – the 1980 eruption of Mount St. Helens was a phreatic eruption.

The 1924 eruption at Halemaʻumaʻu documents and illustrates the explosive nature of Kilauea.  However, the 1924 explosions were small by geologic standards and by the standards of some past Kilauea explosions.

The hazards of larger explosions, such as those that took place multiple times between about AD 1500 and 1790, are far worse than those associated with the 1924 series.  (USGS)

There were explosions in 1790, the most lethal known eruption of any volcano in the present United States. The 1790 explosions, however, simply culminated (or at least occurred near the end of) a 300-year period of frequent explosions, some quite powerful.  (USGS)

Keonehelelei is the name given by Hawaiians to the explosive eruption of Kilauea in 1790.  It is probably so named “the falling sands” because the eruption involved an explosion of hot gas, ash and sand that rained down across the Kaʻu Desert.  The character of the eruption was likely distinct enough to warrant a special name.  (Moniz-Nakamura)

At the time, Kaʻū Chief Keōuakūʻahuʻula (Keōua) was the only remaining rival of Kamehameha the Great for control of the Island of Hawaiʻi; Keōua ruled half of Hāmākua and all of Puna and Kaʻū Districts.  They were passing through the Kilauea area at the time of the eruption. The 1790 explosion led to the death of one-third of the warrior party of Keōua.  (Moniz-Nakamura)

Camped in Hilo, Keōua learned of an invasion of his home district of Kaʻū by warriors of Kamehameha. To reach Kaʻū from Hilo, Keōua had a choice of two routes one was the usually traveled coastal route, at sea level, but it was longer, hot, shadeless and without potable water for long distances.  (NPS)

The other route was shorter, but passed over the summit and through the lee of Kilauea volcano, an area sacred to, and the home of, the Hawaiian volcano goddess Pele. Keōua chose the volcano route, perhaps because it was shorter and quicker, with water available frequently.  (NPS)

In 1919, Ruy Finch, a geologist at the Hawaiian Volcano Observatory discovered human footprints fossilized in the Kaʻū desert ash. Soon, this area of the desert became known as “Footprints.”

Barefoot walkers left thousands of footprints in wet volcanic ash within a few miles southwest of Kīlauea’s summit.

Many historians and Hawaiians believe the footprints were made by Keōua and his warriors.  Keōua was known to be in the area at the time, and previous thought suggested this part of the desert did not have pre-contact use, so it was narrowed down to them.

Scientists later investigated – one approach was to look deeper at the evidence.

Forensic studies indicate that the length of a human foot is about 15% of an individual’s height. A man’s foot may be slightly more that 15%, a woman’s slightly less, but it is possible to estimate the height to a couple of inches.  (USGS)

They measured 405-footprints to determine how tall the walkers were.  The average calculated height is only 4-feet 11-inches, and few footprints were made by people 5-feet 9-inches or more tall. Early Europeans described Hawaiian warriors as tall; one missionary estimated an average height of 5-feet 10-inches. Many now believe that most of the footprints were made by women and children, not by men, much less warriors.  (USGS)

Meanwhile, Keōua’s party was camped on the upwind side of Kīlauea’s summit – perhaps on Steaming Flat – waiting for Pele’s anger to subside. They saw the sky clear after the ash eruption and began walking southwestward between today’s Volcano Observatory and Nāmakanipaio.  (USGS)

Suddenly, the most powerful part of the eruption began, developing a high column and sending surges at hurricane velocities across the path of the doomed group. Later, survivors and rescuers made no footprints in the once wet ash, which had dried.  (USGS)

Then, archaeologists looked for other evidence to help identify who the footprints may have belonged to.  Contrary to general thought that the area was not used by the Hawaiians, archaeological investigations discovered structures, trails and historic artifacts in the area.  (Moniz-Nakamura)

Most of the features were along the edge of the Keʻāmoku lava flow.  Several of the trails converge south of the flow, suggesting a major transportation network.  The structures are likely temporary, used as people were traversing through the desert on their way to/from Kaʻū and Hilo.  (Moniz-Nakamura)

The sheer number of temporary shelters along the Keʻāmoku flow, as well as the trail systems and quarry sites, strongly suggest that this area was frequently used by Hawaiians travelling to and through the area – before and after the 1790 eruption.  (Moniz-Nakamura)

If the footprints aren’t Keōua’s warriors, then how did one-third of his warriors die?

Several suggestions have been made: suffocation due to ash; lava, stones, ash and other volcanic material; or strong winds produced by the eruption, asphyxiation and burning killed them.  (Moniz-Nakamura)

A more recent suggestion is that a “hot base surge, composed primarily of superheated steam … (traveling at) hurricane velocity” was the cause of death.  The wind velocity prevented the people from running away; they probably huddled together, then “hot gases seared their lungs.”  (Moniz-Nakamura)

Some now suggest that, if these observations and ideas are correct, the footprints were made in 1790, but not by members of Keōua’s group.  (USGS)

A reconstruction of events suggests that wet ash, containing small pellets, fell early in the eruption, blown southwestward into areas where family groups, mainly women and children, were chipping glass from old pāhoehoe. They probably sought shelter while the ash was falling. Once the air cleared, they slogged across the muddy ash, leaving footprints in the 1-inch thick deposit.  (USGS)

On August 1, 1916, President Woodrow Wilson signed the country’s 13th national park into existence – Hawaiʻi National Park.  At first, the park consisted of only the summits of Kilauea and Mauna Loa on Hawaiʻi and Haleakalā on Maui.

Eventually, Kilauea Caldera was added to the park, followed by the forests of Mauna Loa, the Kaʻū Desert, the rain forest of Olaʻa and the Kalapana archaeological area of the Puna/Kaʻū Historic District.

In 1961, Hawaiʻi National Park’s units were separated and re-designated as Haleakalā National Park and Hawaii Volcanoes National Park.) (Lots of good information here is from USGS, NPS and Jade Moniz-Nakamura.)

© 2023 Hoʻokuleana LLC

 

Filed Under: General, Hawaiian Traditions Tagged With: Kilauea, Kamehameha, Hawaii Volcanoes National Park, Kau, Keoua, Haleakala National Park, Hawaii National Park, Keonehelelei, Hawaii, Halemaumau, Hawaii Island, Volcano

April 7, 2023 by Peter T Young Leave a Comment

Coffee Schedule

“You know, when you in the seventh grade like that, to carry one bag of coffee was quite a chore. And load three bags on a donkey and come up the trail. When it rain, the donkey would slip on the trail, fall. Had to unload the coffee, get the donkey up, load it again. I know, many times, I used to cry.” (Minoru Inaba)

As early as 1684, a grammar school founded in Massachusetts required 12 months of education. In 1841, Boston schools operated for 244 days while Philadelphia implemented a 251-day calendar.

In the beginning of the nineteenth century, large cities commonly had long school years, ranging from 251 to 260 days. During this time, many of these rural schools were only open about 6 months out of the year.  (Pedersen)

The origin for the traditional school calendar based purely on agrarian needs was not entirely accurate. In the 19th century districts organized their calendars around the needs of the community.

For example, some special provisions were made for vacations during September and October for communities with large fall harvests. Prior to 1890, students in major urban areas were in school for 11 months a year. But by 1900, the more popular 180 day, 9-month calendar had been firmly established. (Pedersen)

In the days before air conditioning, schools and entire cities could be sweltering places during the hot summer months. Wealthy and eventually middle-class urbanites also usually made plans to flee the city’s heat, making those months the logical time in cities to suspend school.

By the late 19th century, school reformers started pushing for standardization of the school calendar across urban and rural areas. So a compromise was struck that created the modern school calendar.  (PBS)

In Kona, the harvest of coffee used to set the school calendar.  “(B)ecause coffee was the basic industry in those days, much of the land was planted in coffee, of course. As of now, much of the land has been abandoned. But in those days, coffee was the basic industry in Kona.”

“(T)here was no other industry in Kona except coffee farming, and the sugar plantation, for a while. And of course, ranching, they had from way back. There was no tourism. No other businesses except coffee farming in Kona. … Most of the families were farmers. … coffee farmers.” (Minoru Inaba)

“As early as 1916 a ‘coffee vacation’ of three weeks in each November was an established institution in central Kona, where 95 per cent of Hawaii’s coffee industry is located.”

“It continued up to 1924, when the ‘vacation’ became optional – each school deciding when and how many weeks the vacation may be held each autumn.” (Inouye)

Then, in 1931, “A special vacation of three weeks for all schools in Kona has been sanctioned by the department of public instruction … The length of the vacation was a compromise between four or five weeks wanted by the (coffee) planters, and two weeks favored by most school principals.” (Hawaii Tribune Herald, Sep 23, 1931)

That, apparently, wasn’t good enough to address the needs of families of Konawaena – a couple weeks later it was announced, “Members of the Kona-waena Parent-Teacher association gave their unanimous approval at a meeting yesterday …”

“… to the plan to change the Kona-waena school year from September to June to December to September, allowing school children to assist in the coffee harvest during the months of September, October, and November.”

“The action was taken to eliminate the so-called ‘coffee vacation’ which makes it necessary for students to make up the time lost by attending school during the Thanksgiving holiday period and for five Saturdays after the first of February.”

“Much opposition had developed to the coffee vacation and the new proposal was suggested as a means of adapting the school year to the needs of industry in the Kona district.” (Hawaii Tribune Herald, Nov 23. 1931)

The Star Bulletin announced “Change in Vacation Time at Kona-Waena … With the approval of the new vacation schedule for the Kona-waena high school and grammar school in Kona by the West Hawaii commissioners, the annual vacation will be shifted from summer to winter.” (SB, Feb 13, 1932)

“)B)ecause of the need of the farmers to have their children help them on the farms, the coffee schedule was established. And the coffee schedule ran from … August, September, October, November – those three months – was the regular vacation – coffee vacation. This is the time when it was coffee season, you see?” (Minoru Inaba)

“(T)he summer vacation was really a fall vacation and started around the 16th of August and went through to about the 16th of November. So, that took most of the football season. The community associations didn’t get into football, because that would have only hurt the reason for the schedule as it was.”

“It would take kids away from picking coffee and helping their families. I think eventually, though, these kids found other things to do – possibly (because of) family transportation. Kids found other things to do a lot better than picking coffee.” (Sherwood Greenwell)

“You see, how they got that, you have to have the school kids pick coffee, eh? That’s the only way they can help the parents, by picking coffee. So, if you stay home from school, you lose that much education. I guess they entered a resolution or whatever you call it. Anyway, they got their school to change the time … that’s when you’re picking coffee.”

“We [normally] go back September. … the peak season is right when the school go back. So, they change it so that they have their Kona schedule on a coffee harvest time. Well, it worked out all right like that.” (Willie Thompson)

“(I)n the earlier days, on off season, the time before harvesting and after trimming, there weren’t job opportunities for the farmers. There was a criticism – probably doesn’t hold as much today because there’re not as many schoolteachers that are in the coffee business – but a lot of the schoolteachers that came back here, came back here because they had coffee farms – their

families had coffee farms.”

“Well, the coffee schedule really ended because the families could no longer get the kids to come back and spend the time on the farms to pick coffee, which the coffee schedule was supposed to take care of.”

“But those teachers that had coffee farms were more concerned about their coffee operations really than they were on their teaching. The teaching gave them the security of a steady income, while the coffee income was what they were really concerned about.” (Sherwood Greenwell)

“There were probably five or six years of where there was a question, (should) the coffee schedule be continued or (should) they give it up?  This became quite a hassle. It was kept, I think, longer than it was practical.”

“Probably for one reason more than anything else, and that was that a lot of the farmers felt that it was a concession that they had somehow gotten that was very important to them. Not that it was that worthwhile to them, but it was a concession that government had given them and they wanted it sort of there, even though it wasn’t working out as well as it should.”

“So, I think that probably extended the [time].  And it also – you got a feeling from the attitude of some people that if you were for going back to the regular schedule, that you were an enemy to coffee.”

“This was a feeling, I think, that a lot of people had who would like to have seen the thing [coffee schedule] dropped. It took some time and some guts for most of the people to overcome that feeling. So, I think it did continue longer than it should have.”

“I think it would have been better for the kids and everybody that it would be over with sooner. Kids going into college off the Kona schedule, college almost had started before they graduated, and I don’t think it helped that type of education – you know, ongoing education – for the kids.”  (Sherwood Greenwell)

Kona was not the only place with crop-based vacations … “(O)ne year, we were cutting back across the states, and there was a kid in Idaho fishing at a stream where we were fishing. We asked him how come he wasn’t in school. He said, ‘oh, spud vacation’. What they did was, school was let out at the height of the potato harvesting season for two weeks.”

“Something like that probably would have been a better way of doing it. Going on the regular schedule and then just having a vacation tied right into the harvesting period.” (Sherwood Greenwell)

“Then, the coffee kind of faded out. All the new teachers, they didn’t like teaching when all the other teachers have a rest, and they working. Then, they changed back to the regular. Then, the weather kind of changed too. Not much coffee. The season kind of different, too. So, that’s how they got the schools like that … about in the ’60s, they changed back to the regular schedule.” (Willie Thompson)

“I think, at the beginning, there was a real reason for it and I think it worked out very well. I think it strengthened the ties within the family where they all were working together for something.”

“I know it’s been said at times, if you had someone applying for a job that came from Kona, he was a good worker. He had good loyalty and he was a good worker. I think that all comes from that period where everybody in the family worked hard together.” (Sherwood Greenwell)

In 1932, the school coffee schedule was inaugurated. There are 1,077 coffee farms in Kona, covering 5,498 acres. The farms ranged in size from 3 to 30 acres, with the average size being 5 acres.

Kona students picked a total of 25,320 bags during their “summer” vacation period between October and December in 1932.  (Social History of Kona)

On June 20, 1968, “The Kona coffee schedule of November – to – August year for Kona schools was ended … in a complicated series of actions by the State Board of Education.  The board thus ended a 36-year-old unique tradition devised to free youngsters to pick coffee during the harvest months of September and October.”

A transition year in 1968-69 was “a temporary measure to provide time to plan for implementing an entirely new system in the 1969-70 school year.”  (SB, June 21, 1968)

© 2022 Ho‘okuleana LLC

Filed Under: Schools Tagged With: Hawaii, Kona, Kona Coffee, Konawaena High, Coffee Schedule, Vacation

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