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January 30, 2016 by Peter T Young 4 Comments

ʻAilāʻau

The longest recorded eruption at Kilauea, arguably, was the ʻAilāʻau eruption and lava flow in the 15th century, which may be memorialized in the Pele-Hiʻiaka chant. It was the largest in Hawaiʻi in more than 1,000-years.

The flow was named after ʻAilāʻau was known and feared by all the people. ʻAi means the “one who eats or devours.” Lāʻau means “tree” or a “forest.”

ʻAilāʻau was, therefore, the forest eating (destroying) fire-god. Time and again he laid the districts of South Hawaii desolate by the lava he poured out from his fire-pits. (He was the fire god before Pele arrived at Hawaiʻi Island.)

He was the god of the insatiable appetite; the continual eater of trees, whose path through forests was covered with black smoke fragrant with burning wood, and sometimes burdened with the smell of human flesh charred into cinders in the lava flow.

ʻAilāʻau seemed to be destructive and was so named by the people, but his fires were a part of the forces of creation. He built up the islands for future life. The flowing lava made land. Over time, the lava disintegrates and makes earth deposits and soil. When the rain falls, fruitful fields form and people settled there.

ʻAilāʻau still poured out his fire. It spread over the fertile fields, and the people feared him as the destroyer giving no thought to the final good.

He lived, the legends say, for a long time in a very ancient part of Kilauea, on the large island of Hawaii, now separated by a narrow ledge from the great crater and called Kilauea Iki (Little Kilauea).

The ʻAilāʻau eruption took place from a vent area just east of Kilauea Iki. The eruption built a broad shield. The eastern part of Kilauea Iki Crater slices through part of the shield, and red cinder and lava flows near the center of the shield can be seen on the northeastern wall of the crater.

The eruption probably lasted about 60 years, ending around 1470 (based on evaluation of radiocarbon data for 17 samples of lava flows produced by the ʻAilāʻau shield – from charcoal created when lava burns vegetation.) The ages obtained for the 17 samples were averaged and examined statistically to arrive at the final results.

The radiocarbon data are supported by the magnetic declination and inclination of the lava flows, frozen into the flows when they cooled. This study found that these “paleomagnetic directions” are consistent with what was expected for the 15th century.

Such a long eruption naturally produced a large volume of lava, estimated to be about 5.2 cubic kilometers (1.25 cubic miles) after accounting for the bubbles in the lava. The rate of eruption is about the same as that for other long-lasting eruptions at Kilauea.

This large volume of lava covered a huge area, about 166 square miles (over 106,000-acres) – larger than the Island of Lānaʻi. From the summit of the ʻAilāʻau shield, pāhoehoe lava flowed 25-miles northeastward, making it all the way to the coast.

Lava covered all, or most, of what are now Mauna Loa Estates, Royal Hawaiian Estates, Hawaiian Orchid Island Estates, Fern Forest Vacation Estates, Eden Rock Estates, Crescent Acres, Hawaiian Acres, Orchid Land Estates, ʻAinaloa, Hawaiian Paradise Park and Hawaiian Beaches. (USGS)

After a time, ʻAilāʻau left these pit craters and went into the great crater and was said to be living there when Pele came to the seashore far below.

When Pele came to the island Hawaiʻi, she first stopped at a place called Keahialaka in the district of Puna. From this place she began her inland journey toward the mountains. As she passed on her way there grew within her an intense desire to go at once and see ʻAilāʻau, the god to whom Kilauea belonged, and find a resting-place with him as the end of her journey.

She came up, but ʻAilāʻau was not in his house – he had made himself thoroughly lost. He had vanished because he knew that this one coming toward him was Pele. He had seen her toiling down by the sea at Keahialaka. Trembling dread and heavy fear overpowered him.

He ran away and was entirely lost. When he came to that pit she laid out the plan for her abiding home, beginning at once to dig up the foundations. She dug day and night and found that this place fulfilled all her desires. Therefore, she fastened herself tight to Hawaii for all time.

These are the words in which the legend disposes of this ancient god of volcanic fires. He disappears from Hawaiian thought and Pele from a foreign land finds a satisfactory crater in which her spirit power can always dig up everlastingly overflowing fountains of raging lava. (Westervelt)

The ʻAilāʻau flow was such a vast outpouring changed the landscape of much of Puna. It must have had an important impact on local residents, and as such it may well be described in the Pele-Hiʻiaka chant.

Hiʻiaka, late on returning to Kilauea from Kauaʻi with Lohiau, sees that Pele has broken her promise and set afire Hiʻiaka’s treasured ʻōhiʻa lehua forest in Puna. Hiʻiaka is furious, and this leads to her love-making with Lohiau, his subsequent death at the hands of Pele, and Hiʻiaka’s frantic digging to recover the body.

The ʻAilāʻau flows seem to be the most likely candidate because it covered so much of Puna. The timing seems right, too – after the Pele clan arrived from Kahiki, before the caldera formed (Hiʻiaka’s frantic digging may record this), and before the encounters with Kamapuaʻa, some of which probably deal with explosive eruptions between about 1500 and 1790. (Information here is from USGS and Westervelt.)

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Ailaau Flow-Kīlauea summit overflows-their ages and distribution in the Puna District, Hawai'i-Clague-map
Ailaau Flow-Kīlauea summit overflows-their ages and distribution in the Puna District, Hawai’i-Clague-map
Ailaau_lava_flow-map-USGS
Ailaau_lava_flow-map-USGS
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Kilauea_map-Johnson
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Hawaii-Volcanoes-NPS-map
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CraterRimDrive-dartmouth
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Kilauea-Kilauea_Iki-Bosick
Age and Distribution of Lava Flows in Kilauea-USGS
Age and Distribution of Lava Flows in Kilauea-USGS
Kilauea-Byron-1825
Kilauea-Byron-1825

Filed Under: General, Hawaiian Traditions, Place Names Tagged With: Ailaau, Hawaii, Hawaii Island, Volcano, Pele, Puna, Kilauea

January 6, 2016 by Peter T Young 2 Comments

“the loveliest fleet of islands that lies anchored in any ocean”

In 1866, Samuel Langhorne Clemens (Mark Twain) was retained by The Sacramento Union newspaper to write a series of articles on Hawaiʻi. Here are some of his words about Hawaiʻi (from that series, as well as his other writing.)

“I was there for four or five months, and returned to find myself about the best known man on the Pacific Coast.” (Twain) Popular pieces, some credit the series with turning Twain into a journalistic star.

Like they get to a lot of people, the Islands struck a chord with Clemens.

“On the seventh day out we saw a dim vast bulk standing up out of the wastes of the Pacific and knew that that spectral promontory was Diamond Head”.

“So we were nearing Honolulu, the capital city of the Sandwich Islands – those islands which to me were Paradise; a Paradise which I had been longing all those years to see again. Not any other thing in the world could have stirred me as the sight of that great rock did.”

“The town of Honolulu (said to contain between 12,000 and 15,000 in habitants) is spread over a dead level; has streets from twenty to thirty feet wide, solid and level as a floor, most of them straight as a line … houses one and two stories high, … there are great yards, (that) are ornamented by a hundred species of beautiful flowers and blossoming shrubs, and shaded”.

“A mile and a half from town, I came to a grove of tall cocoanut trees, with clean, branchless stems reaching straight up sixty or seventy feet and topped with a spray of green foliage sheltering clusters of cocoa‐nuts”.

“… not more picturesque than a forest of colossal ragged parasols, with bunches of magnified grapes under them, would be. … It is the village of Waikiki once the Capital of the kingdom and the abode of the great Kamehameha I.”

“What a picture is here slumbering in the solemn glory of the moon! How strong the rugged outlines of the dead volcano stand out against the clear sky! What a snowy fringe marks the bursting of the surf over the long, curved reef!”

“I tried surf-bathing (surfing) once, subsequently, but made a failure of it. I got the board placed right, and at the right moment, too; but missed the connection myself. – The board struck the shore in three quarters of a second, without any cargo, and I struck the bottom about the same time, with a couple of barrels of water in me.”

“It has been six weeks since I touched a pen. In explanation and excuse I offer the fact that I spent that time (with the exception of one week) on the island of Maui. … I never spent so pleasant a month before.”

“I went to Maui to stay a week and remained five. I had a jolly time. I would not have fooled away any of it writing letters under any consideration whatever. … I sail for the island of Hawaiʻi tomorrow.”

“We landed at Kailua (Kona,) a little collection of native grass houses reposing under tall cocoanut trees ‐ the sleepiest, quietest, Sundayest looking place you can imagine.”

“Ye weary ones that are sick of the labor and care, and the bewildering turmoil of the great world, and sigh for a land where ye may fold your tired hands and slumber your lives peacefully away, pack up your carpet sacks and go to Kailua!”

“I suppose no man ever saw Niagara for the first time without feeling disappointed. I suppose no man ever saw it the fifth time without wondering how he could ever have been so blind and stupid as to find any excuse for disappointment in the first place.”

“I was disappointed when I saw the great volcano of Kilauea to‐day for the first time. It is a comfort to me to know that I fully expected to be disappointed, however, and so, in one sense at least, I was not disappointed.”

“I said to myself ‘Only a considerable hole in the ground ‐ nothing to Haleakala ‐ a wide, level, black plain in the bottom of it, and a few little sputtering jets of fire occupying a place about as large as an ordinary potato‐patch, up in one corner ‐ no smoke to amount to anything.’”

“I reflected that night was the proper time to view a volcano … I turned my eyes upon the volcano again (now, at night.)”

“… the floor of the abyss was magnificently illuminated; beyond these limits the mists hung down their gauzy curtains and cast a deceptive gloom over all … Here was room for the imagination to work! … it was the idea, of eternity made tangible ‐ and the longest end of it made visible to the naked eye!”

“We hear all our lives about the ‘gentle, stormless Pacific,’ and about the ‘smooth and delightful route to the Sandwich Islands,’ and about the ‘steady blowing trades’ that never vary, never change, never ‘chop around’”.

“No alien land in all the world has any deep, strong charm for me but that one; no other land could so longingly and beseechingly haunt me, sleeping and waking, through half a lifetime, as that one has done.”

“Other things leave me, but it abides; other things change, but it remains the same. For me its balmy airs are always blowing, its summer seas flashing in the sun; the pulsing of its surf beat is in my ear”.

“I can see its garlanded craigs, its leaping cascades, its plumy palms drowsing by the shore; its remote summits floating like islands above the cloudrack”.

“I can feel the spirit of its woodland solitudes; I can hear the plash of its brooks; in my nostrils still lives the breath of flowers that perished twenty years ago.”

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RJ_Baker_Twain-1915
RJ_Baker_Twain-1915

Filed Under: General, Prominent People Tagged With: Mark Twain, Samuel Clemens, Hawaii

January 3, 2016 by Peter T Young 1 Comment

Collapse to Caldera

The Hawaiian Islands are volcanic in origin. Each island is made up of at least one primary volcano, although many islands are composites of more than one. The Big Island, for instance, is constructed of 5 major volcanoes: Kilauea, Mauna Loa, Mauna Kea, Hualālai and Kohala. Mauna Loa is the largest active volcano on Earth.

Kilauea is presently one of the most productive volcanoes on Earth (in terms of how much lava it erupts each year). The primary volcanoes on each of the islands are known as a shield volcanoes, which are gently sloping mountains produced from a large number of generally very fluid lava flows. (SOEST)

To the casual observer, Kilauea appears to be part of the larger volcano Mauna Loa, but geological data indicates that it is a separate volcano with its own vent and conduit system. (livescience) When Kilauea began to form is not known, but various estimates are 300,000-600,000-years ago. (USGS)

Kilauea is a broad shield volcano built against the southeastern slope of Mauna Loa. The summit presently has a caldera that is roughly 2.5-miles by 2-miles wide, and walls nearly 400-feet. Another feature, known as Halemaʻumaʻu crater, lies within the main caldera (on the southwestern side.)

For the past century, Halemaʻumaʻu has been the principal site of activity at Kilauea’s summit. There has also been frequent activity along the Southeast rift zone (such as the presently active Puʻu ʻOʻo eruption, which started in 1983.)

While at nearby Mauna Loa eruptions tend to occur in pairs (i.e., a summit eruption followed by one on the flank), Kilauea’s pattern of summit versus flank activity appear to be more random. However, evidence of numerous flank eruptions occurring after a summit eruption can be found. (SOEST)

Sometimes, volcano summits form calderas. When an erupting volcano empties a shallow-level magma chamber, the edifice of the volcano may collapse into the voided reservoir, thus forming a steep, bowl-shaped depression called a caldera (Spanish for kettle or cauldron.)

The summit regions of many active shield volcanoes are marked by calderas. Hawaiian examples include the Mokuaweoweo caldera on Mauna Loa and the Kilauea caldera on Kilauea. (sdsu-edu)

So, when and how was the Kīlauea Caldera formed?

The modern caldera at Kilauea collapsed in about 1470-1500 AD, as recognized by geologic field work and C-14 radiocarbon dating. Two lines of geologic evidence indicate it was very deep soon after it formed, as is also suggested by Hawaiian oral tradition.

Scientists suggest at least a couple possibilities exist for the collapse. One is that the magma reservoir emptied rapidly without erupting; the other possibility is that magma withdrawal was prolonged, not rapid, in response to slow eruption of the ʻAilāʻau lava flow (the largest in Hawaiʻi in more than 1000 years.)

The flow erupted on the east side of Kilauea’s summit during a ca. 60-yr period ending in about 1470. It has typical tube-fed formation, consistent with slow eruption. The eruption just predates the caldera – its shield is cut by the outermost caldera fault – and in fact could have ended when the caldera formed. (Swanson)

Geologic evidence indicates that the caldera appeared in about AD 1500, give or take several decades. It developed at the end of, or soon after, a 60-year-long eruption from the ʻAilāʻau shield just east of Kilauea Iki, flooding much of Puna with lava flows. The caldera formed at the start of, or shortly before, a series of explosions that radiocarbon ages date to about AD 1500. (USGS)

However, most geologic models assume very rapid removal of material to form a caldera. The argument is that a large void cannot support itself underground, so an empty volume of a few cubic miles could not exist for long. If so, a huge volume of magma must have almost instantaneously left the reservoir under Kilauea’s summit, leaving a void into which the summit fell.

Both geologic and cultural evidence should exist for such a major volcanic event. Indeed, the events are likely chronicled in the Pele-Hiʻiaka chants. But neither cultural nor geologic evidence tells us where the rocks disappeared when the top of the volcano sunk to form the caldera.

How much material was removed? The volume is uncertain but very large. If the entire caldera formed at one time, scientists estimate a volume of 1.4 cubic miles, equivalent to 780-million loads for a 10-cubic-yard dump truck. That estimate is based on the caldera’s dimensions when first surveyed in the 1820s and on guesses as to how much deeper it might have been. (USGS)

Historical eruptions at Kilauea volcano have occurred from both the summit caldera and from vents along the East Rift Zone. The historical record began with a very explosive eruption in 1790.

After this, the volcano was almost continuously active, mostly showing gentle effusion from a lava lake at the summit until 1924, when it again erupted explosively. The period 1924 to 1955 saw mostly short-duration summit eruptions.

From 1955 to the present Kilauea has seen mostly East Rift Zone activity interspersed with small summit eruptions. Two notable rift eruptions were Mauna Ulu (1969-1974) and Puʻu ʻOʻo (1983-present). Kilauea’s Eruption rate diminished steadily over the first half of the historic period but has been increasing again since 1924. (SOEST)

Since the Puʻu ʻOʻo eruption started on January 3, 1983, the southern part of the caldera has been sinking 2.5-4 inches/year. (USGS)

Currently there are 3 Hawaiian volcanoes that we can be classified as active: Kilauea, actively erupting since 1983; Mauna Loa, which last erupted in 1984 and is building for a new eruption in the next few years; and Loihi, which erupted in 1996.

All three of these active Hawaiian volcanoes share the Hawaiian hot spot, but retain unique volcanic histories and compositions.

The most likely dormant volcanoes are: Hualālai, which last erupted in 1801; Haleakalā, which last erupted in about 1790; and Mauna Kea, which last erupted about 4,000-years ago. (SOEST)

Due to the ongoing eruption, portions of the Hawaiʻi Volcanoes National Park are periodically closed, due the hazardous and unsafe conditions; check conditions and area closures before venturing.

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CraterRimDrive-dartmouth
CraterRimDrive-dartmouth
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Kilauea-Byron-1825
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Kilauea_Summit-Klemetti
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Kilauea’s summit caldera-Dzurisin-1980
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‎Kilauea-Caldera-Kauahikaua-1997
Kilauea_Overlook-NPS - Ed Shiinoki
Kilauea_Overlook-NPS – Ed Shiinoki
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Overlook at Jaggar Museum-Shiinoki
Age and Distribution of Lava Flows in Kilauea-USGS
Age and Distribution of Lava Flows in Kilauea-USGS
Simplified cutaway view (not to scale) of Kilauea Volcano-Johnson
Simplified cutaway view (not to scale) of Kilauea Volcano-Johnson
Ailaau Flow-Kīlauea summit overflows-their ages and distribution in the Puna District, Hawai'i-Clague-map
Ailaau Flow-Kīlauea summit overflows-their ages and distribution in the Puna District, Hawai’i-Clague-map
Ailaau_lava_flow-map-USGS
Ailaau_lava_flow-map-USGS

Filed Under: General Tagged With: Hawaii, Volcano, Kilauea, Halemaumau

December 25, 2015 by Peter T Young 2 Comments

Merry Christmas!!!

Wishing you and your loved ones peace, health, happiness and prosperity in the coming New Year! Merry Christmas!!!

One of my favorite Christmas songs, Henry Kapono – Merry Christmas to You:

Christmas-2014

Filed Under: General Tagged With: Hawaii, Christmas

December 24, 2015 by Peter T Young 5 Comments

Merry Christmas

Let’s not forget the reason for the season. Merry Christmas!!!

Here is Willie K singing O Holy Night:

Christmas_Eve-2014

Filed Under: General Tagged With: Christmas

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