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February 23, 2017 by Peter T Young Leave a Comment

Wilkes Trail

Hawaiians laid out trails and evolved practices which assured availability of shelter, drinking fluids and firewood. (NPS)

In 1840, Lt Charles Wilkes, as part of the US Exploring Expedition, came to Hawai‘i to conduct experiments and make observations, including swinging pendulums on Mauna Loa’s summit to calculate the force of gravity. They hiked from Hilo to the summit.

Wilkes noted, “I had the pleasure of being accompanied by Mr. Brinsmade, our worthy consul, and my friend Dr GP Judd, both of whom volunteered to accompany me in the novel and arduous enterprise I was about to undertake.”

They first landed in Hilo, “The scene which the island presents as viewed from the anchorage in Hilo Bay, is both novel and splendid : the shores are studded with extensive groves of cocoa-nut and bread-fruit trees, interspersed with plantations of sugar-cane …”

“… through these, numerous streams are seen hurrying to the ocean; to this succeeds a belt of some miles in width, free from woods, but clothed in verdure …”

“… beyond is a wider belt of forest, whose trees, as they rise higher and higher from the sea, change their characters from the vegetation of the tropics to that of polar regions ; and above all tower the snow-capped summits of the mountains.”

“From Hilo, Mauna Loa looks as if one might walk over its smooth surface without difficulty; there is, indeed, so much optical deception in respect to this mountain, that it served to give us all great encouragement, and we set about making our preparations with a determination to succeed in the attempt to reach its highest summit.”

“Beside about two hundred natives, the party consisted of Lieutenant Budd, Passed Midshipman Eld, Midshipman Elliott, Mr Brinsmade, Dr Pickering, Mr Brackenridge, Dr Judd, myself, and ten men, including our servants from the ship.”

“This was a large party; but when it is considered, that besides our instruments, tents, &c., provisions were to be carried, it will not be considered so disproportionate, especially as it generally requires one-third of the number, if not more, to carry provisions for the rest.” (Wilkes)

Then, the confusion started, “our chief scribe, Kalumo, who had the books containing the lists (of who was to do what,) was missing, and there was an uproar resembling that of Bedlam.”

“In consequence of the absence of Kalumo, the natives had an opportunity of trying the weight of some of the bundles, and before he was forthcoming, many of the lightest loads had very adroitly been carried off. … it was soon found that there would be many loads for which we had no bearers, and these were, of course, all those of bulk and weight”.

Wilkes was forced to hire, at double pay through another chief, a second group of porters to carry the bulky and heavy items … two days later and 30 miles inland … and close to the summit of Kilauea volcano, Wilkes had become increasingly disenchanted … (NPS)

Then, things got worse … Wilkes took the ‘wrong road;’ actually, he ignored references to take traditional trials, and, leading a party of 300 Caucasians and Hawaiians, Wilkes took off on a trackless beeline from Kilauea toward Mauna Loa’s summit, guided by a midshipman holding a compass. (NPS)

Wilkes substituted his own route for the Hawaiian Ainapo trail. Wilkes’ line of march was through wooded country, but without streams or waterholes. Shoes of the Caucasians scuffed and soles abraded on the lava they crossed.

Most of the Hawaiians were barefoot. To mark the path for the straggling porters, Wilkes’ associates built fires and blazed trees. Bushes were broken with their tops laid down to indicate the direction of travel. (NPS)

“Our (first) encampment was called the Sunday Station, on account of our having remained quietly here on that day. The altitude given by the barometer was six thousand and seventy-one feet, at which we found ourselves above the region of clouds, and could look down upon them.” (Wilkes) It ended up being the principal base camp.

Much unnecessary thirst, hunger, cold, altitude sickness, fatigue, and snowblindness were suffered by both Caucasians and Hawaiians of the expedition when Wilkes substituted his own route for the Hawaiian Ainapo trail.

‘Mountain’ sickness, probably caused from the combination of fatigue, dehydration, chill, hunger, and the altitude, was prevalent.

Fuel was scarce to make fires for warmth or cooking, Hawaiians sold water at 50 cents a quart to thirsty sailors and accepted warm clothing if cash was not available.

To the rescue came the Hawaiian guides ‘Ragsdale’ and Keaweehu, a famous bird catcher. Both had apparently been waiting at Kapapala for the expedition to arrive and planned to guide the expedition up the Ainapo trail.

Ragsdale was hired to supply water for the camp. His men delivered it the next day – fifteen gallons carried in open-top vessels over the trackless ten miles of rugged lavas which separated Wilkes’ camp from the Ainapo trail.

At about the same elevation on the Ainapo was a large lava tube with pools of water inside. This tube was used by Hawaiians on the Ainapo trail and was easily supplied with grass (for insulation from the cold ground) and firewood from a point on the trail not far below. (NPS)

Eventually, Wilkes ended up with other camps on the way up to and at the summit area of Mauna Loa: “Recruiting Station” just below the 10,000-foot elevation (used primarily staging & medical care) …

… “Flag Station” between the 12,000- and 13,000-foot elevation (Wilkes “left a flag on a rocky peak near by” and “Pendulum Peak” near the summit where they conducted pendulum and other observations.

After conducting their experiments and observations, “When day broke, on the 13th January, all was bustle on the summit of Mauna Loa.”

“Every one was engaged in taking down and packing up the instruments and equipage, loaded with which the native labourers scampered off. Some of them, indeed, unable to bear the cold any longer, and hoping to obtain loads afterwards, withdrew without burdens.”

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Hawaii-Wilkes-map-1841
Hawaii-Wilkes-map-1841
Crater of Moku-A-Weo-Weo, Mauna Loa-Wilkes
Crater of Moku-A-Weo-Weo, Mauna Loa-Wilkes

Filed Under: Place Names, Prominent People, Economy, General Tagged With: Hawaii, Hawaii Island, Mauna Loa, Charles Wilkes

April 16, 2016 by Peter T Young 2 Comments

Hoʻopuloa

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)

“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”.

“(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)

“In 1926, there was a brief summit eruption, followed by 14 days of eruption on the southwest rift zone. A flow from this rift zone passed through a South Kona forest, crossed the main road on April 16, and pooled behind the coastal village of Hoʻopuloa.”

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)

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

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)

“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. The fiery lava engulfed the harbor and village of Hoʻopuloa, and now they are but a heap of pāhoehoe lava.”

“According to eyewitnesses of this engulfing lava, it was frightening seeing the lava coming down, and others say that it was truly awesome watching the flowing lava and its sweeping aside of all obstructions in its path.”

“The last word heard before the Hoku went to the press was that this Wondrous Woman of Halemaʻumaʻu returned to her Palace at Kilauea, and she is bringing to life her fires at the famed crater of Halemaʻumaʻu.”

“Perhaps her rage has been quenched as the skin of that woman has touched the sea, but the memory of the tragedy which befell the people of that section of Kona is heartbreaking.” (Hoku o Hawaii, April 20, 1926)

One enterprising youth used his small truck to haul water from the Hoʻopuloa tanks to Miloliʻi, the end of the road.

When the flow reached the sea, he and his truck were cut off; he later took his truck apart and transported it piece by piece by outrigger canoe to the road on the Kona side of Hoʻopuloa. (USGS)

“Between 0400 and 0900 HST on April 18, the flow buried the village, wharf and harbor and entered the ocean. As soon as lava began falling into the sea, steam shot up in jets. Hundreds of dead fish floated along the edge of the turbulent water that spread out from the contact area of hot rock and cold ocean.”

Hawaiians from Miloliʻi came in their canoes and gathered the dead fish for salting and preserving. Jaggar collected some dead, floating fish and noted that they were perfectly fresh and in no sense cooked. (USGS)

Destruction of the village was gradual and complete. … This was Hawaiian Volcano Observatory’s first real experience with property destruction by a lava flow. (USGS)

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© 2016 Hoʻokuleana LLC

Hoopuloa
Hoopuloa
Hoopuloa_lava_flow-1926
Hoopuloa_lava_flow-1926
Hoopuloa lava flow
Hoopuloa lava flow
Monument to Catholic church engulfed by lava, Hoopuloa, So. Kona, Hawaii Island-PP-29-6-031
Monument to Catholic church engulfed by lava, Hoopuloa, So. Kona, Hawaii Island-PP-29-6-031
Hoopuloa Landing-taken from anchorage-1904
Hoopuloa Landing-taken from anchorage-1904
Hoopuloa Landing-PP-29-6-002-1916
Hoopuloa Landing-PP-29-6-002-1916
Hoopuloa landing from Mauna Loa eruption, Hawaii Island - April 18, 1926-PP-29-6-013
Hoopuloa landing from Mauna Loa eruption, Hawaii Island – April 18, 1926-PP-29-6-013
Hoopuloa -June 21, 1926 (man by sign -- 1926 flow)-HMCS
Hoopuloa -June 21, 1926 (man by sign — 1926 flow)-HMCS
Hoopuloa -- June 21, 1926 (lava entering sea)-HMCS
Hoopuloa — June 21, 1926 (lava entering sea)-HMCS
Hoopuloa -- June 21, 1926 (large boulders in foreground)-HMCS
Hoopuloa — June 21, 1926 (large boulders in foreground)-HMCS
Hoopuloa -- June 21, 1926 (five figures near boardwalk)-HMCS
Hoopuloa — June 21, 1926 (five figures near boardwalk)-HMCS
Hoopuloa -- June 21, 1926 (figure near low peak)-HMCS
Hoopuloa — June 21, 1926 (figure near low peak)-HMCS
Hoopuloa -- June 21, 1926 (edge of lava flow)-HMCS
Hoopuloa — June 21, 1926 (edge of lava flow)-HMCS
Hoopuloa - June 21, 1926 (canoe on sea)-HMCS
Hoopuloa – June 21, 1926 (canoe on sea)-HMCS
Hoopuloa -- June 21, 1926 (brush in foreground -- lava)-HMCS
Hoopuloa — June 21, 1926 (brush in foreground — lava)-HMCS
Stamp with Hoopuloa postmark
Stamp with Hoopuloa postmark
Milolii_Beach Lots-Hoopuloa-Milolii-GoogleEarth
Milolii_Beach Lots-Hoopuloa-Milolii-GoogleEarth
Hoopuloa-Milolii-USGS-1925
Hoopuloa-Milolii-USGS-1925

Filed Under: Place Names Tagged With: Hawaii, Eruption, Mauna Loa, Volcano, Kona, Hoopuloa

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