Buffalo Soldiers

Before the Army’s 25th Infantry Division, stationed at Schofield Barracks on Oʻahu (formed in 1941,) for a while during the time of World War I (1913 - 1918) Hawaiʻi had the Army’s 25th Infantry Regiment.

The Division is known as the “Tropic Lightning;” the Regiment was known as the “Buffalo Soldiers.”

In 1866, Congress created six segregated regiments which were soon consolidated into four black regiments. They were the 9th and 10th Cavalry and the 24th and 25th Infantry.

"The officers say that the negroes make good soldiers and fight like fiends … the Indians call them 'buffalo soldiers' because their woolly heads are so much like the matted cushion that is between the horns of the buffalo." (Roe, Army Letters from an Officer’s Wife, 1871-1888)

Although African Americans have fought in America’s wars since the Revolution, they weren’t allowed to enlist in the Regular Army until after the Civil War (and, from July 28, 1866 - February 3, 1946, America’s Army was segregated.)

While the Buffalo Soldiers fought in the Spanish-American and Philippine-American Wars at the turn of the century, they did not see combat in World War I (1914 – 1918.)

At the time, the National Park Service did not exist, however a few National parks had been created: Yellowstone (1872,) Sequoia (1890,) Yosemite (1890,) Mount Rainier (1899,) Crater Lake, 1902,) Wind Cave, (1903,) Mesa Verde (1906,) Glacier (101) and Rocky Mountain (1910.)

Rather than fight, the Buffalo Soldiers and other Army regiments were assigned to duties at some National Parks.

The US Army served as the official administrator of Yosemite and Sequoia National Parks between 1891 and 1913; Buffalo Soldiers, like their white counterparts in US Army regiments, were among the first Park Rangers, and created a model for park management as we know it today.  (NPS)

In addition to bringing law and order to the mountain wilderness, their accomplishments included the completion of the first usable road into Giant Forest and the first trail to the top of Mt. Whitney (the tallest peak in the contiguous United States) in Sequoia National Park in 1903; and the building of an arboretum in Yosemite National Park near the south fork of the Merced River in 1904. One scholar considered the latter area to contain the first marked nature trail in the national park system.  (NPS)

Starting in 1906, George Lycurgus (operator of the Volcano House) and newspaperman Lorrin Andrews Thurston were working to have the Mauna Loa and Kilauea Volcanoes area made into a National Park.  In 1912, geologist Thomas Augustus Jaggar arrived to investigate and joined their effort.

Jaggar had tried to lead several expeditions to the top of Mauna Loa in 1914 but was unsuccessful due to the elevation (13,678 feet) and the harsh conditions: rough lava, violent winds, noxious fumes, shifting weather, extreme temperatures and a lack of shelter, water and food.  (Takara)

About 800 Buffalo Soldiers from the 25th Regiment had been assigned to garrison duty in Hawaiʻi at Schofield Barracks.  Given their experience in Parks on the continent, some of the soldiers were called upon to assist at the volcanoes on the Island of Hawaiʻi.

In September 1915, Jaggar, Thurston and a US Army representative conducted a survey to determine a route for a trail up Mauna Loa.

The following month, a local paper noted, “Soldiers Building Mountain Trail.  Negro soldiers of the Twenty-fifth Infantry to the number of 150 are at work constructing a trail from near the Volcano House to the summit of Mauna Loa. It is estimated that three or four weeks will be devoted to this work. The soldiers are doing the work as a part of their vacation exercises.”  (Maui News, October 29, 1915)

The Buffalo Soldiers built the 18-mile trail to the summit of Mauna Loa. They also built the ten-man Red Hill Cabin and a twelve-horse stable, so scientists could spend extended periods of time studying the volcano.

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 Kīlauea 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.

The National Park Service, within the federal Department of Interior, was created on August 25, 1916 by Congress through the National Park Service Organic Act.

The experience of working with the Army did not end with the construction of the Mauna Loa Trail, and Thurston's energy did not seem to wane. He continued to promote the Kīlauea area to the public and the military who he thought could benefit from, and would be a benefit to Kīlauea.  (NPS)

In 1916, Thurston, recognizing the long tradition of soldiers and sailors who had visited the area, proposed the establishment of a military camp at Kīlauea. Thurston promoted his idea and was able to raise enough funds through public subscription for the construction of buildings and other improvements.  By the fall of 1916 the first group of soldiers arrived at Kīlauea Military Camp (KMC.)  (NPS)

Later, in the 1930s, the Civilian Conservation Corps (CCC) built research offices, hiking trails and laid the foundations for much of the infrastructure and roads within the Hawaiʻi Volcanoes and other parks across the country.

On, July 1, 1961, Hawaiʻi National Park’s units were separated and re-designated as Haleakalā National Park and Hawaii Volcanoes National Park.

Oh, one more thing … another lasting legacy of the Buffalo Soldiers to the National Parks is the Ranger Hat (popularly known as the Smokey the Bear Hat) - with it the Montana Peak (or pinch) at the top of the hat; a recrease of the Stetson hat to better shed water when it rains.

The image shows members of the 25th Infantry Regiment while deployed to the Philippines (1899.)  In addition, I have added related images in a folder of like name in the Photos section on my Facebook and Google+ pages.

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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 is 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)

The 1790 explosion led to the death of one-third of the warrior party of Kaʻū Chief Keōuakūʻahuʻula (Keōua.)  At the time 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.  (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)  The image shows the 1924 eruption column rising from Halemaʻumaʻu near the end of the explosion, taken from outside Volcano House (Tai Sing Loo, USGS.)  I added a couple of other images in a folder of like name in the Photos section on my Facebook and Google+ pages.

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