TuTu Pele: The Living Goddess of Hawai'i's Volcanoes
…
6 pages
Sign up for access to the world's latest research
Abstract
Pele is known to virtually all who call the island of Hawai’i home, be they native Hawaiians or from foreign shores. Hawaiians recognize a vast polytheistic hierarchy similar to the ancient Greeks. Born of Haumea, Pele is one of 14 children. “The major gods represented the universal forces of nature....The lesser gods were usually associated with particular activities or places. Of these, the most famous is Pele, the volcano goddess.” When one speaks of Pele in contemporary Hawai’i, her name is oftentimes spoken with reverence and usually accompanied by the respectful title “Madame” or “Tūtū.” Unlike many of the Greek deities, however, Tūtū Pele has a variety of names and can transform her appearance: “She is Pele-honua-mea, Pele of the sacred land. She is Pele-‘ai-honua, Pele the eater of the land, when she devours the land with her flames....Her sacred name as a spirit is Ka-‘ula-o-ke-ahi, the redness of fire.” As such, Tūtū Pele can and, according to contemporary eye witnesses, does take many physical forms. Hawaiian historian Herb Kane states that “in folklore she may appear as a tall, beautiful young woman, or as an old woman, wrinkled and bent with age, sometimes accompanied by a white dog. When enraged she may appear as a woman all aflame or as pure flame.... To know Pele is to know the awe that the first Hawaiians must have felt when they came upon this huge island crowned with fiery volcanoes and trembling earthquakes.”
Related papers
Open-File Report, 1996
The most recent eruptions of Hualalai produced three lava flows and two flow fields from at least six different vents. Because they occurred early in the history of Hawai'i after contact with the western world, scientific descriptions of the events were not made. We have found a few details from a search of available sources including ship logs, missionary diaries, travel diaries, maps, early geologic papers, and Hawaiian legends. Of all the events, it is most certain that the Hu'ehu'e flow field occurred in 1801, but dates for the other eruptions are less certain. Most, if not all, of the descriptions of eruptive behavior may also be for the Hu'ehu'e flow. [This must be a reference to the Hu'ehu'eflow, which is pahoehoe, and not the Ka'upulehuflow, which is almost entirely 'a'a along its lower half.]
1995
1750(1) lava flow, contains phenocrysts of olivine and microphenocrysts of augite in a very fine granular nonporphyritic olivine basalt. The lava from Puu Pimoe is an olivine basalt containing phenocrysts of olivine (3%) and a few of augite in an internal groundmass composed of olivine (5%); augite (32%) ... ; labradorite (35%); interstitial andesine ... ; magnetite (15%); and pale-grown interstitial glass (5%). An older lava flow crossed by the coastal trail 1.2 miles southeast of Keoneoio, is similar to the Pimoe flow, but augite phenocrysts area more numerous, and interstitial andesine has not been recognized. The Historic (1750) Lava Flow The lava flow near Makena [Kanaio] erupted about the year 1750, probably in and from two separate vents low on the southwest rift. One flow originated at Kaluaolapa, at an altitude of 575 feet, and the other from a fissure at an altitude of 1,200 feet, a mile to the northeast. The two lavas are identical in composition in hand specimen and under the microscope. The rock is a picritic basalt of aa type, containing abundant phenocrysts of yellowish-green olivine up to 5 mm across and black augite as much as 8 mm across. The augites phenocrysts (18%) are pale purplish-brown, euhedral to subhedral in outline ... In places a number of such grains are grouped together to form glomerocrysts. The olivine phenocrysts (20%) are colorless in thin section ... The ground mass is interstitial, with an average grain size of .05 mm. It consists of olivine (5%); augite (25% } ... black glass (3%), heavily charged with-dusty iron ore. The lava was briefly described by Sidney Powers (1920) and a specimen collected by him was described by Washington and analyzed by Keyes (1928). Powers noted that the 1750 flow issued from Puu Pimoe, and Washington accepts this argument. Inasmuch as the 1750 flow and the flow from Puu Pimoe area entirely separate flows, probably of different age, there is some doubt as to which flow was analyzed by Miss Keyes. Washington's description, however, fits better the flow from Kaluaolapa, and on Powers' map the lava labeled "1750 flow" is the Kaluaolapa flow. It is probable, therefore, that the analysis is of the 1750 lava flow. (Stearns 1942:302-03). Historic Flow of 1750 A generally accepted fact is the recent historic flow that covered much of the coast from west Kanaio to Ke'one'oi'o. This flow, which significantly changed the coastline and formed La Perouse Bay, is of interest not only for the oral traditions surrounding it, but also the implications it has for similar flows and their social impact in Kanaio and A'uahi. The analysis in Stearns (1942) has been the basis of all subsequent dialogs and thus is here quoted in full. Historic Lava Flow Many of the lava flows in the summit depression and in the Ulupalakua-Nuu area are black and bare, obviously erupted in recent time. Two of the freshest are near La Perouse Bay. They are differentiated from the other Hana lavas ... simply because Hawaiian legend has recorded them. The upper one broke out of a fissure 1 1/4 miles south of Ulupalakua (Makena P.O.) on the south slope of the old cone, Pu'u Mahoe, at an altitude of 1,550 feet. [In actuality the fissure is on the south slope of Kemehunehune, at 4200 feet] The spatter bordering the fissure is covered with brush and the upper stretches of pahoehoe support a little vegetation. Farther seaward, where there is little rain and the aa clinker is very rough and open, the lava looks as fresh as some of the flows of Mauna Loa that have been poured out in the last 50 years. The flow is 3 miles long, 5 to 20 feet thick, and is an olivine augite porphyry. It extended the coast line about three-quarters of a mile. The lower flow broke out at Kalua 0 Lapa cone, which is on a fissure parallel to the upper vent, but a little to the eastward at an altitude of 575 feet. The flow is similar to the upper one and is covered with rough aa clinker and a little pahoehoe that congealed while changing to aa. It overlies the Mahoe flow but may have been laid down only a few hours or days later. Both flows contain large balls, or wrapped masses of aa typical of many Hawaiian lava flows. The earliest published record seems to indicate that the Lapa flow might be the historic flow and the Mahoe flow earlier, but the similarity of petrology and degree of weathering suggest simultaneous eruption. The opening of two distinct vents during one eruption on the same rift is common in Hawaii. The record appears in Dana, who states "The period of the last summit eruption is unknown. Mr. Bailey, of Wailuku, Maui, has stated that, according to an island tradition, a lateral eruption of the mountain occurred about 150 years since in the district of Honuaula of the southern part of East Maui, at an estimated elevation above the sea of about 400 feet. "(Dana 1890:278-79) This definitely describes the lower flow. The late Lorrin A. Thurston, a serious student of Hawaiian canoes and lore, published the following account, which confirms the recency of the eruption. It is quoted in full because many geologic writers have given categorically the date 1750 to the lava flow. Popular impression and report is to the effect that there is no record, or even tradition, of volcanic activity on the island of Maui, although the mute evidence thereof, both in the crater of Haleakala and on its outer slopes, is the shape of comparatively recent lava flows, are many and plain. Among more recent flows, one, especially, is quite as fresh in appearance as the 1801 flow from the western slope of Hualalai, in Kona, Hawaii, which was seen and the date recorded by a white resident. The writer shared the popular opinion, and, about 1879, remarked upon the supposed fact to Father Bailey, the venerable American missionary who came to Hawaii in 1837. He was stationed on Maui in 1841 and lived there for many years. In his usual deliberate drawl, Father Bailey replied: "That is not so!" "What do you know to the contrary?" I asked. He thereupon made in substance the following statement, which for 26 years was all that I heard concerning knowledge or tradition of volcanic activity on the island of Maui. "I was first stationed on Maui in 1841," said Father Bailey. "In my trips about the island I noticed a lava flow at Honuaula, at the south end of East Maui, which appeared much fresher than the other flows-much more so than it appears now (1879). "I asked the natives if they knew when that flow occurred, and they told me that their grandparents saw it. They also told me that a woman and child were surrounded by the flow, but escaped after it cooled." I have since visited the locality indicated by Father Bailey an examined several other recent appearing flows nearby. The government map of Maui shows three such flows, all in Honuaula and originating below the upper road around the island. The flow in question, manifestly the latest, begins about halfway down, between the upper road and the sea. It spreads to a width of a mile or so at the coast, having built quite a promontory out into the ocean. Its source is at a small hillock or crater, two rocky projections with perpendicular interior sides, a few feet apart, marking the spot from which the torrent of lava poured forth. The flow rapidly widening, ran to the sea, a distance of a couple of miles or so. The lava is rough aa, entirely devoid of vegetation, and looks as though it might have first seen daylight in the twentieth instead of the eighteenth century. The flow forms the western side of Keoneoio, or La Perouse Bay, named after the French explorer who landed there in 1780. The government lighthouse , known as the Kianu Light, is at the eastern point of the bay. The flow partially Halapepe Dracaena aurea H. Mann. On the Kula slopes of Maui there once existed a forest of this tree, the remnants of which can still be seen.(Rock: 109) On the lava fields of Auahi, on the southern slope of Haleakala, the tree is most numerous, but differs in many regards from the specimens found in the forest of Makawao on the same mountain. The leaves of the Auahi specimens are much smaller and more graceful.(Rock:112) 'Iliahi Santalum Freycinetiantum Gaud. On Lanai and East Maui on the southern slopes of Haleakala occurs Hillebrand's var. cuneatum, which differs from the species in its small thick, fleshy, suborbicular leaves, which are slightly cuneate at the base. It is usually shrub, but to the writer's astonishment it grew as a veritable vine, completely covering a species of Sideroxylon.(Rock:129) `Iliahi Santalum Haleakakalae Hbd. This species, which is easily distinguished from the other Hawaiian Sandalwoods by its dense corymbose inflorescence, which is bright scarlet, is peculiar to the Island of Maui, and at that confined to the eastern part Mt. Haleakala, after which mountain it was named by Hillebrand, who records it as a shrub. It is, however, also a tree, though not of any size; the highest trees observed by the writer were about 25 feet. It grows around the crater of Puunianiau, on the northeastern slope of Mt. Haleakala, at an elevation of 7000 to 9000 feet.(Rock: 133) It has been reported by Hillebrand to grow only at very high elevations near the summit of the mountain, together with Rainardia and Geranium. It may, however, be of interest to state that it was observed by the writer on the southern slopes of Haleakala on the lava flows of Auahi, Kahikinui, at an elevation of 2600 feet. At this locality, which is one of the richest botanical districts in the Territory, it is a fine-looking tree and does not show any of the signs of stiff branches and short, gnarled trunks, as, of course, must be expected at high altitudes. Were it not for the dense inflorescence and bright scarlet perigones, one could easily mistake it for Santalum ellipticum of Oahu, which it, in reality, resembles greatly.(Rock: 135) Mamani Sophora chrysophylla Seem. On Haleakala, Maui, the trees are of medium...
Journal of Volcanology and Geothermal Research, 2007
We present a detailed petrographic study of Pele's hairs and tears sampled from Masaya volcano (Nicaragua). This study provides new observations of these little-known pyroclastic objects using both secondary electron images (SEI) and back scattering electron images (BSEI). Our work shows that Pele's tears can be associated with Pele's hairs after their formation: tears can be trapped on the walls and/or in the cavities of Pele's hairs. Moreover, chemical investigations of the Pele's hairs and tears highlight the presence of a chemical zonation. The edge of these tears and hairs show a siliceous enrichment, allowing us to quantify the interaction time of the silicate glass with acid gases in the volcanic plume. This study confirms the syneruptive and post eruptive volatile exsolution from Pele's hairs and tears.
Asian and African Studies, 2009
I have analysed in this study the most completely recorded variants o f the Maui myths concerning the origin o f fire in eastern Polynesia. Those myths show the diversity o f form assumed in each island. No two islands have an identical myth about the origin o f fire. This diversity is most probably caused by narrative traditions and by individual interpretations made by each tribe. But the figure o f Maui which appears in the great majority o f noted myths o f eastern Polynesia confirms their common origin.
Changing Contexts, Shifting Meaning: Transformations of Cultural Traditions in Oceania. Book Editor(s): Elfriede Hermann (University of Hawai'i Press). , 2013
2017
you are my life long mentor and I feel honored to have had your wisdom and company during this academic pursuit. Kahakaʻio Ravenscraft, mahalo for your participation on my advisory committee and amazing contribution to the Oral History Project. You set the tone for this entire thesis based on your spiritual focus in ʻŌiwi culture and willing-open heart in sharing your manaʻo and ʻike.
Hawaiian, Marquesan, Tongan, and other prophetic women and priestesses
Journal of Volcanology and Geothermal Research, 2021
. Tracking the behaviour of persistently degassing volcanoes using noble gas analysis of Pele's hairs and tears: A case study of the Masaya volcano (Nicaragua). Journal of Volcanology and Geothermal Research, 414, article no. 107212. For guidance on citations see FAQs.
Patricia 'Iolana, PhD