Template:Short description Template:For Template:Good article Template:Use mdy dates Template:Infobox mountain
Kīlauea (Template:IPAc-en Template:Respell, {{#invoke:IPA|main}}) is an active shield volcano in the Hawaiian Islands. It is located along the southeastern shore of Hawaii Island. The volcano is between 210,000 and 280,000 years old and grew above sea level about 100,000 years ago. Since the islands were settled, it has been the most active of the five volcanoes that together form the island and among the most active volcanoes on Earth. The most recent eruption began in December 2024, with episodic lava fountains and flows continuing into 2025.
Kīlauea is the second-youngest product of the Hawaiian hotspot and the current eruptive center of the Hawaiian–Emperor seamount chain. Because it lacks topographic prominence and its activities historically coincided with those of Mauna Loa, Kīlauea was once thought to be a satellite of its much larger neighbor. Kīlauea has a large, fairly recently formed caldera at its summit and two active rift zones, one extending Template:Convert east and the other Template:Convert west. An active fault of unknown depth moves vertically an average of Template:Convert per year.
Between 2008 and 2018, Halemaʻumaʻu, a pit crater located within Kīlauea's summit caldera, hosted an active lava lake. Kīlauea erupted nearly continuously from vents on its eastern rift zone between January 1983 and April 2018, causing major property damage, including the destruction in 1990 of the towns of Kalapana and Kaimū along with the community's renowned black sand beach.
Beginning in May 2018, activity shifted further downrift from the summit to the lower Puna district, during which lava erupted from two dozen vents with eruptive fountains that sent rivers of lava into the ocean in three places. The eruption destroyed Hawaii's largest natural freshwater lake, covered substantial portions of Leilani Estates and Lanipuna Gardens, and destroyed the communities of Kapoho, Vacationland Hawaii, and most of the Kapoho Beach Lots.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref><ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> The County of Hawaii reported that 716 dwellings were destroyed.<ref name="USGS2018summary">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> Concurrent with the activity downrift in lower Puna, the lava lake within HalemaTemplate:OkinaumaTemplate:Okinau drained and a series of explosive collapse events occurred at the volcano's summit, with at least one explosion emitting ash Template:Convert into the air. This activity prompted a months-long closure of the Kīlauea section of Hawaii Volcanoes National Park.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> The eruption ended in September 2018.<ref name="USGS2018summary" /> Since 2020, several eruptions have occurred within the enlarged Halemaʻumaʻu crater from the 2018 collapse events as well as along the volcano's southwest and east rift zones.
BackgroundEdit
Kīlauea is a Hawaiian word that means "spewing" or "much spreading", referring to its frequent outpouring of lava. Its earliest lavas date back to its submarine preshield stage. Samples were recovered by remotely operated underwater vehicles; samples of other flows were recovered as core samples. Lavas younger than 1,000 years old cover 90 percent of the volcano's surface. The oldest exposed lavas date back 2,800 years.
Radiocarbon and paleomagnetic dating identified a major eruption of Kīlauea around 1410, the first to be mentioned in Native Hawaiians' oral history.<ref name=":0">Template:Cite journal</ref> Western contact and written history began in 1778. The first documented eruption of Kīlauea came in 1823 with repeated eruptions thereafter. Most occurred at the volcano's summit or its eastern rift zone, and were prolonged and effusive. The geological record shows that pre-contact explosive activity was common; in 1790 one such eruption killed more than 400 people, making it the deadliest volcanic eruption in what became the United States.<ref name="1790 eruption">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
Kīlauea's eruption from January 3, 1983, to 2018 was by far its longest-duration period of activity in modern times, as well as one of the longest-duration eruptions documented on Earth; as of January 2011, the eruption had produced Template:Convert of lava and resurfaced Template:Convert of land. Centuries prior to this event, the even larger ʻAilāʻau eruption of 1410 lasted about 60 years, ending in 1470 with an estimated volume of Template:Convert.<ref name=":1">Template:Cite journal</ref>
Kīlauea's activity has a major impact on its mountainside ecology, where plant growth is often interrupted by fresh tephra and drifting volcanic sulfur dioxide, producing acid rains particularly in a barren area south of its southwestern rift zone known as the Kaʻū Desert. Nonetheless, wildlife flourishes left undisturbed elsewhere on the volcano and is highly endemic thanks to Kīlauea's (and the island of HawaiTemplate:Okinai's) isolation from the nearest continental landmass. Historically, the island's five volcanoes were considered sacred by the Hawaiian people, and in Hawaiian mythology HalemaTemplate:OkinaumaTemplate:Okinau served as the body and home of Pele, goddess of fire, lightning, wind, and volcanoes.<ref name="Alia Wong">Template:Cite news</ref>
English missionary William Ellis gave the first modern account of Kīlauea and spent two weeks exploring the volcano. Since its foundation by Thomas Jaggar in 1912, the Hawaiian Volcano Observatory, for many years located on the rim of Kīlauea's summit caldera (Kaluapele), has served as the principal investigative and scientific body on the volcano and the island. In 1916, a bill forming Hawaii Volcanoes National Park was signed into law by President Woodrow Wilson. The park is a World Heritage Site and a major tourist destination, attracting roughly 2.6 million visitors annually.
GeologyEdit
SettingEdit
<imagemap> File:Location Kilauea.svg|thumb|Location of Kīlauea on [[Hawaii (island)|HawaiTemplate:Okinai island]]
poly 65 65 97 105 138 126 229 113 236 134 207 171 174 180 151 201 139 237 121 259 97 286 57 261 48 240 56 197 39 159 60 157 85 127 63 90 47 90 54 74 Mauna Loa poly 67 55 66 65 99 106 121 115 140 127 213 116 215 88 186 59 121 33 106 52 Mauna Kea poly 39 158 61 159 85 127 65 89 40 89 20 105 20 122 Hualalai poly 67 54 106 53 120 35 87 20 85 10 63 2 51 6 54 33 Kohala (mountain)
desc bottom-left </imagemap>
Like all Hawaiian volcanoes, Kīlauea was formed as the Pacific tectonic plate moved over the Hawaiian hotspot in the Earth's underlying mantle.<ref name="usgs-2007">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> Hawaii island volcanoes are the most recent evidence of this process that, over 70 million years, has produced the Template:Convert-long Hawaiian–Emperor seamount chain.<ref name="Watson">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> The prevailing view is that the hotspot has been largely stationary within the planet's mantle for much of the Cenozoic Era.<ref name="Watson"/><ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> However, while the Hawaiian mantle plume is well understood and extensively studied, the nature of hotspots themselves remains uncertain.<ref>Template:Cite book</ref>
Kīlauea is one of five subaerial (originating under water) volcanoes that make up the island of Hawaii, originated from the Hawaiian hotspot.<ref name=hvo-kilauea>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> The oldest volcano on the island, Kohala, is more than a million years old,<ref name="hvo-kohala">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> while Kīlauea, the youngest, is between 300,000 and 600,000 years of age.<ref name=hvo-kilauea/> Kamaʻehuakanaloa (the ruddy, reddish child of Kanaloa,<ref name=":5">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> formerly Lōʻihi), on the island's flank, is younger and has yet to breach the surface.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> Thus Kilauea is the second youngest volcano in the Hawaiian–Emperor seamount chain, a chain of shield volcanoes and seamounts extending from Hawaii to the Kuril–Kamchatka Trench in Russia.<ref name="USGS Hotspots">Template:Cite book</ref>
Kīlauea started as a submarine volcano, gradually growing larger and taller via underwater eruptions of alkali basalt lava before emerging from the sea with a series of explosive eruptions<ref name=hov-evolution>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> about 50,000 to 100,000 years ago. Since then, the volcano's activity has produced a continual stream of effusive and explosive eruptions of roughly the same pattern as its activity since records began to be kept.<ref name=hvo-eruptive />
Hawaii island's oldest volcano, Kohala, experienced almost 900,000 years of activity before going extinct.<ref name=hvo-kohala /> Eruptions and explosive activity will make Kīlauea taller, build up its rift zones, and fill and refill Kaluapele.<ref name=hvo-eruptive/>
StructureEdit
Kīlauea has been active throughout its history.<ref name=hvo-eruptive/> Cinder cones, satellite shields, lava tubes, and other eruptive structures are present, evidence of its recent activity.<ref name="osu-landforms" /> Since 1918, Kīlauea's longest pause lasted 18 years between 1934 and 1952.<ref name=soest-hist /> The bulk of Kīlauea consists of solidified lava flows, intermixed with volcanic ash and tephra produced by lower-volume explosive eruptions.<ref name=hvo-eruptive>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> Much of the volcano is covered in historical flows, while 90 percent of its surface is from the last 1,100 years.<ref name=usgs-hazard>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> Much of its bulk remains underwater;<ref name=hov-evolution/> its subaerial surface is a gently sloping, elongate, decentralized shield with a surface area of approximately Template:Convert,<ref name=usgs-erz /> making up 13.7 percent of the island's total surface area.<ref name=hvo-kilauea/>
Kīlauea lacks topographical prominence, appearing only as a bulge on the southeastern flank of Mauna Loa. Native Hawaiians and early geologists considered it an active satellite of its host. However, lava analysis shows that the two have separate magma chambers. Nonetheless, high activity at one volcano roughly coincides with low activity at the other. When Kīlauea lay dormant between 1934 and 1952, Mauna Loa became active, and when the latter remained quiet from 1952 to 1974, the reverse was true. This is not always the case; the 1984 eruption of Mauna Loa started during an eruption at Kīlauea, but had no discernible effect on the Kīlauea eruption, and the ongoing inflation of Mauna Loa's summit, indicative of a future eruption, began the same day as new lava flows at Kīlauea's [[Puʻu ʻŌʻō|PuTemplate:Okinau Template:OkinaŌTemplate:Okinaō]] crater. In 2002, Kilauea experienced a high-volume effusive episode at the same time that Mauna Loa began inflating. This unexpected communication is evidence of crustal-level interactions between them.<ref>Template:Cite journal</ref> Geologists suggested that "pulses" of magma entering Mauna Loa's deeper magma system may have increased pressure inside Kīlauea and triggered the concurrent eruptions.<ref name="hvo-loa_kilauea">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> Mauna Loa began erupting on November 27, 2022, during Kīlauea's ongoing eruption, the first time since 1984 that both volcanoes were simultaneously erupting.
KaluapeleEdit
Kīlauea has a large summit caldera named Kaluapele (the pit of Pele),<ref name=":5" /> measuring Template:Convert with walls up to Template:Convert high, breached by lava flows on the southwestern side.<ref name="soest-hist" /> The age of Kaluapele is unknown, and it is possible that it has appeared and disappeared multiple times.<ref name="hvo-eruptive" /> Kaluapele likely formed over several centuries, beginning about 500 years ago,<ref name="usgs-pamphlet">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> while its present form was finalized around 1470–1510 after a particularly powerful eruption from 1410 to 1470.<ref name="hvo-eruptive" /> A major feature within Kaluapele is HalemaTemplate:OkinaumaTemplate:Okinau, a large pit crater and one of Kīlauea's most historically active eruption centers. The crater is approximately Template:Convert in diameter and Template:Convert deep, but its form has varied widely; its floor is mostly covered by flows from its 1974 eruption.<ref name="wisconsin">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
Rift zonesEdit
Kīlauea has two rift zones radiating from its summit, one leading Template:Convert out to the east, the other Template:Convert long and trending towards the southwest.<ref name="hvo-eruptive" /> A series of fault scarps connecting the rift zones form the [[Koa'e Fault Zone|KoaTemplate:Okinae Fault Zone]]. Tectonic extension along them is causing Kīlauea's bulk to slowly slide seaward off its southern flank at a rate of about Template:Convert per year, centered on a basal décollement fault Template:Convert beneath the volcano's surface.<ref name="agu-swrz" /> The eastern rift zone is a dominant feature on the volcano; it is almost entirely covered in lava from the last 400 years, and at its crest near the summit is Template:Convert wide.<ref name="usgs-erz" /> Non-localized eruptions, typical of rift zone activity,<ref name="hvo-eruptive" /> have produced a series of low-lying ridges down the majority of the east rift zone's length.<ref name="usgs-erz">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> Its upper segment is the most active section.<ref name="usgs-hazard" /><ref name="usgs-pamphlet" /> It is the site of large pit craters.<ref name="osu-landforms">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> It reaches down Kīlauea's submerged flank to a depth of more than Template:Convert.<ref name="usgs-pamphlet" /> By contrast, the much smaller southwestern rift zone last had a rifting episode in 1974, and has not been active in the current eruptive cycle.<ref name="agu-swrz">Template:Cite journal</ref> The southwestern rift zone's extremity is underwater, although its subaerial length is more limited. The southwestern rift zone lacks a well-defined ridge line and pit craters, evidence that it is less active than the eastern rift zone.<ref name="usgs-pamphlet" />
Hilina fault systemEdit
A prominent structure on Kīlauea's southern flank is the Hilina fault system, an active fault slipping vertically an average of Template:Convert per year.Template:Clarify Its physiographic province is Template:Convert deep, but it is unknown whether it is a shallow listric fault or penetrates deeply.<ref name="usgs-2007" />
Eruptive historyEdit
Template:See alsoAll historical eruptions occurred at either Kaluapele, the eastern rift zone, or the southwestern rift zone.<ref name="hvo-kilauea" /> Half of Kīlauea's historical eruptions have occurred at or near Kaluapele. Activity there was nearly continuous for much of the 19th century, capped by an explosive eruption in 1924, before petering out by 1934. Later activity mostly shifted to the eastern rift zone, the site of 24 historical eruptions, located mostly on its upper section. By contrast, the southwestern rift zone remained relatively quiet, hosting five events.<ref name="hvo-eruptive" />
Prehistoric eruptionsEdit
Geologists dated and documented dozens of major eruptions over the volcano's history, bridging the gap between Kīlauea's oldest known rock and written records and historical observation.<ref name=gvp-dates/> Lava flows are generally recovered by scientists in one of three ways. The oldest flows, 275,000 to 225,000 years ago, were recovered from Kīlauea's submerged southern slope by remotely operated vehicles. These lavas exhibit forms characteristic of early, submerged preshield-stage eruptive episodes, from when the volcano was a rising seamount yet to breach the ocean surface,<ref name=hvo-dates>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> and their surface exposure is unusual, as in most other volcanoes such lavas would have since been buried by later flows.<ref name=usgs-2007 />
The second method is by drilling core samples; however, the cores are difficult to date. Paleomagnetic dating, limited to rocks dating from after Kīlauea's emergence from the sea, suggested ages of around 50,000 years. Exposed flows above sea level are younger. Some of the oldest reliably dated rock is 43,000 years old. It comes from charcoal sandwiched beneath an ash layer on a fault scarp known as Hilina Pali; however, samples dated from higher up the scarp indicate ash deposition at an average rate of Template:Convert per thousand years, indicating that the oldest exposed flows, from the base of the feature, could date back as far as 70,000 years.<ref name=hvo-dates/> This date is similar to that of the oldest dated extant lava flow, a southwestern rift zone flow with uncorrected radiocarbon dating of approximately 4650 BC.<ref name=gvp-dates>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
The oldest well-studied eruptive product from Kīlauea is the Uwēkahuna Ash Member, the product of explosive eruptions from 800 to 100 BC. Although it was mostly buried by younger flows, it remained exposed in some places, and was traced more than Template:Convert from Kaluapele, evidence of powerful eruptions. Evidence suggests the existence of an active eruptive center at this time, termed the Powers Caldera, whose fractures and faults lie Template:Convert outside Kaluapele. At least 1,200 years ago, lava from the Powers Caldera overtopped its rim and solidified the structure; this was followed by a period of voluminous tube-fed pāhoehoe flows from the summit. Following the end of activity around 1600 CE, eruptions moved to the eastern part of Kīlauea's summit, and concurrently activity increased at the northern end of the eastern rift zone.<ref name=usgs-pamphlet />
1410 to 1790Edit
The longest-duration major eruption witnessed by Native Hawaiians took place from about 1410 to 1470. Lasting around 60 years, the Template:OkinaAilāTemplate:Okinaau eruption's effusive flow covered most of Kīlauea, north of the East Rift Zone in what became the Puna District.<ref name=":2">Template:Cite journal</ref> Most likely due to the duration of this flow, the summit collapsed around 1470–1510, creating Kaluapele. These discoveries and the collapse of the summit were supplemented by translations of Native Hawaiian chants on the mythology of Pele and [[Hiʻiaka|HiTemplate:Okinaiaka]]; these events were interpreted from this story.<ref name=":0"/><ref name=":4">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
After arriving in Hawaii, Pele made Kīlauea her home. She sent her sister HiTemplate:Okinaiaka to retrieve LohiTemplate:Okinaau, an attractive man she met on KauaTemplate:Okinai, on the condition that Pele protect the forests of Puna if HiTemplate:Okinaiaka returned in 40 days. As the journey lasted longer than 40 days, Pele set fire to the forest. When HiTemplate:Okinaiaka finally returned with LohiTemplate:Okinaau and made the smoky discovery, she became angry and made love to LohiTemplate:Okinaau right in front of Pele. In retaliation, Pele then killed LohiTemplate:Okinaau before throwing him in a pit on the summit of Kīlauea. HiTemplate:Okinaiaka started digging ferociously to recover his body, letting rocks fly everywhere.
These events are interpreted to describe the Template:OkinaAilāTemplate:Okinaau flow.<ref name=":0" /><ref name=":4" /> In addition to Hawaiian oral history, geologists studied and confirmed them with radiocarbon and paleomagnetic dating.<ref name=":2" />
Kīlauea then entered a 300-year period of explosive eruptions from around 1510 to 1790 as discovered by the radiocarbon dating of the Keanakākoʻi (the cave in which adzes were made) Tephra.<ref name=":1" /><ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> This tephra was formed after lava erupted hundreds of meters into the sky and spread ash across the area.<ref name=":3">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
1790 to 1934Edit
The earliest reliable written records date to about 1820,<ref name="footprints" /> and the first eruption well-documented by westerners occurred in 1823.<ref name="hvo-eruptive" /> One pre-contact eruption in particular, a phreatomagmatic event in 1790,<ref name="soest-hist">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> was responsible for the death of a party of warriors, part of the army of [[Keoua Kuahuula|Keōua KuahuTemplate:Okinaula]], the last Hawaii island chief to resist Kamehameha I's rule; their death is evidenced by footprints preserved within the Hawai‘i Volcanoes National Park - it is listed on the National Register of Historic Places.<ref name="footprints">Template:Cite journal</ref> Kīlauea was the site of 61 separate eruptions between 1823 and 2024, making it one of Earth's most active volcanoes.<ref name="hvo-kilauea" /><ref name="soest-hist" />
The volume of lava expelled by Kīlauea varied widely across eruptions. After 1823 Kaluapele gradually filled, filling up under nearly continuous summit eruption, with Template:Convert of lava released by 1840. The period between 1840 and 1920 saw approximately half that in lava volume. In the thirty years between then and about 1950, the volcano was unusually quiet and exhibited little activity; Kīlauea's eruptive volume increased steadily thereafter, with activity comparable to that of the early 1800s.<ref name="hvo-eruptive" />
The length and origin of these eruptions varied. Events lasted anywhere between days and years, and occurred at a number of different sites. Activity around Kaluapele was nearly continuous for much of the 19th century, and after a reprieve between 1894 and 1907, continued until 1924.
Effusive eruptions are of relatively recent vintage there. Prior to the arrival of Europeans, Kīlauea was the site of regular explosive activity, evidenced by tribal chants.<ref name=hov-explosive />
Kīlauea erupted in 1823 and 1832, but the first major eruption after 1790 occurred in 1840, when its eastern rift zone became the site of a large, effusive Hawaiian eruption over Template:Convert of its length, unusually long even for a rift eruption.<ref name="hvo-1840">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> The eruption lasted for 26 days and produced an estimated 205 to 265 million cubic meters of lava;<ref name="soest-hist" /> the light generated by the event was so intense that one could reportedly read a newspaper in Hilo at night, Template:Convert away.<ref name="hvo-1840" />
The volcano was active again in 1868, 1877, 1884, 1885, 1894, and 1918,<ref name=soest-hist/> before its next major eruption in 1918–1919. HalemaTemplate:OkinaumaTemplate:Okinau, then a small upwelling in Kaluapele floor, was topped by a lava lake that then drained and refilled, forming a lava lake and nearly reaching the top edge of Kaluapele before draining once more. This activity eventually gave way to the construction of Mauna Iki, building up the lava shield on the volcano's southwest rift zone over eight months. The eruption featured concurrent rift activity and lava fountaining.<ref name=hvo-1919>{{#invoke:citation/CS1|citation |CitationClass=web
}}</ref>
Activity in 1921–1923 followed.<ref name=soest-hist/> The next major eruption occurred in 1924. HalemaTemplate:OkinaumaTemplate:Okinau first drained, then quickly began sinking, deepening to nearly Template:Convert beneath a thick cloud of volcanic ash. Explosive activity began on May 10, blowing out rock chunks weighing as much as Template:Convert Template:Convert, and smaller fragments weighing about Template:Convert as far as Template:Convert. After a brief reprieve, the eruption intensified through a major blast on May 18, when an enormous explosive event caused the eruption's only fatality. The eruption continued and formed numerous eruption columns above Template:Convert in height, declining and ending by May 28.<ref name=hov-explosive>{{#invoke:citation/CS1|citation
|CitationClass=web }}</ref><ref name=usgs-1924>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> Volcanic activity was soon confined to the summit, and ended after 1934.<ref name=soest-hist/> From 1823 to 1924, the volcano erupted 15 times, with an additional 11 subsidence events occurring at the summit.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
1952 to 1982Edit
After the HalemaTemplate:OkinaumaTemplate:Okinau event, Kīlauea remained relatively quiet, and for a time, completely silent, with activity confined to the summit.<ref name=soest-hist/> The volcano came alive again in 1952, with a lava fountain Template:Convert high at HalemaTemplate:OkinaumaTemplate:Okinau. Multiple continuous lava fountains between Template:Convert persisted, and the eruption lasted 136 days.<ref name=hvo-1952>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> Eruptions followed in 1954, 1955, and 1959, capped by a large event in 1960, when fissure-based phreatic eruption and earthquake activity gave way to a massive [[a'a|Template:OkinaaTemplate:Okinaā]] flow overran evacuated communities and resorts; the resulting summit deflation eventually caused HalemaTemplate:OkinaumaTemplate:Okinau to collapse even further.<ref name=hvo-1960>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
After 1960 eruptive events occurred frequently until August 2018. The period 1967–1968 saw a particularly large, 80-million-cubic-meter, 251-day event from HalemaTemplate:OkinaumaTemplate:Okinau.<ref name=soest-hist/> In 1969 the marathon Mauna Ulu eruption was an effusive eruption that lasted from May 24, 1969, to July 24, 1974, and added Template:Convert of land to the island. Afterwards a magnitude 7.2 earthquake caused a partial summit collapse, after which activity paused until 1977.<ref name=hvo-1969>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> At the time, Mauna Ulu was the longest flank recorded eruption of any Hawaiian volcano. The eruption formed a new vent, covered a large area of land with lava, and enlarged the island. The eruption started as a fissure between two pit craters, Template:OkinaĀloTemplate:Okinai and Template:OkinaAlae, where the Mauna Ulu shield eventually formed. Both pāhoehoe and [[Block lava|Template:OkinaaTemplate:Okinaā]] lava erupted from the volcano. Fountains of lava surged as much as 540 meters (1772 ft) into the air. In early 1973, an earthquake occurred that caused Kīlauea to briefly stop erupting near Mauna Ulu and instead erupt near the craters Pauahi and HiTemplate:Okinaiaka.<ref name=hvo-1969/>
1983–2018Edit
{{#invoke:Labelled list hatnote|labelledList|Main article|Main articles|Main page|Main pages}}
Another eruption occurred from January 1983 to September 2018. It had the longest duration of any observed eruption at this volcano. Template:As of, it was the twelfth-longest duration volcanic eruption on Earth since 1750.<ref name="GVPDatabase2020-12">Template:Cite journal</ref> The eruption began on January 3, 1983, along the eastern rift zone. The vent produced lava fountains that quickly built up into the Puʻu ʻŌʻō cone, sending lava flows downslope.
In 1986, activity shifted down the rift to a new vent, named KūpaTemplate:Okinaianahā, where it took on a more effusive character. KūpaTemplate:Okinaianahā built up a low, broad volcanic shield, and lava tubes fed flows extending 11 to 12 km (about 7 mi) to the sea. Between 1986 and 1991, the connection between Chain of Craters Road and Hawaii Route 130 was cut, and the community of Kapa’ahu, the village of Kalapana, and the subdivisions of Kālapana Gardens and Royal Gardens were lost to the lava.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> A black sand beach at Kaimū was engulfed.<ref name="Kaimu">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> In 1992, the eruption moved back to Puʻu ʻŌʻō, but continued in the same manner, covering nearly all of the 1983–86 lava flows and large areas of coastline.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
As of the end of 2016, the east rift zone eruption had produced Template:Convert of lava, covered Template:Convert of land, added Template:Convert of land to the island, destroyed 215 structures, and buried Template:Convert of highway under lava as thick as Template:Convert.<ref name=hvo-1983-summary>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
In addition to the nearly continuous activity at PuTemplate:Okinau Template:OkinaOTemplate:Okinao and other vents on the east rift zone, a separate eruption began at Kilauea's summit in March 2008. On March 19, 2008, following several months of increased sulfur dioxide emissions and seismic tremor, a new vent opened at HalemaTemplate:OkinaumaTemplate:Okinau. Following this event, a new crater formed in the explosion, informally named the "Overlook Crater," emitting a thick gas plume that obscured views into the vent. Explosive events occurred at the vent throughout 2008.<ref name=hvo-2008-summary>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
On September 5, 2008, scientists observed a lava pond deep within the Overlook Crater for the first time. Beginning in February 2010, a lava pond was visible at the bottom of the crater almost continuously through the beginning of May 2018. Lava briefly overflowed the vent onto the floor of HalemaTemplate:OkinaumaTemplate:Okinau in April and May 2015, October 2016, and April 2018.<ref name=hvo-2008-summary /><ref>Global Volcanism Program, 2017. Report on Kilauea (United States). In: Venzke, E (ed.), Bulletin of the Global Volcanism Network, 42:8. Smithsonian Institution.</ref><ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
2018 eruptive episodesEdit
{{#invoke:Labelled list hatnote|labelledList|Main article|Main articles|Main page|Main pages}}
Beginning in March 2018, Hawaiian Volcano Observatory began to detect rapid inflation at Pu‘u ‘Ō‘ō,<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> leading scientists to warn that the increased pressure could form a new vent at Kilauea.<ref>Template:Cite news</ref>
Following weeks of increased pressure, the crater floor of the cone of Puʻu ʻŌʻō collapsed on April 30, 2018, as magma migrated underground into the lower Puna region of Kilauea's lower east rift zone.<ref name=volcanowatch-2018-05-06>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> Over the next few days, hundreds of small earthquakes were detected on Kīlauea's East rift zone, leading officials to issue evacuation warnings. On May 3, 2018, new fissures formed, and lava began erupting in lower Puna after a 5.0 earthquake earlier in the day, causing evacuations of the Leilani Estates and Lanipuna Gardens subdivisions.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref><ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
A seemingly related 6.9 magnitude earthquake occurred on May 4.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> By May 9, 27 houses had been destroyed in Leilani Estates.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref><ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
By May 21, two lava flows had reached the Pacific Ocean, creating thick clouds of laze (a toxic lava and haze cloud made up of hydrochloric acid and glass particles).<ref>Template:Cite news</ref>
By May 31, lava had destroyed 87 houses in Leilani Estates and nearby areas, accompanied by additional evacuation orders, including for the town of Kapoho.<ref>Template:Cite news</ref><ref>Template:Cite news</ref> By June 4, the lava had crossed through Kapoho and entered the ocean. The confirmed number of houses lost reached 159,<ref>Template:Cite news</ref> then two weeks later, 533,<ref>{{#invoke:citation/CS1|citation |CitationClass=web
}}Template:Dead link</ref> and ultimately 657.<ref>Template:Cite news</ref>
The lava lake at HalemaTemplate:OkinaumaTemplate:Okinau began to drop on May 2.<ref name=volcanowatch-2018-05-06 /> The Hawaiian Volcano Observatory warned that this increased the potential for phreatic (steam) explosions at the summit caused by interaction of magma with the underground water table, similar to the explosions that occurred at HalemaTemplate:OkinaumaTemplate:Okinau in 1924. These concerns prompted the closure of HawaiTemplate:Okinai Volcanoes National Park.<ref>{{#invoke:citation/CS1|citation
|CitationClass=web }}</ref> On May 17, at approximately 4:15 a.m., an explosive eruption occurred at HalemaTemplate:OkinaumaTemplate:Okinau, creating a plume of ash 30,000 feet into the air.<ref>Template:Cite news</ref> This marked the beginning of a series of vigorous explosions that produced significant ash plumes from HalemaTemplate:OkinaumaTemplate:Okinau.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> These explosions, accompanied by large earthquakes and inward slumping and collapse within and around HalemaTemplate:OkinaumaTemplate:Okinau, continued until early August.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref><ref>Changes in the Kīlauea caldera from May 14 to July 19, 2018 (Planet Labs Inc.)</ref>
2019–20: Water lake appears at the summitEdit
In late July 2019, a water lake appeared on the bottom of HalemaTemplate:OkinaumaTemplate:Okinau for the first time in over 200 years,<ref name="volcanowatch 2019-08-01">Template:Cite news</ref> as water from the rebounding water table began to enter the crater. The crater lake gradually grew in size.<ref name="recently formed">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> On December 1, 2020, the lake was approximately Template:Convert deep.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> Meanwhile, the temperature of the lake's surface, as measured by a thermal camera, generally measured between Template:Convert.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> Within a month, the water lake was replaced by a lava lake during the new eruption.
December 2020 – May 2021 summit eruptionEdit
On December 20, 2020, at 9:30 pm local time, an eruption broke out within HalemaTemplate:OkinaumaTemplate:Okinau. The Hawaiian Volcano Observatory reported that three vents were feeding lava into the bottom of HalemaTemplate:OkinaumaTemplate:Okinau Crater, boiling off the water lake that had been growing since summer 2019 and replacing it with a lava lake.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> The eruption produced a plume that reached Template:Convert in the air. The eruption was preceded by earthquake swarms centered at Kaluapele on November 30, 2020, and December 2, 2020, the second of which was interpreted as a small intrusion of magma.<ref name="2020eruption">Template:Cite news</ref> By the following morning, the eruption had stabilized. Two of the three vents remained active and continued to fill the floor with lava.<ref name="Dec 21 update">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> By 7:30 a.m. on December 25, 2020, the lava lake had filled in Template:Convert of the crater,<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> On January 8, 2021, depth had increased to Template:Convert,<ref name="Jan 8 update">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> and by February 24 to Template:Convert. A spatter cone had formed around the western vent.<ref name="Feb 24">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
The eruption continued for another few months, with decreasing activity. On May 26, 2021, it was no longer erupting. Lava supply appeared to have ceased between May 11 and May 13, and the lake had crusted over by May 20. The last surface activity in HalemaTemplate:OkinaumaTemplate:Okinau was observed on May 23.<ref name="VNS update 2021-05-27">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref><ref>Template:Cite news</ref> When activity ceased, the lava lake was Template:Convert deep.<ref>Template:Cite news</ref>
On August 23, 2021, the Hawaiian Volcano Observatory raised Kīlauea's alert status from "Yellow/Advisory" to "Orange/Watch" due to an earthquake swarm and a concurrent increase in ground deformation at the summit.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> The observatory returned Kīlauea's alert status to "Yellow/Advisory" two days later.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
September 2021 summit eruptionEdit
[[File:Kīlauea volcano - HalemaTemplate:OkinaumaTemplate:Okinau crater eruption in 2023 (C0608).webm|thumb|Eruptive activity within HalemaTemplate:OkinaumaTemplate:Okinau crater in January 2023]] The Hawaiian Volcano Observatory recorded increased earthquake activity and changes in ground deformation patterns at Kīlauea's summit at about noon local time on September 29, 2021.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> An eruption began at 3:20 p.m. local time when several fissures opened within HalemaTemplate:OkinaumaTemplate:Okinau crater.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> During the initial stages of the eruption, lava erupted in fountains more than Template:Convert tall. The fountain heights declined as the level of lava in the crater rose, partially drowning the erupting vents.<ref>Template:Cite news</ref>
Lava continued to erupt at HalemaTemplate:OkinaumaTemplate:Okinau throughout the fall. Overflight measurements from October 5, 2022, indicated that Template:Convert of lava had been effused, and that the floor of HalemaTemplate:OkinaumaTemplate:Okinau had risen Template:Convert, since the beginning of this eruption.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref><ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> The eruption paused on December 9, and the alert level was reduced accordingly on December 13, 2022, though seismic activity was still unsettled.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
2023 summit eruptionsEdit
Eruptive activity within HalemaTemplate:OkinaumaTemplate:Okinau resumed on January 5, 2023.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> The eruption ended 61 days later on March 7, 2023.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
On June 7, 2023, the Hawaiian Volcano Observatory detected a glow in web camera images atop Kilauea, indicating that an eruption had begun in the HalemaTemplate:OkinaumaTemplate:Okinau crater, within Hawaii Volcanoes National Park.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> The eruptive episode ended after twelve days on June 19, 2023.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
2023's third HalemaTemplate:OkinaumaTemplate:Okinau eruption episode occurred from September 10 to September 16, 2023, when multiple vents opened.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
2024 – 2025 eruptionsEdit
Shortly after midnight on June 3, 2024, an eruption occurred from a series of fissures on Kīlauea's upper southwest rift zone. The eruption lasted about 8.5 hours.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref><ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
A second eruption took place between September 15 and September 20, 2024 near and within Nāpau Crater, a pit crater located in a remote and uninhabited part of the volcano's middle east rift. The eruption had four eruptive phases between September 15 and September 20. The final eruptive activity from a small vent west of Nāpau Crater ended at about 10 AM HST on September 20.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
On December 23, 2024, an eruption began within HalemaTemplate:OkinaumaTemplate:Okinau.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> The eruption carried on into 2025, with episodic lava fountains reaching as high as Template:Convert as of March.<ref> https://www.bigislandvideonews.com/2025/01/01/kilauea-volcano-eruption-continues-into-2025/</ref><ref> https://bigislandnow.com/2025/03/04/enormous-lava-geysers-once-again-erupt-from-kilauea-summit-as-episode-12-begins/</ref>
HazardsEdit
In 2018, the USGS National Volcanic Threat Assessment gave Kīlauea an overall threat score of 263, and ranked it first among volcanoes in the United States most likely to threaten lives and infrastructure.<ref name="USGS">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
Volcanic Explosivity IndexEdit
The Global Volcanism Program assigned a Volcanic Explosivity Index (VEI; the higher the number, the more explosive) to 90 of Kīlauea's 96 known eruptions of the last 11,700 years. The eruption of 1790 received a VEI of 4.<ref name=VEIdata>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> The 1983–2018 eruption was marked 3.<ref name="SmithsonianGVP1983-2018">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> The eruptions of 1820, 1924, 1959 and 1960 received 2s. The eruptions of 680, 1050, 1490, 1500, 1610, 1868 and four eruptions in 1961 scored a 1. The other seventy-four stayed at 0.<ref name=VEIdata/>
Oral traditionsEdit
Native Hawaiians have passed down ancient oral traditions surrounding the volcanoes ever since they settled on the islands. These oral histories provide rich cultural and geologic knowledge. In the field of volcanology, the use of oral history emerged from obscurity to become a resource for understanding the eruption history of a given region. While oral history has been used to confirm previously known geologic data, it can be used to assess hazards surrounding an eruption, in addition to guiding the rehabilitation of affected communities.<ref>Template:Cite book</ref>
Using the oral history of the Template:OkinaAilāTemplate:Okinaau eruption, volcanologists learned that Kīlauea was much more explosive than previously thought. Given its eruption history, the tradition predicts a long period of explosive eruptions.<ref name=":3"/> Hawaiian chants provided clues that surface water had been found at the summit in earlier times. The story of Pele and Hiʻiaka recorded extensive lava flows, as well as a collapse of Kaluapele in about 1500.<ref name=":5" />
EcologyEdit
BackgroundEdit
[[File:Kalapana May 2009.jpg|thumb|right|[[Metrosideros polymorpha|Template:OkinaŌhiTemplate:Okinaa]] (Metrosideros polymorpha) growing on a barren lava field dating from 1986, formerly the village of Kalapana, Hawaii. The myrtle in this picture, taken in 2009, may have since been covered over—fresh flows in 2010 partially re-covered the area.]] Because of its position more than Template:Cvt from the nearest continental landmass, the island of HawaiTemplate:Okinai is one of the most geographically isolated landmasses; this strongly influenced its ecology. The majority of the species present on the island are endemic, the result of its isolated lineage sheltered; its ecosystem is vulnerable to invasive species and to human development–an estimated one-third of the island's natural flora and fauna is extinct.<ref>Template:Cite journal</ref>
Kīlauea's ecological community is further threatened by the volcano itself;<ref name=osu-landforms /> lava flows often overrun and incinerate forest sections, while ash smothers local plant life. Layers of carbonized organic material at the bottom of ash deposits are evidence of this destruction. Parts of the volcano's slopes display the dichotomy between pristine montane forest and volcanic "deserts" yet to be recolonized.<ref>Template:Cite journal</ref>
Kīlauea's bulk affects local climate through the influence of trade winds coming predominantly from the northeast, which, when squeezed upwards by the volcano's height, result in a moister windward side and an arid leeward flank. The volcano's ecology reflects its height, and by the distribution of volcanic products, making for varied soil conditions. The northern part of Kīlauea is mostly below Template:Convert and receives more than Template:Convert mean annual rainfall, and is mostly a lowland wet community; farther south, with precipitation less than Template:Convert mean annual rainfall, is considered mostly a lowland dry environment.<ref name=tma-management>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
EcosystemsEdit
Much of Kīlauea's southern section lies within the national park. It offers aTemplate:Okinae ferns, ʻōhiʻa trees (Metrosideros polymorpha), and hapu’u of genus Cibotium are common.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> The park hosts many bird species, including the Template:Okinaapapane (Himatione sanguinea); Template:Okinaamakihi (Hemignathus virens); iTemplate:Okinaiwi (Vestiaria coccinea); ‘ōma’o (Myadestes obscurus), ʻelepaio (Chasiempis sp.); and the endangered Template:Okinaakepa (Loxops coccineus), Template:OkinaakiapolaTemplate:Okinaau (Hemignathus munroi), nēnē (Branta sandvicensis), ʻuaʻu (Pterodroma sandwichensis), and ʻio (Buteo solitarius) species.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> The coast hosts three of the island's nine known critically endangered hawksbill sea turtle (Eretmochelys imbricata) nesting sites.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
Some of the area alongside the southwestern rift zone takes the form of the Kaʻū Desert. Although not a "true" desert (rainfall there exceeds the maximum Template:Convert a year), precipitation mixing with drifting volcanic sulfur dioxide forms acid rain with a pH as low as 3.4, greatly hampering plant growth.<ref>Template:Cite book</ref> The deposited tephra particulates make the local soil very permeable. Plant life there is practically nonexistent.<ref>Template:Cite journal</ref>
Kīlauea's northern lowland wet-forest ecosystem is partially protected by the Puna Forest Reserve and the Kahauale`a Natural Area Reserve. At Template:Convert, Wao Kele o Puna is [[Hawaii|HawaiTemplate:Okinai]]'s largest lowland wet forest reserve, and is home to rare plant species including hāpuTemplate:Okinau ferns (Cibotium spp.), Template:OkinaieTemplate:Okinaie vines (Freycinetia arborea), and kōpiko (Psychotria mariniana), some of which play a role in limiting invasive species' spread. Template:OkinaOpeTemplate:OkinaapeTemplate:Okinaa (Lasiurus cinereus semotus) Template:Okinaio (Buteo solitarius), common Template:Okinaamakihi (Hemignathus virens), and nananana makakiTemplate:Okinai (Theridion grallator) live in the trees. Many more as-yet-undocumented species are thought to lie within the forest.<ref name=nyt>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref><ref name=sg>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> Wao Kele's primary forest tree is Template:OkinaōhiTemplate:Okinaa lehua (Metrosideros polymorpha).<ref name=hsb2001>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
Human historyEdit
Ancient HawaiianEdit
The first Ancient Hawaiians to arrive on Hawaii island lived along the shores, where food and water were plentiful.<ref name=nasa-outrigger>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> Flightless birds that had previously known no predators became a staple food source.<ref name=haw-culture>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> Early settlements had a major impact on the local ecosystem, and caused many extinctions, particularly bird species, while introducing foreign plants and animals and increasing erosion rates.<ref name=ps-1982>Template:Cite journal</ref> The prevailing lowland forest ecosystem was transformed from forest to grassland; some caused by their use of fire, but the main cause appears to have been the Polynesian rat (Rattus exulans).<ref>Template:Cite journal</ref>
The summits of the island's volcanoes are revered as sacred mountains. In one Hawaiian mythology, sky father Wākea marries earth mother Papa, giving birth to the islands.<ref name=haw-culture/> Kīlauea itself means "spewing" or "much spreading" in Hawaiian,<ref name=hvo-kilauea /> and Kīlauea is the body of the deity Pele, goddess of fire, lightning, wind, and volcanoes.<ref>Template:Cite journal</ref> The conflict between Pele and the rain god [[Kamapua'a|KamapuaTemplate:Okinaa]] was centered there; HalemaTemplate:OkinaumaTemplate:Okinau, "House of the [[amaumau|Template:OkinaamaTemplate:OkinaumaTemplate:Okinau]] fern", derives its name from the struggle between the two gods. KamapuaTemplate:Okinaa, hard-pressed by Pele's ability to make lava spout from the ground at will, covered the feature, a favorite residence of the goddess, with fern fronds. Choked by trapped smoke, Pele emerged. Realizing that each could threaten the other with destruction, the other gods called a draw and divided the island between them, with KamapuaTemplate:Okinaa getting the moist windward northeastern side, and Pele directing the drier Kona (or leeward) side. The rusty singed appearance of the young fronds of the Template:OkinaamaTemplate:OkinaumaTemplate:Okinau are said to be a product of the legendary struggle.<ref>Template:Cite book</ref><ref name="haw-culture" />
Modern eraEdit
The first foreigner to arrive at Hawaii was James Cook in 1778.<ref name=uh-2009>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> The first non-native to observe Kīlauea in detail was William Ellis, an English missionary who in 1823 spent more than two weeks trekking across the volcano. He collated the first written account of the volcano and observed many of its features.<ref name=hvo-first>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> Template:Sister project Another missionary, C. S. Stewart, U.S.N., wrote of it in his journal A Residence in the Sandwich Island, which Letitia Elizabeth Landon quoted from in the notes to her poetical illustration to an engraving of a painting by William Ellis after F Howard, The Volcano of Ki-Rau-E-A in Fisher's Drawing Room Scrap Book, 1832.<ref>Template:Cite bookTemplate:Cite book</ref>
One of the earliest and most important surveyors of Kīlauea was James Dwight Dana, who studied and wrote about the island's volcanoes for decades first-hand.<ref>Template:Cite journal</ref> Dana visited Kīlauea's summit in 1840.<ref>Template:Cite journal</ref> After publishing a summary paper in 1852, he directed a detailed geological study of the island in 1880 and 1881. He did not consider Kīlauea a separate volcano, instead referring to it as a flank vent of Mauna Loa; geologist C. E. Dutton elaborated on Dana's research during an 1884 expedition. His work led Kīlauea to be accepted as a separate entity.<ref name="USGS-dw">Template:Cite book</ref>Template:Rp
Hawaiian Volcano ObservatoryEdit
The next era of Kīlauea's history began with the establishment of the Hawaiian Volcano Observatory in 1912. The first permanent such installation in the United States, the observatory was the brainchild of Thomas Jaggar, head of geology at the Massachusetts Institute of Technology. After witnessing the devastation of the 1908 Messina earthquake near Mount Etna in Italy, he declared that systematic volcanic and seismic study was required, and chose Kīlauea as the initial site.
After securing funding from MIT and the University of Hawaiʻi, Jaggar served as director of the observatory between 1912 and 1940. He pioneered seismological and observational study and observation of the volcano.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> After initial funding ran out, the Observatory was funded by the National Weather Service, USGS, and the National Park Service in turn. USGS reclaimed the observatory and funded it after 1946. The main building was moved twice since establishment, and the facility on the northwest rim of Kaluapele served until 2018 when it was damaged beyond repair by volcanic activity, and the buildings were torn down in 2024.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref><ref> https://www.nps.gov/havo/learn/management/jaggar-museum.htm </ref>
NASA used the area to train Apollo Astronauts in recognizing volcanic features, planning traverses, collecting samples and taking photographs. Training took place in April 1969, April 1970, December 1970, December 1971, and June 1972. Astronauts of Apollo 12, Apollo 14, Apollo 15, Apollo 16 and Apollo 17 used this training on the Moon. Notable geologist instructors included William R. Muehlberger.<ref>Template:Cite book</ref>
ResearchEdit
In October 2019, January 2020, and December 2020, USGFS volcanologists used a drone to study gases inside the water lake at the summit, as it was too dangerous for humans to approach. After the lake boiled away, they used the drone to study the resulting gas plumes.<ref>Template:Cite journal</ref>
In 2022, researchers reported that Kīlauea's seismic waves could be used to predict future outbreaks. These waves can last for tens of seconds. After the 2007 eruption ended, they analyzed thousands of events from seismic sensors, GPS stations, and lake height observations, including variables such as temperature and gas bubble density. They reported that magma temperature was associated with seismic signal duration and bubble quantity and composition.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
TourismEdit
Kīlauea became a tourist attraction in the 1840s, and businessmen such as Benjamin Pitman and George Lycurgus operated a series of hotels at the rim, including Volcano House, which is the only hotel or restaurant located within Hawaiʻi Volcanoes National Park.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
In 1891, Lorrin A. Thurston, investor in hotels along the volcano's rim, began campaigning for a park, boosting an idea proposed by William Richards Castle, Jr. in 1903. Thurston, who owned the Honolulu Advertiser newspaper, printed editorials in favor of the idea; by 1911 Governor Walter F. Frear had proposed a draft bill to create "Kilauea National Park". Following endorsements from John Muir, Henry Cabot Lodge, and former President Theodore Roosevelt (in opposition to local ranchers) and several legislative attempts introduced by delegate Jonah Kūhiō Kalanianaʻole, House Resolution 9525 was signed into law by Woodrow Wilson on August 1, 1916. It was the country's 11th National Park, and the first in a Territory.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
Originally called "Hawaii National Park", it was split from Haleakala National Park on September 22, 1960. Today, the park, renamed the Hawaiʻi Volcanoes National Park, is a major conservatory agency and tourist attraction, and, since 1987, a World Heritage Site.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
Hawaii tourism grew slowly before exploding with the advent of jet airliner travel around 1959. Kīlauea, as one of the few chronically erupting volcanoes, was a major part of the island's tourist draw.<ref name=nps-park>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> According to the National Park Service, Kīlauea is visited by roughly 2.6 million people annually.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
The Thomas A. Jaggar Museum was a popular tourist stop. Located at the edge of Kaluapele, the museum's observation deck offered the best sheltered view on the volcano of the activity at HalemaTemplate:OkinaumaTemplate:Okinau; however, the museum was closed permanently after the building sustained structural damage from earthquakes associated with the 2018 eruptions.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
Volcano House provides lodging within the park, while additional housing options are available in the Volcano Village.
Visitors associated with the military can find lodging at the Kilauea Military Camp. The park provides hiking trails, points of interest, and guided ranger programs.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref><ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> The Crater Rim Trail around the volcano is designated as a National Recreation Trail.<ref name="nrt">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
ReferencesEdit
Further readingEdit
External linksEdit
- Template:Britannica
- Template:Cite gvp
- Hawaiian Volcano Observatory's Kīlauea website
- Live webcams of Kīlauea and Mauna Loa
- USGS updates on Kilauea's Lava (and water) lakes, May 11, 2022
- HawaiTemplate:Okinai Volcanoes National Park website
- Hawaii Groundwater & Geothermal Resources Center by the University of Hawaiʻi at Mānoa
- The Geothermal Collection by University of Hawaiʻi at Mānoa
- Video footage of the March 2011 Kamoamoa Fissure Eruption and the collapse of Puʻu ʻŌʻō crater
Template:Hawaiian volcanism Template:NRHP in Hawaii Volcanoes NP Template:Portal bar