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The Global Volcanism Program has no activity reports for Taranaki [Egmont].
The Global Volcanism Program has no Weekly Reports available for Taranaki [Egmont].
The Global Volcanism Program has no Bulletin Reports available for Taranaki [Egmont].
This compilation of synonyms and subsidiary features may not be comprehensive. Features are organized into four major categories: Cones, Craters, Domes, and Thermal Features. Synonyms of features appear indented below the primary name. In some cases additional feature type, elevation, or location details are provided.
|Feature Name||Feature Type||Elevation||Latitude||Longitude|
|Fanthams Peak||Cone||1962 m||39° 19' 0" S||174° 3' 58" E|
|Feature Name||Feature Type||Elevation||Latitude||Longitude|
|Beehives, the||Dome||952 m||39° 20' 13" S||174° 3' 29" E|
|Dome, the||Dome||1048 m||39° 16' 0" S||174° 2' 0" E|
|Skinner Hill||Dome||1311 m||39° 17' 0" S||174° 3' 0" E|
Summary of Holocene eruption dates and Volcanic Explosivity Indices (VEI).
|Start Date||Stop Date||Eruption Certainty||VEI||Evidence||Activity Area or Unit|
|1755 (?)||Unknown||Confirmed||Dendrochronology||Tahurangi Ash|
|1700 ± 50 years||Unknown||Confirmed||Radiocarbon (uncorrected)|
|1655 (?)||Unknown||Confirmed||4||Dendrochronology||Burrell Lapilli|
|1590 ± 40 years||Unknown||Confirmed||Radiocarbon (uncorrected)|
|1570 ± 40 years||Unknown||Confirmed||Radiocarbon (uncorrected)|
|1560 ± 40 years||Unknown||Confirmed||Radiocarbon (uncorrected)|
|1550 ± 40 years||Unknown||Confirmed||Radiocarbon (uncorrected)|
|1500 ± 30 years||Unknown||Confirmed||Radiocarbon (uncorrected)||Newall Ash|
|1480 ± 50 years||Unknown||Confirmed||Radiocarbon (uncorrected)|
|1400 ± 50 years||Unknown||Confirmed||Radiocarbon (uncorrected)|
|1340 ± 40 years||Unknown||Confirmed||Radiocarbon (uncorrected)|
|1300 ± 50 years||Unknown||Confirmed||Radiocarbon (uncorrected)|
|1070 ± 40 years||Unknown||Confirmed||Radiocarbon (uncorrected)|
|0970 ± 30 years||Unknown||Confirmed||Radiocarbon (uncorrected)|
|0820 ± 30 years||Unknown||Confirmed||Radiocarbon (uncorrected)|
|0550 (?)||Unknown||Confirmed||Tephrochronology||Kaupokonui tephra|
|0520 ± 150 years||Unknown||Confirmed||Radiocarbon (uncorrected)|
|0390 ± 40 years||Unknown||Confirmed||Radiocarbon (uncorrected)|
|0100 ± 40 years||Unknown||Confirmed||Radiocarbon (uncorrected)|
|0040 BCE ± 75 years||Unknown||Confirmed||Radiocarbon (uncorrected)||Maketawa Tephra|
|0150 BCE ± 30 years||Unknown||Confirmed||Radiocarbon (uncorrected)|
|0420 BCE ± 30 years||Unknown||Confirmed||Radiocarbon (uncorrected)|
|0590 BCE ± 500 years||Unknown||Confirmed||Tephrochronology|
|1130 BCE ± 200 years||Unknown||Confirmed||Tephrochronology||Fanthams Peak, Manganui Tephra|
|1190 BCE ± 40 years||Unknown||Confirmed||Radiocarbon (uncorrected)|
|1250 BCE (?)||Unknown||Confirmed||Tephrochronology||Southern Beehive|
|1560 BCE ± 40 years||Unknown||Confirmed||Radiocarbon (uncorrected)|
|1700 BCE ± 100 years||Unknown||Confirmed||5||Radiocarbon (uncorrected)||Inglewood Tephra|
|2150 BCE (?)||Unknown||Confirmed||Tephrochronology||Korito Tephra|
|2400 BCE ± 40 years||Unknown||Confirmed||Radiocarbon (uncorrected)|
|2450 BCE ± 300 years||Unknown||Confirmed||Tephrochronology||Mangatoki Tephra|
|2700 BCE (?)||Unknown||Confirmed||Tephrochronology||Tariki tephra|
|2850 BCE ± 300 years||Unknown||Confirmed||Tephrochronology|
|3250 BCE (?)||Unknown||Confirmed||Tephrochronology||Waipuku tephra|
|5120 BCE ± 50 years||Unknown||Confirmed||Radiocarbon (uncorrected)|
|6050 BCE (?)||Unknown||Confirmed||Tephrochronology|
|7000 BCE ± 100 years||Unknown||Confirmed||Radiocarbon (uncorrected)||Kaponga-f tephra|
|7270 BCE ± 50 years||Unknown||Confirmed||Radiocarbon (uncorrected)|
|7330 BCE (?)||Unknown||Confirmed||Tephrochronology||Kaponga-e tephra|
|7650 BCE (?)||Unknown||Confirmed||Radiocarbon (uncorrected)||Kaponga-b tephra|
Information about Deformation periods will be available soon.
There is no Emissions History data is available for Taranaki [Egmont].
|Symmetrical Taranaki (Egmont) volcano dominates the western coast of New Zealand's North Island. The 2518-m stratovolcano, seen here from the south, is surrounded by a ring plain of debris avalanche and lahar deposits produced by repetitive collapse of the volcanic edifice. Taranaki (Egmont) has been active throughout the Holocene. The latest eruption of Taranaki took place in 1854 CE.
Photo by Jim Cole (University of Canterbury).
|Tarankai (Egmont) volcano has a breached summit crater that is occupied by a partially destroyed lava plug. This view from the SE shows the stacked lava flows that form much of the cone, with the vegetated slopes of the parasitic volcano, Fanthams Peak, at the left. Both Taranaki, the Maori name, and Egmont, the name assigned by Captain Cook, are used for the volcano.
Photo by Chris Newhall, 1986(U.S. Geological Survey).
|Grass-covered conical hills dot the plains around Mount Taranaki (Egmont), on New Zealand's North Island. Small hills such as these, often located in lowland areas well beyond the flanks of a volcano, were once thought to be cinder cones or small secondary vents produced by explosions when a lava flow passed over a body of water. They now are known to be hummocks of massive debris avalanches produced by volcanic landslides. Debris-avalanche deposits originating from repetitive collapse surround the volcano to distances of about 40 km.
Photo by Don Swanson, 1984 (U.S. Geological Survey).
|The pasture-covered, hilly terrain in the foreground is part of a vast ring plain of debris-avalanche and lahar deposits that surrounds Mount Taranaki (Egmont). Repetitive collapse of the volcano during the late Pleistocene and Holocene produced debris avalanches that reached the western coast, nearly 40 km from the volcano.
Photo by Dan Miller (U.S. Geological Survey).
|An aerial view from the south shows Mount Taranaki (Egmont), with its parasitic volcano of Fanthams Peak at the lower right. The summit of Taranaki contains a partially destroyed lava dome; four other lava domes are located low on the south and north flanks. Taranaki volcano collapsed and rebuilt itself repetitively during the late Pleistocene and Holocene.
Photo by Jim Cole, 1971 (University of Canterbury).
|Taranaki volcano, seen here from the SW, rises to 2518 m above the Taranaki ring plain, with its parasitic volcano Fanthams Peak on the left. Taranaki (Egmont) is the youngest and SE-most of a group of volcanoes beginning with the Kaitoke Range, near the west coast of North Island. Tarananki has been active during the past 125,000 years. Its most recent activity, during the 15th to 19th centuries, included the eruption of airfall tephra, pyroclastic flows that traveled to the NW, and emplacement of the summit lava dome.
Photo by Chris Newhall, 1986 (U.S. Geological Survey).
|Mount Taranaki volcano is the centerpiece of Egmont National Park on the western side of the North Island of New Zealand. Farmlands surrounding the volcano extend to the boundaries of the national park, leaving a circular pattern prominent from space. The Pleistocene Kaitoke Range forms the topographic high WNW of Taranaki.
Photo courtesy of NASA (www.earthobservatory.nasa.gov).
There are no samples for Taranaki [Egmont] in the Smithsonian's NMNH Department of Mineral Sciences Rock and Ore collection.
Single Volcano View
Temporal Evolution of Unrest
Side by Side Volcanoes
|WOVOdat is a database of volcanic unrest; instrumentally and visually recorded changes in seismicity, ground deformation, gas emission, and other parameters from their normal baselines. It is sponsored by the World Organization of Volcano Observatories (WOVO) and presently hosted at the Earth Observatory of Singapore.|
|Large Eruptions of Taranaki [Egmont]||Information about large Quaternary eruptions (VEI >= 4) is cataloged in the Large Magnitude Explosive Volcanic Eruptions (LaMEVE) database of the Volcano Global Risk Identification and Analysis Project (VOGRIPA).|
|MIROVA||Middle InfraRed Observation of Volcanic Activity (MIROVA) is a near real time volcanic hot-spot detection system based on the analysis of MODIS (Moderate Resolution Imaging Spectroradiometer) data. In particular, MIROVA uses the Middle InfraRed Radiation (MIR), measured over target volcanoes, in order to detect, locate and measure the heat radiation sourced from volcanic activity.|
|MODVOLC Thermal Alerts||Using infrared satellite Moderate Resolution Imaging Spectroradiometer (MODIS) data, scientists at the Hawai'i Institute of Geophysics and Planetology, University of Hawai'i, developed an automated system called MODVOLC to map thermal hot-spots in near real time. For each MODIS image, the algorithm automatically scans each 1 km pixel within it to check for high-temperature hot-spots. When one is found the date, time, location, and intensity are recorded. MODIS looks at every square km of the Earth every 48 hours, once during the day and once during the night, and the presence of two MODIS sensors in space allows at least four hot-spot observations every two days. Each day updated global maps are compiled to display the locations of all hot spots detected in the previous 24 hours. There is a drop-down list with volcano names which allow users to 'zoom-in' and examine the distribution of hot-spots at a variety of spatial scales.|
|EarthChem||EarthChem develops and maintains databases, software, and services that support the preservation, discovery, access and analysis of geochemical data, and facilitate their integration with the broad array of other available earth science parameters. EarthChem is operated by a joint team of disciplinary scientists, data scientists, data managers and information technology developers who are part of the NSF-funded data facility Integrated Earth Data Applications (IEDA). IEDA is a collaborative effort of EarthChem and the Marine Geoscience Data System (MGDS).|