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Coordinates: 3°19′N 76°11′W / 3.32°N 76.18°W / 3.32; -76.18[1]
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{{Short description|Patera on Io}}
[[Image:Tawhaki Patera.jpg|thumb|300px|right|Highest resolution images of Tawhaki Patera, taken by the ''Galileo'' spacecraft. Color image on the left acquired in July 1999. The gray scale image on the right taken in November 1999.]]
[[Image:Tawhaki Patera.jpg|thumb|300px|right|Highest resolution images of Tawhaki Patera, taken by the ''Galileo'' spacecraft. Color image on the left acquired in July 1999. The gray scale image on the right taken in November 1999.]]
'''Tawhaki Patera''' is an active [[volcano]] on [[Jupiter|Jupiter's]] [[Natural satellite|moon]] [[Io (moon)|Io]]. It is located on Io's leading hemisphere at {{coord|3.32|N|76.18|W|globe:io_type:landmark_source:gpn|display=inline,title|notes=<ref name="Planetarynomenclature">{{gpn|66055|Tawhaki Patera}}</ref>}} within the [[List of regions on Io|equatorial plains]] of western [[Media Regio]]. Tawhaki is an [[Volcanism on Io#Intra-patera eruptions|Ionian patera]], a type of volcanic crater similar to a [[caldera]], {{convert|49.8|km|mi|sp=us}} wide and {{convert|550|m|ft|sp=us}} deep.<ref name="Planetarynomenclature"/><ref name="Bunte2009">{{cite journal |title=Geologic mapping of the Hi'iaka and Shamshu regions of Io |journal=[[Icarus (journal)|Icarus]] |last=Bunte |first=M. |display-authors=etal |pages= 868–886|volume= 207|issue= 2|date=2009 |doi=10.1016/j.icarus.2009.12.006 |bibcode=2010Icar..207..868B}}</ref>
'''Tawhaki Patera''' is an active [[volcano]] on [[Jupiter|Jupiter's]] [[Natural satellite|moon]] [[Io (moon)|Io]]. It is located on Io's leading hemisphere at {{coord|3.32|N|76.18|W|globe:io_type:landmark_source:gpn|display=inline,title|notes=<ref name="Planetarynomenclature">{{gpn|66055|Tawhaki Patera}}</ref>}} within the [[List of regions on Io|equatorial plains]] of western [[Media Regio]]. Tawhaki is an [[Volcanism on Io#Intra-patera eruptions|Ionian patera]], a type of volcanic crater similar to a [[caldera]], {{convert|49.8|km|mi|sp=us}} wide and {{convert|550|m|ft|sp=us}} deep.<ref name="Planetarynomenclature"/><ref name="Bunte2009">{{cite journal |title=Geologic mapping of the Hi'iaka and Shamshu regions of Io |journal=[[Icarus (journal)|Icarus]] |last=Bunte |first=M. |display-authors=etal |pages= 868–886|volume= 207|issue= 2|date=2009 |doi=10.1016/j.icarus.2009.12.006 |bibcode=2010Icar..207..868B}}</ref>
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Tawhaki Patera was first seen as a dark spot in low-resolution ''[[Voyager 1]]'' in March 1979. However, volcanic activity was not observed at Tawhaki until September 1997 when a bright thermal hotspot was observed at near-infrared wavelengths while Io was in the shadow of Jupiter by the camera on the ''[[Galileo (spacecraft)|Galileo]]'' spacecraft.<ref name="McEwen1998">{{cite journal | last=McEwen |first=A. S. |display-authors=etal |title=Active Volcanism on Io as Seen by Galileo SSI |journal=Icarus |volume=135 |pages=181–219 |date=1998 |issue=1 |doi=10.1006/icar.1998.5972 |bibcode=1998Icar..135..181M|doi-access=free }}</ref> Tawhaki would also be observed as a hotspot while Io was in eclipse in November 1997 during ''Galileo's'' eleventh orbit. The high temperature period of the eruption at Tawhaki ceased by May 1998.<ref name="Keszthelyi2001">{{cite journal |title=Imaging of volcanic activity on Jupiter's moon Io by Galileo during the Galileo Europa Mission and the Galileo Millennium Mission |journal=[[Journal of Geophysical Research]] |last=Keszthelyi |first=L. |display-authors=etal |pages=33025–33052 |volume=106 |date=2001 |issue=E12 |doi=10.1029/2000JE001383 |bibcode=2001JGR...10633025K|doi-access=free }}</ref> It is uncertain whether this delay is due to real changes in activity at Tawhaki or the poor resolution of the ''Voyager'' data and ''Galileo'' data from the [[Galileo (spacecraft)#Near-Infrared Mapping Spectrometer (NIMS)|Near-Infrared Mapping Spectrometer (NIMS)]].<ref name="McEwen1998"/>
Tawhaki Patera was first seen as a dark spot in low-resolution ''[[Voyager 1]]'' in March 1979. However, volcanic activity was not observed at Tawhaki until September 1997 when a bright thermal hotspot was observed at near-infrared wavelengths while Io was in the shadow of Jupiter by the camera on the ''[[Galileo (spacecraft)|Galileo]]'' spacecraft.<ref name="McEwen1998">{{cite journal | last=McEwen |first=A. S. |display-authors=etal |title=Active Volcanism on Io as Seen by Galileo SSI |journal=Icarus |volume=135 |pages=181–219 |date=1998 |issue=1 |doi=10.1006/icar.1998.5972 |bibcode=1998Icar..135..181M|doi-access=free }}</ref> Tawhaki would also be observed as a hotspot while Io was in eclipse in November 1997 during ''Galileo's'' eleventh orbit. The high temperature period of the eruption at Tawhaki ceased by May 1998.<ref name="Keszthelyi2001">{{cite journal |title=Imaging of volcanic activity on Jupiter's moon Io by Galileo during the Galileo Europa Mission and the Galileo Millennium Mission |journal=[[Journal of Geophysical Research]] |last=Keszthelyi |first=L. |display-authors=etal |pages=33025–33052 |volume=106 |date=2001 |issue=E12 |doi=10.1029/2000JE001383 |bibcode=2001JGR...10633025K|doi-access=free }}</ref> It is uncertain whether this delay is due to real changes in activity at Tawhaki or the poor resolution of the ''Voyager'' data and ''Galileo'' data from the [[Galileo (spacecraft)#Near-Infrared Mapping Spectrometer (NIMS)|Near-Infrared Mapping Spectrometer (NIMS)]].<ref name="McEwen1998"/>


Tawhaki Patera is one of several volcanoes suspected of being responsible for the August 2, 1999 9908A [[Volcanism on Io#Explosion-dominated eruptions (Pillanian Volcanism)|outburst eruption]], one of the most energetic observed on Io.<ref name="Lopes2001">{{cite journal |title=Io in the near infrared: Near-Infrared Mapping Spectrometer (NIMS) results from the Galileo flybys in 1999 and 2000 |journal=J. Geophys. Res. |last=Lopes |first=R. M. C. |display-authors=etal |pages=33053–33078 |volume=106 |issue=E12 |date=2001 |doi=10.1029/2000JE001463 |bibcode=2001JGR...10633053L}}</ref> However, the low-resolution of the ground-based observation precludes a definitive identification of the source volcano of the eruption beyond that it was located in northwestern Media Regio on Io's leading hemisphere.<ref name="Howell2001">{{cite journal |title=Ground-based observations of volcanism on Io in 1999 and early 2000 |journal=J. Geophys. Res. |last=Howell |first=R. R. |display-authors=etal |pages=33129–33139 |volume=106 |issue=E12 |date=2001 |doi=10.1029/2000JE001382 |bibcode=2001JGR...10633129H|doi-access=free }}</ref> The NIMS instrument did detect a thermal hotspot between one and five micrometres at Tawhaki during ''Galileo's'' 21st orbit in July 1999, a month prior to the eruption.<ref name="Lopes2001"/> The southern half of Tawhaki Patera was observed by Galileo at 260 meters per pixel during an encounter with Io on November 26, 1999, providing the highest resolution image of this volcano.<ref name="Keszthelyi2001"/> This along with a color observation taken in July 1999, showed that the floor of Tawhaki contained some of the darkest material in the area, suggesting the cooled lava at Tawhaki is very young, consistent with the activity seen during the Galileo mission.<ref name="Bunte2009"/> A lava channel, later named [[Tawhaki Vallis]] was also found to the southeast. The channel maybe related to earlier activity at Tawhaki Patera, but the images of the region cut off the northern half of the volcano and channel, preventing a relationship between the two volcanic features to be established.<ref name="Schenk2004">{{cite journal |title=A potential thermal erosion channel on Io |journal=[[Geophysical Research Letters]] |last=Schenk |first=P. M. |author2=D. A. Williams |pages=L23702 |volume=31 |issue= 23|date=2004 |doi=10.1029/2004GL021378 |bibcode=2004GeoRL..3123702S|doi-access=free }}</ref> In August 2001, NIMS once again observed a low level of activity at Tawhaki Patera.<ref name="Lopes2004">{{cite journal |title=Lava lakes on Io: Observations of Io's volcanic activity from Galileo NIMS during the 2001 fly-bys |journal=Icarus |last=Lopes |first=R. M. C. |display-authors=etal |pages=140–74 |volume=169 |date=2004 |issue=1 |doi=10.1016/j.icarus.2003.11.013 |bibcode=2004Icar..169..140L}}</ref>
Tawhaki Patera is one of several volcanoes suspected of being responsible for the August 2, 1999 9908A [[Volcanism on Io#Explosion-dominated eruptions (Pillanian Volcanism)|outburst eruption]], one of the most energetic observed on Io.<ref name="Lopes2001">{{cite journal |title=Io in the near infrared: Near-Infrared Mapping Spectrometer (NIMS) results from the Galileo flybys in 1999 and 2000 |journal=J. Geophys. Res. |last1=Lopes |first1=R. M. C. |author1-link=Rosaly Lopes |display-authors=etal |pages=33053–33078 |volume=106 |issue=E12 |date=2001 |doi=10.1029/2000JE001463 |bibcode=2001JGR...10633053L}}</ref> However, the low-resolution of the ground-based observation precludes a definitive identification of the source volcano of the eruption beyond that it was located in northwestern Media Regio on Io's leading hemisphere.<ref name="Howell2001">{{cite journal |title=Ground-based observations of volcanism on Io in 1999 and early 2000 |journal=J. Geophys. Res. |last=Howell |first=R. R. |display-authors=etal |pages=33129–33139 |volume=106 |issue=E12 |date=2001 |doi=10.1029/2000JE001382 |bibcode=2001JGR...10633129H|doi-access=free }}</ref> The NIMS instrument did detect a thermal hotspot between one and five micrometres at Tawhaki during ''Galileo's'' 21st orbit in July 1999, a month prior to the eruption.<ref name="Lopes2001"/> The southern half of Tawhaki Patera was observed by Galileo at 260 meters per pixel during an encounter with Io on November 26, 1999, providing the highest resolution image of this volcano.<ref name="Keszthelyi2001"/> This along with a color observation taken in July 1999, showed that the floor of Tawhaki contained some of the darkest material in the area, suggesting the cooled lava at Tawhaki is very young, consistent with the activity seen during the Galileo mission.<ref name="Bunte2009"/> A lava channel, later named [[Tawhaki Vallis]] was also found to the southeast. The channel maybe related to earlier activity at Tawhaki Patera, but the images of the region cut off the northern half of the volcano and channel, preventing a relationship between the two volcanic features to be established.<ref name="Schenk2004">{{cite journal |title=A potential thermal erosion channel on Io |journal=[[Geophysical Research Letters]] |last=Schenk |first=P. M. |author2=D. A. Williams |pages=L23702 |volume=31 |issue= 23|date=2004 |doi=10.1029/2004GL021378 |bibcode=2004GeoRL..3123702S|doi-access=free }}</ref> In August 2001, NIMS once again observed a low level of activity at Tawhaki Patera.<ref name="Lopes2004">{{cite journal |title=Lava lakes on Io: Observations of Io's volcanic activity from Galileo NIMS during the 2001 fly-bys |journal=Icarus |last=Lopes |first=R. M. C. |display-authors=etal |pages=140–74 |volume=169 |date=2004 |issue=1 |doi=10.1016/j.icarus.2003.11.013 |bibcode=2004Icar..169..140L}}</ref>


The volcano [[Planetary nomenclature|was formally named]] Tawhaki Patera by the [[International Astronomical Union]] in 2000 after the [[Māori mythology|Māori]] lightning god, [[Tāwhaki]].<ref name="Planetarynomenclature"/> The Galileo imaging team suggested the name [[Hine-i-Tapeka|Hine-i-tapeka]] Patera, but Tawhaki Patera was chosen instead.<ref name="IoNameBank">{{cite web | last=Phillips | first=Cynthia|author-link=Cynthia B. Phillips | date=July 1, 1999 |url=http://pirlwww.lpl.arizona.edu/~phillips/io_features.html | title=Io Name Bank | publisher=Planetary Image Research Laboratory | accessdate=2010-02-06 }}</ref>
The volcano [[Planetary nomenclature|was formally named]] Tawhaki Patera by the [[International Astronomical Union]] in 2000 after the [[Māori mythology|Māori]] lightning god, [[Tāwhaki]].<ref name="Planetarynomenclature"/> The Galileo imaging team suggested the name [[Hine-i-Tapeka|Hine-i-tapeka]] Patera, but Tawhaki Patera was chosen instead.<ref name="IoNameBank">{{cite web | last=Phillips | first=Cynthia|author-link=Cynthia B. Phillips | date=July 1, 1999 |url=http://pirlwww.lpl.arizona.edu/~phillips/io_features.html | title=Io Name Bank | publisher=Planetary Image Research Laboratory | accessdate=2010-02-06 }}</ref>

Latest revision as of 15:29, 31 August 2024

Highest resolution images of Tawhaki Patera, taken by the Galileo spacecraft. Color image on the left acquired in July 1999. The gray scale image on the right taken in November 1999.

Tawhaki Patera is an active volcano on Jupiter's moon Io. It is located on Io's leading hemisphere at 3°19′N 76°11′W / 3.32°N 76.18°W / 3.32; -76.18[1] within the equatorial plains of western Media Regio. Tawhaki is an Ionian patera, a type of volcanic crater similar to a caldera, 49.8 kilometers (30.9 mi) wide and 550 meters (1,800 ft) deep.[1][2]

Tawhaki Patera was first seen as a dark spot in low-resolution Voyager 1 in March 1979. However, volcanic activity was not observed at Tawhaki until September 1997 when a bright thermal hotspot was observed at near-infrared wavelengths while Io was in the shadow of Jupiter by the camera on the Galileo spacecraft.[3] Tawhaki would also be observed as a hotspot while Io was in eclipse in November 1997 during Galileo's eleventh orbit. The high temperature period of the eruption at Tawhaki ceased by May 1998.[4] It is uncertain whether this delay is due to real changes in activity at Tawhaki or the poor resolution of the Voyager data and Galileo data from the Near-Infrared Mapping Spectrometer (NIMS).[3]

Tawhaki Patera is one of several volcanoes suspected of being responsible for the August 2, 1999 9908A outburst eruption, one of the most energetic observed on Io.[5] However, the low-resolution of the ground-based observation precludes a definitive identification of the source volcano of the eruption beyond that it was located in northwestern Media Regio on Io's leading hemisphere.[6] The NIMS instrument did detect a thermal hotspot between one and five micrometres at Tawhaki during Galileo's 21st orbit in July 1999, a month prior to the eruption.[5] The southern half of Tawhaki Patera was observed by Galileo at 260 meters per pixel during an encounter with Io on November 26, 1999, providing the highest resolution image of this volcano.[4] This along with a color observation taken in July 1999, showed that the floor of Tawhaki contained some of the darkest material in the area, suggesting the cooled lava at Tawhaki is very young, consistent with the activity seen during the Galileo mission.[2] A lava channel, later named Tawhaki Vallis was also found to the southeast. The channel maybe related to earlier activity at Tawhaki Patera, but the images of the region cut off the northern half of the volcano and channel, preventing a relationship between the two volcanic features to be established.[7] In August 2001, NIMS once again observed a low level of activity at Tawhaki Patera.[8]

The volcano was formally named Tawhaki Patera by the International Astronomical Union in 2000 after the Māori lightning god, Tāwhaki.[1] The Galileo imaging team suggested the name Hine-i-tapeka Patera, but Tawhaki Patera was chosen instead.[9]

References

[edit]
  1. ^ a b c "Tawhaki Patera". Gazetteer of Planetary Nomenclature. USGS Astrogeology Research Program.
  2. ^ a b Bunte, M.; et al. (2009). "Geologic mapping of the Hi'iaka and Shamshu regions of Io". Icarus. 207 (2): 868–886. Bibcode:2010Icar..207..868B. doi:10.1016/j.icarus.2009.12.006.
  3. ^ a b McEwen, A. S.; et al. (1998). "Active Volcanism on Io as Seen by Galileo SSI". Icarus. 135 (1): 181–219. Bibcode:1998Icar..135..181M. doi:10.1006/icar.1998.5972.
  4. ^ a b Keszthelyi, L.; et al. (2001). "Imaging of volcanic activity on Jupiter's moon Io by Galileo during the Galileo Europa Mission and the Galileo Millennium Mission". Journal of Geophysical Research. 106 (E12): 33025–33052. Bibcode:2001JGR...10633025K. doi:10.1029/2000JE001383.
  5. ^ a b Lopes, R. M. C.; et al. (2001). "Io in the near infrared: Near-Infrared Mapping Spectrometer (NIMS) results from the Galileo flybys in 1999 and 2000". J. Geophys. Res. 106 (E12): 33053–33078. Bibcode:2001JGR...10633053L. doi:10.1029/2000JE001463.
  6. ^ Howell, R. R.; et al. (2001). "Ground-based observations of volcanism on Io in 1999 and early 2000". J. Geophys. Res. 106 (E12): 33129–33139. Bibcode:2001JGR...10633129H. doi:10.1029/2000JE001382.
  7. ^ Schenk, P. M.; D. A. Williams (2004). "A potential thermal erosion channel on Io". Geophysical Research Letters. 31 (23): L23702. Bibcode:2004GeoRL..3123702S. doi:10.1029/2004GL021378.
  8. ^ Lopes, R. M. C.; et al. (2004). "Lava lakes on Io: Observations of Io's volcanic activity from Galileo NIMS during the 2001 fly-bys". Icarus. 169 (1): 140–74. Bibcode:2004Icar..169..140L. doi:10.1016/j.icarus.2003.11.013.
  9. ^ Phillips, Cynthia (July 1, 1999). "Io Name Bank". Planetary Image Research Laboratory. Retrieved 2010-02-06.
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