جبل پيناتوبو

جبل پيناتوبو
Mount Pinatubo
Pinatubo91eruption clark air base.jpg
The eruption column of Mount Pinatubo on June 12, 1991, three days before the climactic eruption.
أعلى نقطة
الارتفاع1,486 m (4,875 ft) (current)
1,745 م (قبل ثوران 1991)
الإدراجبركان نشط
التسمية
لغة الاسمFilipino
النطق /ˌpnəˈtb/
الجغرافيا
جبل پيناتوبو Mount Pinatubo is located in الفلپين
جبل پيناتوبو Mount Pinatubo
جبل پيناتوبو
Mount Pinatubo
الموقع في الفلپين
الموقعلوزون
البلدالفلپين
المنطقةلوزون الوسطى
المقاطعات
السلسلة الأمجبال زامبالس
الجيولوجيا
عمر الصخرBetween 635,000 ± 80,000
and 1.1 ± 0.09 million years[2]
نوع الجبلبركان طبقي[1]
آخر ثورانJune 15, 1991[3]

جبل پيناتوبو (فيليپينو: Bundok Pinatubo/Bulkang Pinatubo؛ إنگليزية: Mount Pinatubo) هو بركان طبقي نشيط في جبال كابوسيلان في جزيرة لوزون، بالقرب من النقطة الثلاثية لـمقاطعات الفلپين زامبالس، تارلاك و پامپانگا.[4][5] تاريخ ثوراته لم يكن معروفاً للغالبية قبل الأنشطة البركانية في 1991. Pinatubo was heavily eroded, inconspicuous, and obscured from view. وكان مغطى بغابة كثيفة which supported a population of several thousand indigenous Aetas people.

The volcano's Plinian / Ultra-Plinian eruption on June 15, 1991 produced the second largest terrestrial eruption of the 20th century after the 1912 eruption of Novarupta in the Alaska Peninsula.[6] Complicating the eruption was the arrival of Typhoon Yunya (Diding), bringing a lethal mix of ash and rain to areas surrounding the volcano. Predictions at the onset of the climactic eruption led to the evacuation of tens of thousands of people from the surrounding areas, saving many lives. Surrounding areas were severely damaged by pyroclastic flows, ash deposits, and, subsequently, by the lahars caused by rainwaters re-mobilizing earlier volcanic deposits. This caused extensive destruction to infrastructure and changed river systems for years after the eruption.[6][7]

The effects of the eruption were felt worldwide. It ejected roughly 10,000,000,000 tonnes (1.1×1010 short tons) or 10 km3 (2.4 cu mi) of magma, and 20,000,000 tonnes (22,000,000 short tons) SO 2, bringing vast quantities of minerals and metals to the surface environment. It injected more particulate into the stratosphere than any eruption since Krakatoa in 1883. Over the following months, the aerosols formed a global layer of sulfuric acid haze. Global temperatures dropped by about 0.5 °C (0.9 °F) in the years 1991-93,[8] and ozone depletion temporarily increased substantially.[9]

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استعراض المنطقة

موقع جبل بيناتوبو وتساقط الركام في الإقليم من ثوران 1991.


البركان يقع على بعد 87 كم شمال غرب مانيلا، عاصمة الفلبين. Near Mount Pinatubo, the United States maintained two large military bases in the region. The U.S. Naval Base Subic Bay was 37 km (23 mi) south of Pinatubo, and the extent of Clark Air Base was just 14 km (8.7 mi) east of the volcano's summit.[10] The volcano's location on Luzon is in proximity to about 6 million people.[11]



التاريخ

ثوران 1991

ثوران جبل بيناتوبو 1991
VulcanoPinatuboJune1991.gif
The eruption cloud shortly before the climactic eruption.
التاريخJune 15, 1991
النوعUltra-Plinian
الموقعمنطقة لوزون الوسطى، لوزون، الفلپين
م.ت.ب6
التأثير
  • About 20,000 people evacuated[12]
  • Approximately 800 people were killed and 10,000 people left homeless
  • Huge destruction left in surrounding areas
  • Release of 17 megatons of sulfur dioxide into the atmosphere, causing global cooling by 0.5 °C (0.9 °F) between 1991-1993[13]
On June 15, 1991, the eruption plume minutes after the climactic eruption.


Vast quantities of minerals and metals were brought to the surface. Overall, introduced to the surface environment, was an estimated 800,000 t (880,000 short tons) of zinc, 600,000 t (660,000 short tons) of copper, 550,000 t (610,000 short tons) of chromium, 300,000 t (330,000 short tons) of nickel, and massive amounts of toxic heavy metals such as 100,000 t (110,000 short tons) of lead, 10,000 t (11,000 short tons) of arsenic, 1,000 t (1,100 short tons) of cadmium, and 800 t (880 short tons) of mercury.[14]


شاحنة تفر من ثوران بيناتوبو، الفلبين، 1991.


أعقاب ثوران 1991

The summit caldera as seen on Aug. 1, 1991.

انظر أيضاً

الهامش

  1. ^ Pinatubo, Global Volcanism Program.
  2. ^ "Pinatubo Volcano". The Philippine Institute of Volcanology and Seismology (PHIVOLCS).
  3. ^ Mount Pinatubo Eruption - Mount Pinatubo
  4. ^ "Tarlac map". University of Texas in Austin Library. Retrieved 2011-08-02.
  5. ^ "Report of the Philippine Commission to the President, 1901 Vol. III", pg. 141. Government Printing Office, Washington, 1901.
  6. ^ أ ب "The Cataclysmic 1991 Eruption of Mount Pinatubo, Philippines". Retrieved 2007-04-09.
  7. ^ "Two Years of Lahars on the Western Flank of Mount Pinatubo: Initiation, Flow Processes, Deposits, and Attendant Geomorphic and Hydraulic Changes". USGS Publications. Retrieved 2012-03-07. {{cite web}}: Cite uses deprecated parameter |authors= (help)
  8. ^ Stephen Self; Jing-Xia Zhao; Rick E. Holasek; Ronnie C. Torres; Alan J. King (1999). "The Atmospheric Impact of the 1991 Mount Pinatubo Eruption". Retrieved July 25, 2014. {{cite web}}: Unknown parameter |last-author-amp= ignored (|name-list-style= suggested) (help)
  9. ^ "Mt. Pinatubo's cloud shades global climate". Science News. Retrieved 2010-03-07.
  10. ^ Tactical Pilotage Chart, Sheet K-11B, Defense Mapping Agency, Department of Defense, 1982.
  11. ^ Philippine Census
  12. ^ خطأ استشهاد: وسم <ref> غير صحيح؛ لا نص تم توفيره للمراجع المسماة usgs
  13. ^ Rosenberg, Matt. "Mount Pinatubo Eruption - The Volcanic Mount Pinatubo Eruption of 1991 that Cooled the Planet".
  14. ^ Garret, R.G. (November 2000). "Natural sources of metals in the environment". Human and Ecological Risk Assessment: an International Journal. 6 (6): 945–963. doi:10.1080/10807030091124383.
خطأ استشهاد: الوسم <ref> ذو الاسم "expoedu" المُعرّف في <references> غير مستخدم في النص السابق.

مراجع


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