Puncak Erupsi Rinjani benar di Abad 13 kalo menurut literatur yang ada,
seperti kata Abstract-paper di bawah ini:

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Eruptive history during the last 10 ky for the caldera-forming eruption
ofRinjani volcano, Indonesia

# Akira Takada[l], Asnawir Nasution[2], Rosgandika Mulyana[2]

[I] GSJ,AIST, [2] Volcanology and Geologic Hazard Mitigation, Indonesia


  Rinjani volcano, Lombok island (edifice volume: 100 km3), Indonesia, had
grown on the eastern flank of Central Lombok volcano complex (edifice
volume: 850 km3). The eruptive history ofRinjani volcano is divided into
Stratocone building stage, Low volcanic activity stage, and Syn-caldera
stage. Eruption rate was kept constant during Stratocone building stage. It
decreased to 0.6 km3/ky  during the last period of Stratocone building stage
(12000-6000 y.B.P.). Finally, it became 0.15 km3/ky  during the last 5200
years before the caldera-forming eruption (6000-800 y.B.P.) (Low activity
stage). At Low activity stage, eruption interval became longer than the
previous stage; subplinian Propok pumice (DRE volume: 0.1 km3) and Lember
lava flow (volume: 0.4 km3), Rinjani asb, and subplinian Rinjani pumice (ORE
volume: 0.3 km3)  occurred. Plagioclase-phyric basalt, and andesite became
common for the last period of Stratocone building stage. Dacite with hydrous
minerals erupted during Low activity stage. The main magma path shifted 5 km
toward the eastern flank of Central Lombok volcano complex to grow Rinjani
volcano at the end of the complex. Afler stratocone building, the volcanic
activity migrated more 5 km eastward for Low activity stage. Pmpock pumice
and Lembah lava flow erupted. Next, the activity migrated back to Rinjani
summit. Rinjani ash and Rinjani pumice erupted. Syn-caldera stage started
with plinian West Rinjani pumice (DRE volume: 3 km3)  at the center of
Central Lombok volcano complex.    Segaraanak caldera collapsed with
eruption of huge pyroclastic flows (The subarea! ORE volume: 7 km km3),  not
at Rinjani, but at the center of Central Lombok volcano complex. The dated
results of seven charcoals indicate the climax of caldera forming-eruption
is the period of AD 1210-1260 years B.P. The caldera collapse may have been
associated with the sector collapse of the western flank of Rinjani volcano.
The present caldera is 6 km x 7 km in size of rim to rim, and, in its
eastern part, is connected to a horseshoe-shaped caldera of 3.5 km long and
3.5 km wide.

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-----Original Message-----
From: Budi Brahmantyo [mailto:bud...@gc.itb.ac.id] 
Sent: 20 Juli 2012 16:01
To: iagi-net@iagi.or.id
Subject: RE: [iagi-net-l] Erupsi besar gunungapi, abad ke 13 di Indonesia ?

Setahu saya Kaldera Rinjani terbentuk 14.000 tahun yang lalu (cross
reference ke pak Heryadi Rachmat).

BB



> Pak Yatno, Frank Lavigne memang belum mau bilang Gunung Api di 
> Indonesia yang mana yang meletus tahun 1257/8 AD yang menyebabkan 
> dunia menjadi dingin dan memasuki jaman es kecil itu (i.e. little ice 
> age).  Mungkin takut dibajak orang lain meneliti/mempublikasikannya.  
> Tapi sebagian ahli menduga kuat yang dimaksud adalah Rinjani.  Di 
> http://en.wikipedia.org/wiki/Mount_Rinjani disebutkan kaldera Rinjani 
> terbentuk di Abad 13, tapi belum ada info tahun persisnya. Di copy-an 
> berita di bawah katanya  sudah ada charcoal dating yang menunjuk ke 
> 1210-1260 AD untuk letusan Rinjani itu.  Jadi bagi saya sih logis saja 
> kalo mengajukan Rinjani sebagai tersangka-nya kalau memang info umur 
> kaldera ini benar.
>
>
>
> Hayoo siapa yang mau ngedulu-in si Frank, buruan  J
>
>
>
> Salam,
>
> DHN
>
>
>
> Di bawah ini komentar seorang ahli tentang isue Si Frank dan Rinjani itu:
>
> http://goodnewsfromindonesia.org/category/nature/
>
> If you’ve been following the news out the AGU Chapman Meeting of 
> Volcanoes & the Atmospheremeeting going on this week, you might have 
> seen some interesting news about the missing 1258 A.D. eruption. I 
> wrote about the eruption a few months back, speculating on some 
> potential volcanoes that could be the culprit for this 
> climate-altering event. However, trying to match a sulfate signal on 
> the poles with a volcano somewhere on the planet is hard, so finding 
> that “smoking gun” is a challenge to say the least.
> However, Franck Lavigne  from the Panthéon-Sorbonne University’s 
> Laboratory of Physical Geography in Meudon, France claimed to have 
> solved the mystery.
> It isn’t that simple, though. Lavigne will not reveal the site of the 
> eruption until his study is published (it may or may not be submitted 
> for peer review at this point). So, instead of sharing news of his 
> discovery, he showed the data he used to “solve” the mystery … but 
> never revealed what volcano it was! What harm could come from Lavigne 
> revealing his location before the article is published, especially if 
> he is willing to show data that supposedly correlates the sulfate and 
> ash composition in the polar record with the terrestrial record of the 
> mystery volcano? Overall, this is shocking behavior for a geologist at 
> a large meeting such as this – people commonly discuss data and 
> information that has not be published yet, so why Lavigne chose to do 
> this is beyond me (unless you want to think theatrics are part of the 
> rationale).
>
> The consensus of people at the meeting (N.B., I am not at the meeting) 
> is that the mystery volcano is in Indonesia. Lavigne wouldn’t confirm 
> or deny this assessment, but it got me thinking – what might a 
> contender be for a caldera eruption in Indonesia during the 13th 
> century. Indonesia is filled with volcanoes, and as I mentioned a few 
> weeks back when I discussed a recent study by Salisbury and others 
> (2012), we really don’t have a lot of good ages for Indonesian 
> eruptions prior to ~1800 A.D. However, one very likely candidate might 
> be the ~6 x 8.5 km Rinjani caldera. Rinjani hosts a caldera that may 
> have formed in the 13th century, so it not only fulfills the role of 
> being a large eruption but also falls within the right century.
> We don’t have any good ages for the caldera eruption beyond some 
> charcoal dated at 1210-1260 A.D. However, with the evidence that 
> Lavingne’s volcano is in Indonesia and how little we know about the 
> caldera eruption at Rinjani, it makes sense that Rinjani could be an 
> excellent candidate for an eruption that could be matched with the 
> polar sulfate and ash.
>
> At this point, all we can do is wait for Lavigne’s study to be 
> published, but we might be able to narrow the search for the 1257-58 
> eruption to Indonesia – and even to a target caldera that might be the 
> weapon of choice.
>
>
>
>
>
>
>
> From: Yustinus Suyatno Yuwono [mailto:yuw...@gc.itb.ac.id]
> Sent: 06 Juli 2012 15:23
> To: iagi-net@iagi.or.id
> Subject: RE: [iagi-net-l] Erupsi besar gunungapi, abad ke 13 di 
> Indonesia ?
>
>
>
> Rekan Danny,
>
> Gak peduli Bule atau Melayu, kalo statement nya (maaf) terlalu berani 
> dan menurut saya (terbatas pada disiplin ilmu yang saya tekuni) kurang 
> logis ya saya akan berikan opini. Contohnya ini: G. Rinjani meletus 
> dengan skala letusan 7 pada abat 13???????? Begitu bodohnya orang 
> Indonesia pada waktu itukah, sehingga sama sekali tidak ada catatan 
> mengenai peristiwa alam begitu dahsyatnya? Misal dalam Babat Tanah 
> Jawi atau legenda rakyat dan sejenisnya (barangkali Awang Satyana bisa 
> memberi pencerahan krn koleksi bukunya luar biasa, sebagai referensi). 
> Kedua, tidak ada catatan dari Direktorat Volkanologi yang pernah saya 
> baca dan dengar mengenai super erupsi Rinjani pada abat tersebut? 
> Ketiga, data yang kita lihat lewat satelit dapat memperlihatkan berapa 
> ukuran kaldera dari G Rinjani ini yang diakibatkan super erupsi ini? 
> Kalau melihat ukuran kalderanya mungkin Kaldera Tengger lebih prospek 
> jadi kandidatnya (hanya melihat ukuran kaldera), tapi saya tidak tahu 
> apakah Dir Volk kita sudah punya data umur kapan terbentuknya kaldera 
> Tengger (dan juga Rinjani?).
>
> Danny, jangan tersinggung kalau saya ber-opini keras terutama yang 
> menyangkut bidang saya, inilah gunanya sharing pengetahuan.
>
> Salam,
>
> Yatno (YSY).
>
>
>
> From: Danny Hilman Natawidjaja [mailto:danny.hil...@gmail.com]
> Sent: Tuesday, July 03, 2012 1:40 PM
> To: iagi-net@iagi.or.id
> Subject: RE: [iagi-net-l] Erupsi besar gunungapi, abad ke 13 di 
> Indonesia ?
>
>
>
> Salah besar pak.
>
> Culpritnya memang Rinjani.  Bisa dilihat di:
>
>
>
> http://www.sciencenews.org/view/generic/id/341497/title/13th_century_v
> olcano
> _mystery_may_be_solved
>
>
>
> http://en.wikipedia.org/wiki/Mount_Rinjani
>
>
>
> http://volcano.oregonstate.edu/aggregator/sources/9
>
>
>
>
>
> From: Yustinus Suyatno Yuwono [mailto:yuw...@gc.itb.ac.id]
> Sent: 03 Juli 2012 12:05
> To: iagi-net@iagi.or.id
> Subject: RE: [iagi-net-l] Erupsi besar gunungapi, abad ke 13 di 
> Indonesia ?
>
>
>
> He… geodukun lagi?????
>
> YSY
>
>
>
> From: abacht...@cbn.net.id [mailto:abacht...@cbn.net.id]
> Sent: Saturday, June 16, 2012 7:48 PM
> To: iagi-net@iagi.or.id
> Subject: Re: [iagi-net-l] Erupsi besar gunungapi, abad ke 13 di 
> Indonesia ?
>
>
>
> Gunung Rinjani, Vick.
>
> Powered by Telkomsel BlackBerry®
>
>   _____
>
> From: Rovicky Dwi Putrohari <rovi...@gmail.com>
>
> Date: Sat, 16 Jun 2012 19:31:05 +0700
>
> To: IAGI<iagi-net@iagi.or.id>; geologi...@googlegroups.com 
> <mailto:geologi...@googlegroups.com%3cgeologi...@googlegroups.com>
> <geologi...@googlegroups.com>
>
> ReplyTo: <iagi-net@iagi.or.id>
>
> Subject: [iagi-net-l] Erupsi besar gunungapi, abad ke 13 di Indonesia ?
>
>
>
> Gunung mana ya ?
>
>
>
> Rdp
>
>
>
> http://www.sciencenews.org/view/generic/id/341497/title/13th_century_v
> olcano
> _mystery_may_be_solved
>
>
>
>
> 13th Century Volcano Mystery May Be Solved - Science News
>
>
> SELFOSS, Iceland — One of the biggest mysteries in volcanology may 
> finally have a solution. An eruption long thought to have gone off in 
> the year 1258, spreading cooling sulfur particles around the globe, 
> happened the year before in Indonesia, scientists report.
>
> Until now, researchers have known a big volcano went off somewhere in 
> the world around that time, but they didn’t know exactly where or when.
>
> The new report still remains something of a mystery. Franck Lavigne, a 
> geoscientist at Panthéon-Sorbonne University's Laboratory of Physical 
> Geography in Meudon, France, showed data and close-up photographs of 
> the remains of the perpetrator volcano on June 14 at an American 
> Geophysical Union conference on volcanism and the atmosphere. But he 
> declined to name the specific volcano, saying he had agreed with his 
> international colleagues not to identify it until the work is 
> published in a peer-reviewed journal.
>
> “We have new and solid evidence for the biggest volcanic eruption in 
> 7,000 years,” Lavigne said.
>
> Consensus in the meeting hallways was that he showed pictures of 
> Indonesia.
> Lavigne would say only that Indonesia has more than 130 active volcanoes.
>
> Scientists know a big eruption must have happened in the mid-13th 
> century because ice cores from Greenland and Antarctica dating to that 
> time contain huge amounts of sulfur. Tree rings, historical records 
> and other evidence also show that the planet cooled soon thereafter. 
> Big volcanic eruptions can spew sulfur particles into the upper 
> atmosphere, where they spread around the globe and reflect sunlight, 
> temporarily chilling the planet.
>
> Leading candidates for the 1258 eruption have included Mexico’s El 
> Chichón, which also erupted in 1982, and Quilotoa in the Ecuadorean 
> Andes. But the chemical composition of rocks from those volcanoes, 
> among other factors, don’t really match the 1258 sulfur from ice 
> cores.
>
> At the meeting, Lavigne showed geochemical analyses of rocks from his 
> mystery volcano. They matched the chemistry of the polar sulfur almost 
> perfectly. The rocks come from a caldera, the collapsed remains left 
> behind after a large volcanic eruption drains an underground magma 
> chamber.
>
> Newly unearthed historical records and other evidence show that 
> climate changes were already happening in the region by the winter of 
> 1257-1258, Lavigne said. “We think the eruption may have been in the 
> late spring or summer of 1257,” he said. That’s nearly a year earlier 
> than previously thought.
>
> Computer simulations suggest the eruption sent pumice flying into the 
> air more than 40 kilometers high, showering debris for tens of 
> kilometers around. The eruption would have ranked a 7 on the volcanic 
> explosivity scale that measures an eruption’s magnitude. That scale 
> tops out at 8.
>
> Still, volcanologists have spent decades looking for the source of the
> 1257/1258 eruption. It’s not yet clear whether Lavigne will be able to 
> marshal enough evidence to convince everyone else.
>
>
>
>
>
> --
> "Sejarah itu tidak pernah usang untuk terus dipelajari"
>
>



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Jangan lupa PIT IAGI 2012 di Jogjakarta tanggal 17-20 September 2012.
Kirim abstrak ke email: pit.iagi.2012[at]gmail.com. Batas akhir pengiriman 
abstrak 28 Februari 2012.
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Pembayaran iuran anggota ditujukan ke:
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