> Coba kita tengok bagaimana jurnal-jurnal ilmiah luar negeri mengulas LUSI
> ini. Saya mengamati beberapa, dan ternyata semua sama yaitu bahwa mereka
> hanya sepakat bahwa Lusi adalah "mud volcano eruption" Apa penyebab
> erupsinya ? Gempakah, pengeboran Lapindokah ? Tak tahu. Besar kemungkinan
> dua-duanya. Sebuah jurnal menyebutkan juga gejala geotermal. Di bawah ini
> adalah salah satunya.
>
> Salam,
> Awang
>
>
> Mud volcano floods Java
>
>
> Disaster-plagued Indonesian island faces new threat.
>
> by Richard Van Noorden
>  <http://www.nature.com/news> [EMAIL PROTECTED]
> What Has Happened ?
> For 3 months a sea of hot mud has been gushing from the ground in
> Sidoarjo, East Java, 35 kilometres south of Indonesia's second largest
> city, Surabaya. The steaming mud pool is growing at an estimated 50,000
> cubic metres a day, accompanied by hydrogen sulphide gas, and now
> reportedly covers more than 25 square kilometres. The flow has not yet
> been stopped; thousands of people have lost their homes.
>
> How bizarre... has this sort of disaster happened before?
>
> The Sidoarjo disaster is an example of a 'mud volcano'.
________________________________________________________________________

  Mud and gas
> accumulates when sea sediments are trapped in subduction zones, where one
> tectonic plate slides under another, and can erupt out of volcanic cones
> or simply from a crack in the ground.

  Kang Awang.

  Re- keterangan diatas , bagaimana mengaplikasikan - nya dalam kasus
  Sidoarjo  ?

  Apakah posisi subduction zone dan  saat sedimentasi  mendukung pendapat
  diatas ?

  Kelihatannya kita harus melihat dan belajar dari kejadian kejadian di -
  region lain untuk menambah data sebelum suatu kesimpulan final dicapai.
  Hal ini penting SEKALI karena akan menyangkut suatu keputusan Pengadilan
  dalam banyak "pengaduan dari masyarakat".

  Si- Abah

  ________________________________________________________________________



 Mud volcanoes have burst on every
> continent, but are abundant in the South Caspian region (offshore and
> onshore Azerbaijan) and offshore Indonesia in the East Java Basin.
> But the Sidoarjo mud volcano is rather unusual. It's huge. And, says Sam
> Rice, a geologist at the University of Cambridge, UK, reports of the mud
> eruption suggest that it is a hybrid between typical mud volcanoes and
> hydrothermal vents. The mud is of an unusually high temperature (60 °C)
> and contains enormously high concentrations of hydrogen sulphide gas. This
> suggests that some kind of volcanic, hydrothermal activity is going on at
> the same time.
>
> What creates the conditions for a mud volcano?
>
> Achim Kopf, a geologist from the University of Bremen, Germany, who has
> studied mud volcanoes extensively, explains that marine sediment can be
> scraped off an oceanic tectonic plate as it slides underneath a
> continental plate. If the sediment accumulates rapidly and water is
> trapped in its pores, this can stop the sediment being cemented by
> pressure. The resulting reservoir of mud can be trapped underground. In
> the case of the East Java mud flow, the mud is thought to have come from a
> reservoir some 2.7 kilometres below the Earth's surface.
>
> And what triggers an eruption?
>
> A number of things can create a crack that allows trapped mud to bubble to
> the surface; particularly earthquakes and drilling.
>
> And in Java specifically?
>
> In Java both of these things have happened recently. The oil and gas
> exploration company PT Lapindo Brantas is drilling in the area, and the
> gas and hot mud first spewed from the company's drilling rig on 28 May.
> Geologist Georg Delisle of the Federal Institute for Geosciences and
> Natural Resources (BGR), Hannover, Germany, explains that the drilling
> apparently penetrated into the liquid sediment and created a connection
> back to the surface. The pressure then squeezed up the mud, like
> toothpaste from a tube. But it is likely that other connections were made
> to the surface, he adds not just through the drilling pipe because
> attempts to pump concrete into the pipe to block the flow of mud have
> failed.
> On 27 May an earthquake struck and devastated Yogyakarta on Java, and this
> too could have cracked the ground, potentially helping to release the mud.
> But the quake's epicentre was some 300 kilometres away from the mud
> volcano (making it only 2 on the Richter scale in that area).
> The issue of what, exactly, caused this disaster is highly politically
> charged. It is still under investigation by police, the government and
> international experts.
>
> Just how big is the eruption?
>
> According to many geological experts, the scale of this mud volcano is
> unprecedented at least on land.
> In 1945, the Makran earthquake in Pakistan triggered the sudden emergence
> of three offshore mud volcanoes, and in March 1999 a mud volcano rose out
> of the water overnight to form Malan Island, 3 kilometres from Pakistan's
> coast. It is hard to estimate the volume of mud created by such underwater
> eruptions. And, notes Rice: "Because the extrusion of mud and toxic gas
> occurs on the seabed it does not threaten human life and does not make the
> headlines."
> 'Well-kick' the sudden surface eruption of gas and mud during offshore oil
> drilling is common, but usually stops after a few days. Delisle recalls a
> smaller-scale incident in the 1960s where a geothermal well in the
> Wairakei geothermal field, New Zealand, ran wild: it took 3 months to stop
> the geothermal steam that found its way to the surface alongside the
> original borehole.
>
> Can the disaster be stopped?
>
> Nobody knows. So far, nothing has worked. PT Lapindo Brantas's senior
> vice-president Imam Agustino has been quoted saying: "The best-case
> scenario [for stopping the mudflow] is now mid-November, but I have to
> admit it might never be stopped."
> Visit our newsblog to read and post comments about this story.
> Article Copyright © 2006 MacMillan Publishers Ltd.
> <http://www.macmillan.com>  All rights reserved. This material may not be
> published, broadcast, rewritten, or redistributed.
>
>



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