Thera are in Bali about 1000 Swedish tourists waiting the flight back to Swedn. Flights are cancelled yet.
Where is Bali is there r alternative ways to travel back home from Bali?frpm, Bali to Australia 1300 km. Thera are boats. 1300 is as long a journey as from Helsinki to the uttermost Northern point of Finnish lapland. Lappland.
JOHN SEACH Volcano News from Bali:
Volcano News, November 2017
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Archived Volcano News
Monday 27th November 2017
Agung Volcano, Bali, Indonesia
Renewed eruption of Agung volcano, Indonesia sent ash to an altitude of 30,000 ft. Exclusion zone increased to radius of up to 10 km from the crater. Agung was raised to highest level 4 alert.
More on Agung Volcano…
Volcanoes of Indonesia…
Wednesday 22nd November 2017
Agung Volcano, Bali, Indonesia
A summit eruption occurred at Agung volcano, Bali, Indonesia, 21st November 2017. Small ash cloud rising 700 m above summit and drifting east. Five villages affected by the ash, including Pidpid, Nawakerti, Bukit Galah, Sebudi and Abang.
More on Agung Volcano…
Volcanoes of Indonesia…
Monday September 2017
Ambae Volcano, Vanuatu
A summit eruption has been reported at Ambae volcano, Vanuatu. A new cinder cone formed in the summit lake, and a lava pond is visible. This is the first time a lava pond has been observed at Ambae volcano.
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Volcanoes of Vanuatu…
Sunday 24th September 2017
Agung Volcano, Bali, Indonesia
On 22nd September 2017, Agung volcano, Bali was raised to maximum level 4 alert. 35,000 people were evacuated. Previous reported eruptions of Agung were in 1963, 1843, 1821?, 1808. The last eruption in 1963 was similar in magnitude/intensity to Mt St Helens (1980) and Mt Vesuvius (79 AD).
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Volcanoes of Indonesia…
Sunday 24th September 2017
Ambae Volcano, Vanuatu
Activity increased at Ambae volcano, Vanuatu on 23 September 2017. Ash emissions occurred from the summit. The alert level was raised to 4 (out of a maximum 5). Preparations were being made to evacuate up to 5000 people.
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Volcanoes of Vanuatu…
Tuesday 19th September 2017
Agung Volcano, Bali, Indonesia
On 18th September 2017, Agung volcano, Bali was raised to level 3 alert (out of a maximum 4). People are advised not to climb or camp inside Agung crater, and in areas within a 6 km radius of Agung, or at elevations above 950 m from sea level. The exclusion zone radius is increased to 7.5 km in the North, Southeast and South-Southwest. An increase in earthquakes at the volcano is caused by magma pressure cracking rocks. The history of activity at Agung indicates the potential threats of pyroclastic falls, pyroclastic flows, and lava flows. Agung volcano last erupted in 1963. The eruptions of Agung volcano in 1963 created a crimson sunset glow over America and Europe.
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Volcanoes of Indonesia…
About Submarine´s fate
November 24, 2017
http://edition.cnn.com/2017/11/23/americas/argentina-submarine/index.html
An explosion incidence can be possible according registered data. Searching of the submarine is going on under difficult circumstances, stormy weather, waves can be 8 meter high. The sea bottom along Argentine coast line has also very peculiar complex geomorphology with a steeps towards abyssus , where no rescue is possible. Searching is made in frames of possibilities and probabilities. Enormous international searching operation is going.
Submarine may be localized at 230ft depth ( 70 m)
November 22, 2017
http://www.dailymail.co.uk/news/article-5106689/Missing-Argentine-submarine-located-Navy.html
Geomorphology
Volume 128, Issues 3–4, 15 May 2011, Pages 116-136
Submarine canyon formation and evolution in the Argentine Continental Margin between 44°30’S and 48°S
Author links open overlay panel G.LastrasabJ.AcostabA.MuñozcM.Canalsa
a
GRC Geociències Marines, Universitat de Barcelona, E-08028, Spain
b
Instituto Español de Oceanografía, E-28002, Madrid, Spain
c
TRAGSA – Secretaría General del Mar, E-28006, Madrid, Spain
Received 4 May 2010, Revised 23 November 2010, Accepted 24 December 2010, Available online 3 January 2011.
https://doi.org/10.1016/j.geomorph.2010.12.027Get rights and content
Abstract
In the framework of the Vulnerable Marine Ecosystems (VME) of the High Seas of the South West Atlantic, large areas of the Argentine Continental Margin (ACM) between 44°30’S and 48°S have been swath-mapped for the first time, obtaining full data coverage of the seafloor in this region between the outermost continental shelf and the middle slope down to 1600 m water depth.
https://ars.els-cdn.com/content/image/1-s2.0-S0169555X10005714-gr16.jpg
The slope is characterized by the presence of smooth terraces (Nagera, Perito Moreno and Piedra Buena) that widen towards the south, limited by morphological steps with evident signs of erosion in the form of scours. These terraces form part of the Argentine contourite depositional systems, generated by the interaction of the northwards flowing Antarctic water masses with the seafloor. Within the studied area, seven canyons and their multiple branches dissect the upper and middle continental slopes, from west to east, across the terraces and the steps.
These canyons, which belong to the Patagonia submarine canyon system and are collected at a depth of ~ 3.5 km by a slope-parallel, SSW–NNE-oriented channel known as the Almirante Brown transverse canyon, display a large variety of morphologies. These include incisions from just a dozen of metres to 650 m, straight to highly meandering sections with sharp bends, well-developed levees and walls that reach 35° in slope gradient, hanging branches, conspicuous axial incisions and multiple knickpoints. Only the northernmost canyon indents in the continental shelf, whereas the others start at the limit between the upper and middle slopes, and are often fed by small, straight, leveed gullies.
The action of both across-slope processes represented by submarine canyons and along-slope processes represented by terracing and scouring conform the ACM as a peculiar mixed margin, with the presence of both contour and gravity currents at the same place at the same time. We propose that at present, along-slope erosion and transport mainly occurs along the Perito Moreno terrace, whereas across-slope processes are much more dominant in the Nagera terrace. Erosive bedforms such as crescent scours, generated by contour currents, contribute to the progressive bottom-up erosion of the Nagera terrace and act as an initial collector of across-slope transported sediment, that later, due to flow focusing and recurrence, incise and interconnect creating definitive canyons that progress upslope by retrogressive erosion until their head indents the shelf break.
Changes in the balance between across-slope and along-slope transport would imply a disequilibrium in the combination of processes leading to canyon formation, producing canyon abandonment, and partial or total filling. These changes could be produced by a variation in the depth of the main interfaces of Antarctic water masses leading to either an increase or a decrease in the erosion and transport capacity of contour currents, and/or by an enhancement of across-slope transport related to an increase of sediment availability.
Keywords
Submarine canyon
Contourite depositional system
Argentina Continental Margin
Gullies
Canyon formation
Missing submarine
November 21, 2017
CNN 21.11. 2017
How long could the crew survive?
Argentina: Missing Submarine, 44 inside
November 20, 2017
PM of Lebanon went to Saudia
November 12, 2017
Lebanon’s president urged Saudi Arabia on Saturday to explain why Saad Hariri had not returned to Beirut since his surprise resignation as prime minister a week ago.
Hariri announced on November 4 in a televised statement from Riyadh that he would be stepping down from the post, sending shock waves through Lebanese politics.
The premier has yet to return to Lebanon and rumors have swirled that he is being held in Saudi Arabia against his will.