Talk:Types of volcanic eruptions

message: I disagree with the speedy deletion nomination of this page. The tag is completely wrong- this is not a non-notable group of people, at all, it is a description of the different types of volcanic eruptions. There is no reason to delete this page, unless it is original research, which I do not believe it is. It needs sources, wikifying and sections, but the content of the article and its style of writing is sound. I will now contact the page author to ask them about sources. J Milburn 16:37, 14 January 2007 (UTC)
thread_title: Disagree with speedy deletion

message: to the information already available in Volcano.  Paul 16:40, 14 January 2007 (UTC)
replies: text: I have not read the article from start to end, but I cannot see this information anywhere. Could you be more precise? Where is it explained in the Volcano article? J Milburn 16:56, 14 January 2007 (UTC)
thread_title:  this article adds nothing 

message: I am currently in the process of rewriting the article, so that it is not a copyright violation, in my sandbox. Please do not delete it in the mean time. J Milburn 17:06, 14 January 2007 (UTC)
replies: text: Done. J Milburn 17:24, 14 January 2007 (UTC)
thread_title:  Rewrite 

message: Good work - thanks for cleaning it up. Paul 17:28, 14 January 2007 (UTC)
thread_title:  much better 

message: In compiling information from various places on Wikipedia to improve Hawaiian eruption beyond stub status, I removed the description of Hawaiian eruptions from this page because it appeared to be WP:COPYVIO from a book called Geology Super Review.  Further research, however, appears to reveal that the original source of the text was a U.S. government publication.  So I'll restore the text but add a link to the above USGS glossary.  Sorry for the confusion. PubliusFL 20:17, 1 April 2007 (UTC)
replies: text: All information was originally copied from the link at the bottom by a new editor, and then edited by me to stop it being a copyvio. I'll move the external link to the references section. J Milburn 20:22, 1 April 2007 (UTC)
thread_title: Hawaiian eruption

message: In the part regarding Mount Erebus, it states that Erebus has been erupting since 1972. This is in fact wrong. Members of the expedition lead by the British explorer Sir Ernest Shackleton ascended Erebus during the 1907-1909 British Antarctic expedition and peered intot he crater. They reported the existence of a pulsating lava lake. Earlier than Shakleton other expeditions had reported the there was a plume of "smoke" from the volcano. Indeed it was during an expedition in 1841 lead by Sir James Clark Ross that the volcano was named after one of his ships - Erebus, and he reported the existence of the plume. It was in 1972 that the Mount Erebus Observatory was set up by the New Mexico Institute of Mining and Technology.The Geologist (talk) 16:16, 9 August 2015 (UTC)
thread_title: Strombolian eruption - Mount Erebus

message: It is not clear what is the the difference between Plinian and Vesuvian types of eruptions. Aren't these two names of one type? After all, the Plinian was named after the Mount Vesuvius eruption first description by Pliny the Younger.
::I agree with the unsigned comment. I've read they were actually named for Pliny the Elder who died during the 79 eruption. I'm removing Vesuvian from the list. Anynobody 09:43, 24 May 2007 (UTC)
replies: text: The images of a Stone Pine I found online indicate Plinian eruptions are formed in the same manner as thunder clouds: The ability to rise unimpeded until it breaks through the relatively still air or perhaps reaches a layer where the physics of gas laws allows it to spread out evenly. Has there been any research into that idea?
Weatherlawyer (talk) 14:01, 21 May 2016 (UTC)
thread_title:  What is the difference? 

message: There are three Types of volcanic eruption: Magmatic, Phreatomagmatic and Phreatic. Magmatic and phreatomagmatic eruptions produce juvenile clasts or new material, phreatic does not. magmatic eruptions do not include water. There are three mechanisms of ash formation: gas release under decompression causing magmatic eruptions; thermal contraction from chilling on contact with water causing phreatomagmatic eruptions and ejection entrained particles during steameruptions causing phreatic eruptions (Heiken & Wohletz 1985). The Types that you have listed are merely aspects of these groups,a hawaiian, strombolian, vulcanian, plinian these are all types of MAGMATIC eruption, with the different eruption styles being a result of varying mass flux. Ta-aalian, surtseyan and phreato-plinian are all types of phreatomagmatic eruption, with the only difference being the varying mass flux and the varying ratio of mass flux of lava to mass flux of water. For example a surtseyan eruption style is a phreatomagmatic eruption caused by thermal contraction on contact with water, where the mass flux of magma is relatively low compared to the mass flux of an ocean or large lake. The phreato-plinian on the other hand would have relatively equal mass flux of water and magma caused by, for example rising magma interacting with an acquifer.
A distinction also needs to be made between effusive and explosive eruption; Hawaiian is effusive, strombolian is explosive [B] both[/B] are magmatic.
So a vesuvian eruption is also a type of plinian eruption
Reference cited: Heiken, G. & Wohletz, K. 1985. Volcanic Ash. University of California Press, Berkeley.  —Preceding unsigned comment added by Russjass (talk • contribs) 13:12, 12 May 2008 (UTC)
replies: text: Although your observations are correct in respect of causation, the classifications discussed here are based on the overall violence (energy and mass release) exhibited by a given eruption, and hence a relative measure of the potential human/planetary impact. This is to some extent quantified by the VEI, but both schemes are useful and continue to be widely used. Peter b (talk) 04:52, 2 March 2012 (UTC)
thread_title: you may be missing the point

message: Plinian and vesuvian and strombolian etc are all magmatic eruptions as i have said above. they are distinguished by eruption column height and mass flux with hawaiian fire fountains being the lowest and ultra-plinian being the heighest. Paraxysmal is a term that is not used any more. The column height of many old and ancient eruptions cannot be known, nor can mass flux, but they can be estimated by isopleth mapping of the tephra apron, wich will give an estimation. the system is subjective due to the relative ease with which tephra can be eroded, for example the 1991 eruption of Pinatubo, within months the majority of tephra had been reworked into the sea, giving very very conservative estimates of the column height, which were much lower than the observed column.
Phreatomagmatic eruptions are plotted on a different scale, because the eruptive mechanisms are too different to compare, but mass flux and column height are the distinguiching characteristics.
Russjass (talk) 13:33, 12 May 2008 (UTC)
thread_title:  Difference between plinian and vesuvian 

message: Should I put the origins of the name of this eruption? Firio (talk) 17:40, 24 February 2009 (UTC)
replies: text: No, because I already did. --The High Fin Sperm Whale (talk) 18:12, 22 October 2009 (UTC)
thread_title: Peléan

message: I think that it seems rather out of place. If it took place under a glacier, shouldn't it be a subglacial eruption? Thus, I see no reason why it should be put there arnd on the page "Volcano" because it was just another eruption. Sure, it might have beeen a very large eruption, but then it should be given its own page, if it hasn't been given one already. 
--Guanlong wucaii  —Preceding undated comment added 09:01, 2 June 2009 (UTC)
replies: text: I agree. If the eruption happened under an ice sheet it would therefore be a subglacial eruption. --The High Fin Sperm Whale (talk) 18:10, 22 October 2009 (UTC)
thread_title:  ''Antarctica Eruption'' 

message: Why does the article call Kelud 'Mt Kelut' when the WP article itself is named 'Kelud'? Also, I see the name Kelud/Kelut (without a 'Mt' in front) more often. --Guanlong wucaii 12:41, 4 February 2010 (UTC)
thread_title:  Kelud 

message: I think it would be worth including a link to the Volcanic Explosivity Index page, as this is an important part of classifying eruptions.
 TimKasoar (talk) 10:31, 4 June 2010 (UTC)
thread_title:  VEI 

message: This page is an absolute mess! I should probably get to it, after I'm done with Seamount. ResMar 02:44, 26 July 2010 (UTC)
replies: text: Comming out good. Volcanoguy 22:55, 1 August 2010 (UTC)
replies: text: It's at GAN now. ResMar 01:46, 10 August 2010 (UTC)
thread_title:  Tisk... 

message: Is there any real reason why this article can't be named volcanic eruption? Articles with "types of ..." in the title would normally be lists, and this is more than a list. JFW | T@lk 06:13, 11 August 2010 (UTC)
thread_title:  Name 

message: 'During a volcanic eruption, lava, tephra (ash, lapilli, volcanic bombs and blocks), and various gases are expelled from a volcanic vent or fissure. Several types of volcanic eruptions have been distinguished by volcanologists. These are often named after famous volcanoes where that type of behavior has been observed. Some volcanoes may exhibit only one characteristic type of eruption during a period of activity, while others may display an entire sequence of types all in one eruptive series.
There are three different metatypes of eruptions. The most well-observed are magmatic eruptions, which involve the decompression of gas within magma that propels it forward. Phreatomagmatic eruptionItalic texts are another type of volcanic eruption, driven by a the compression of gas within magma,the direct opposite of the process powering magmatic activity. The last eruptive metatype is the Phreatic eruption, which is driven by the superheating of steam via contact with magma; these eruptive types often exhibit no magmatic release, instead causing the granulation of existing rock.
Within these wide-defining eruptive types are several subtypes. The weakest are Hawaiian and submarine, then Strombolian, followed by Vulcanian and Surtseyan. The stronger eruptive types are Pelean eruptions, followed by Plinian eruptions; the strongest eruptions are called "Ulta Plinian." Subglacial and Phreatic eruptions are defined by their eruptive mechanism, and vary in strength. An important measure of erruptive strength is Volcanic Explosivity Index (VEI), a magnitudic scale ranging from 0 to 8 that often correlates to eruptive types.'Bold text  —Preceding unsigned comment added by IloveMirza (talk • contribs) 12:47, 11 August 2010 (UTC)
thread_title:  Volcanic Eruptions 

message: Quote, former wiki text: "Only five of these types of eruptions have occurred in historical times, often in very remote regions, ()..." I think this revision is wrong. Does not a subglacial eruption only occur when tuyas are formed ??? --Chris.urs-o (talk) 15:17, 30 August 2010 (UTC)
replies: text: Subglacial eruptions can also occur without the formation of a tuya. They can happen when subglacial mounds are being formed or when shields, calderas, etc erupt under ice sheets. The only historical subglacial eruptions I know of took place in Iceland. Volcanoguy 00:30, 4 June 2011 (UTC)
thread_title:  Subglacial eruption 

message: I would very much like to understand more about volcanic eruptions on Jupiter's moon Io and other non-Earth instances. How does the liquid magma on such a cold far-from-the-sun extra-terrestrial body, Io, compare to that on Earth? Do we believe that it is the same type of gases causing the eruptions? Do we gain any new understanding about volcanic eruptions from witnessing them on other moons or planets? Are there surprising results that do not fit with what is expected? Please provide a chapter on extra-terrestrial volcanic eruptions.
--Sally Seaver Shabaka72.74.241.10 (talk) 03:13, 15 July 2011 (UTC)
replies: text: Volcanism on Io is a Featured article. ResMar 03:10, 2 March 2012 (UTC)

text: That article should be labelled "Geologist's impression". The image should be titled as "an artists impression" as it is the ultimate in image manipulation. (Weatherlawyer not logged in)  — Preceding unsigned comment added by Weatherlawyer (talk • contribs) 22:35, 22 May 2016 (UTC)
thread_title: Other planets and moons

message: In the section on Submarine Eruptions there is the following sentence;
Eruptions near subducting zones, meanwhile, are driven by subducting plates that adds volatiles to the rising plate, raising its melting point.
I think it should be lowering instead of raising.
Apologies if I am wrong.
E E Leigh (talk) 16:00, 23 November 2011 (UTC)
replies: text: Changed it, thanks for noticing that. And I checked the reference to verify there wasn't some confusion in reading it - clear cut. Vsmith (talk) 16:22, 23 November 2011 (UTC)
thread_title:  Possible small error. 

message: What are the carbon dioxide emissions of volcanic eruptions? --41.150.174.58 (talk) 15:16, 13 March 2014 (UTC)
thread_title:  carbon dioxide emissions 

message: I would like to add an image to explain the different types of volcanoes and their respective eruption.
  — Preceding unsigned comment added by Chiaraci (talk • contribs) 21:05, 18 January 2015 (UTC)
thread_title:  add image 

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