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Archive 1 (May 2004 to Feb 2006), Archive 2 (Feb 2006 to Dec 2008 |
Red Zone and Blue Zone
Adding to my previous entry, the Red Zone and Blue Zone also played a major role in keeping the death toll to a minimum. The Red Zone and Blue Zones were roughly ten-and-20 mile boundaries around the volcano (with exception to the northwest side, in wich the Red and Blue Zone bordered only three miles away from the summit, and both restricted zones weren't full complete "circles" as some thought), and were signed into order on April 30 by Dixy Lee Ray. The Red Zone was a restricted area closed to all persons except those in the scientific community, while the Blue Zone was a limited-access restricted area, which allowed approved persons in only on a day-to-day basis, and only during daylight hours.
Interestingly, of the 57 killed, only three were in the Red Zone. The remainder were both either within, or totally outside the Blue Zone entirely.Srosenow 98 (talk) 10:02, 18 January 2008 (UTC)
- When the danger area was set up no-one envisaged such a large blast. The only similar blast had occurred at Shiveluch inthe Soviet Union in the 1950's and information was rather limited.The Geologist (talk) 12:00, 11 April 2012 (UTC)
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- Source: Up From the Ashes. 60 Minutes. VHS. (C) 1990 Fisher Broadcasting Inc., KOMO-
- The "Source" note was part of Srosenow's preceding post, yes? (Otherwise, since the signature precedes it, it almost looks as though the note was added by the author of the following paragraph.) Memetics (talk) 07:20, 20 August 2009 (UTC)
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The american goverment set a 25 mile radious and anyone who lived in that radious were evacuated from there homes to be protected from the eruption but one person who refused to leave was Harry Trumen who was 84 years old and had lived in his house for 50 years and that is why he would not leave —Preceding unsigned comment added by 86.163.147.223 (talk • contribs) 11:04, 3 November 2008 (UTC)
- What is a radious?? - I assume you mean RADIUS. Harry Truman refused to leave and is on record as saying that he didn't believe that MSH was dangerous. One of his sayings was "I know that mountain and that mountain knows me. That mountain will sure never hurt me." He died, like the others who died because they refused to accept what scientist were telling them, preferring to believe pseudo-scientists who claimed they knew better. The same pseudo-scientists told the good citizens of Montserrat that the volcano was harmless and it was safe to enter the danger area. Many people died when a pyroclastic surge overflowed the Tar Valley and engulfed them. When a volcanologist says a volcano is dangerous there is a good reason for saying so and you ignore the safety limits at your own risk.The Geologist (talk) 12:00, 11 April 2012 (UTC)
Carbon contribution?
I came looking for info on how much carbon Helens has been releasing with it's new activity. I ended up googling since nothing was here, one newspaper reported between 500-1000 tons a day (as compared to a typical US family contributing 50 tons a year). That's the amount of 5,000 families... Is there some hard reference that could be added? -RJFerret 03:01, 17 July 2006 (UTC)
- No -- 12.116.162.162 21:05, 23 August 2007 (UTC)
- Could you provide a link to the article you alluded to? I think it may have been referring to tons of total material, not carbon / greenhouse gases, being ejected during that eruption. (During a lecture in fall 2006, I recall the geology instructor at Lower Columbia College in Longview saying that the eruption was releasing about a cubic meter of material every second. Anyone care to convert that figure to British tons per day?) Memetics (talk) 06:58, 20 August 2009 (UTC)
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- 500 to 1000 tons of CO2 is not unknown at active volcanoes. At standard temperature and pressure, the density of carbon dioxide is around 1.98 kg/m3, about 1.5 times that of air. At atmospheric pressure and a temperature of −78.51 °C (−109.32 °F), carbon dioxide changes directly from a solid phase to a gaseous phase through sublimation, or from gaseous to solid through deposition. See the wikipedia pages about #REDIRECT Carbon Dioxide To answer the question based upon this information of a density of 1.98 kg/m3, this equates to 118.8 kg per minute, 7128 kg per hour and 171072 kg per day (171 metric tonnes). 1 kg = 2.24 pounds so in a day this volcano is releasing about 383,000 pounds which equates to about 171 tons - note the metric tonne and the imperial ton are very similar in mass. However to arrive a the total volume and thereby the total mass emitted per day we need to know the total area that is releasing the gas. A 10 x 10 m area will therefore be releasing 17107200 kg or 17107 metric tonnes 17107 imperial tons daily.The Geologist (talk) 11:53, 11 April 2012 (UTC)
Coordinates
{{geodata-check}}
Please note that the coordinates in this article need fixing as:
THE COORDINATE IS 48 DEGREES WHICH I SEEN IN ANOTHER WEBSITE
- The other website appears to be incorrect.[1] Walter Siegmund (talk) 22:53, 14 January 2009 (UTC)
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- These are the correct co-ordinates: 46° 12' (46.2°) North, 122° 11' (122.183°) West.The Geologist (talk) 11:33, 11 April 2012 (UTC) Try using a calibrated GPS or better still a real DGPS - Differential GPS receiver.The Geologist (talk) 11:33, 11 April 2012 (UTC)
Incorrect: Mount St. Helens the day before the 1980 eruption, which removed much of the northern face of the mountain, leaving a large crater (caldera).
It is not a caldera, just a volcanic crater. A caldera is a collapsed volcano. —Preceding unsigned comment added by Ddrmaxgt37 (talk • contribs) 18:45, 17 February 2009 (UTC)
- Actually IF you read "Williams, 1943 - Calderas," you will discover that NOT all calderas form by collapse, some create ampitheatre calderas and the MSH explosion produced such a caldera - an ampitheatre caldera.The Geologist (talk) 11:24, 11 April 2012 (UTC)
Very little info on sulphur dioxide
There seems to be very little in the article about the amount of sulphur dioxide produced by Mount St. Helens. —Preceding unsigned comment added by 81.158.207.21 (talk) 09:45, 25 March 2009 (UTC)
- That's probably because there was not a lot known about emissions of gases at that time. MSH taught us volcanologists a lot which we had not known before the explosion and it wasn't just gases that we knew little about.The Geologist (talk) 12:01, 11 April 2012 (UTC)
correct pronunciation of Mt. St. Helena?
correct pronunciation of Mt. St. Helena? —Preceding unsigned comment added by 68.105.10.184 (talk) 17:29, 27 March 2009 (UTC)
- The correct pronunciation of Mount Saint Helens is MOUNT SAINT HELENS. Saint Helena is an ISLAND in the Atlantic Ocean which is where Napoleon was imprisoned. Mount Saint Helena is in California and the "Helena" is usually pronounced "He-lay-na." Well my wife says that is how her grandmother who was Russian BTW pronounced it.The Geologist (talk) 13:02, 12 April 2012 (UTC)
Johnston quote
"Johnston uttered his famous last words" seems ambiguous. Would seem more accurate to say "Johnston radioed his famous last words", based on the content of the article cited for the info. Memetics (talk) 05:22, 20 August 2009 (UTC)
- David Johnson SPOKE his last known words when he transmitted them over the radio.The Geologist (talk) 11:24, 11 April 2012 (UTC)
mount helen
how did mount helen fom? —Preceding unsigned comment added by 68.204.217.169 (talk) 23:27, 10 October 2009 (UTC)
- Check out the geology section in the article. --mav (please help review urgent FAC and FARs) 19:30, 20 December 2009 (UTC)
- Mount St Helens is what's called a fold mountain. This is formed when two tectonic plates move towards each other and fold up. —Preceding unsigned comment added by 213.246.114.2 (talk) 17:12, 15 February 2011 (UTC)
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- MSH IS NOT a fold mountain it is an active albeit at times dormant volcano. It sits on top of sediments but MSH is definitely not a tectonic feature - which a fold mountain is, but rather the result of the same process that created the fold mountains upon which it sits.The Geologist (talk) 11:24, 11 April 2012 (UTC)
Coordinate error
{{geodata-check}}
The coordinates need the following fixes:
- Write here 12n 45w
96.240.215.55 (talk) 02:26, 8 March 2010 (UTC)
- I've checked the coordinates, and they're correct as they stand. The ones you suggest are in the middle of the Atlantic Ocean. Deor (talk) 19:17, 8 March 2010 (UTC)
Edit request
{{editsemiprotected}} In the "360-degree panorama," the picture is actually only a "180-degree panorama' as the entire mountain is visible as the photographer positioned along the southern rim. If this were a 360-degree panorama, half the photo would be filled with the rolling hills to the South and you'd see Oregon to the South, etc. Mortonjhop (talk) 18:51, 27 March 2010 (UTC)
- As far as I can tell, this is a true 360 degree image. The right hand end of the picture matches up with the left hand end (pretty much perfectly). Note that the lakes referred to at the right hand end of the image, lie south of the mountain. Mikenorton (talk) 19:16, 27 March 2010 (UTC)
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- It seems 360 to me too. But, if consensus shows otherwise, someone else can do the edit for you or you can request an edit again. --JokerXtreme (talk) 19:38, 27 March 2010 (UTC)
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- It appears to be a full (or very close to a full) 360 to me as well - at the very least it's clearly much more than the 180 claimed in the edit request. Any aparent inconsistency on each end can easilly be attributed to artifacts from the stitching of multiple images.
- To get some clarification, I've requested that Farwestern (talk · contribs) - who uploaded the image - to provide feedback/clarification on the image. --- Barek (talk • contribs) - 19:55, 28 March 2010 (UTC)
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also, can some one enter what was learned after the eruption?
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- The details of the photo says it is 360°, the photo poster says s/he often shoots 360° photos, and it has survived commons Featured Photo review with that description—no small feat. Besides it looks 360° to me too (Mount Hood at 80% from left edge; Mount Jefferson, 88% (with the Three Sisters just to its left); Mount Rainier, 50%; Mount Olympus, 25%; possibly Saddle Mountain, 15%; and all the lakes around the south side. The split appears to be approximately WSW. —EncMstr (talk) 20:28, 28 March 2010 (UTC)
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- Yes, it really is a true 360. To help clarify this point I have created a map on google that identifies various notable landmarks in the image. http://maps.google.com/maps/ms?hl=en&client=firefox-a&ie=UTF8&msa=0&msid=116803011662351216901.000482fdf07a6e4870a4d&ll=46.191358,-122.184277&spn=0.027034,0.075102&t=p&z=14 I hope this helps --Farwestern (talk) 06:41, 30 March 2010 (UTC)
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- "I hope this helps". May help to point out how close to the crater you were standing when you took the picture. I am guessing the crater would normally fill a person's vision from where you were standing, when looking at its center. It looks "normal" in the photo, which may be what is throwing off people's perception. —Preceding unsigned comment added by 72.102.189.120 (talk) 02:27, 28 July 2010 (UTC)
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The image is not a 360°. The right side of the image does not match the left side - look at the snow patterns, also the crater opening would appear wider than it does. It is at most a 180° panorama looking northwards - the clue is the crater opening.The Geologist (talk) 12:22, 12 April 2012 (UTC)
Who walked out with a video camera?
There was a man on the south side of the mountain when it erupted, who managed to find his way to safety through nearly complete darkness from the ash blocking the sun. He had a portable video camera (which 30 years ago was barely carryable by one person) and recorded his ordeal. I remember seeing part of it on TV once.
- Dave Crockett -- see [2] and [3]. — Myasuda (talk) 02:14, 23 April 2010 (UTC)
- There's a very short bit on him in When Yellowstone Erupts but no mention of his name or any other details. Bizzybody (talk) 07:13, 1 September 2010 (UTC)
Bigfoot stuff
I've removed the addition of "bigfoot" to the "Exploration by Europeans" as it was not supported by the references given and was rather out of place. Vsmith (talk) 13:40, 18 July 2010 (UTC)
Ecological recovery
Have been up to St. Helens several times in the past few months and am amazed by the devastation some of the land still exhibits after 30 years. The only "recovery" of note that I can see are where trees were planted by the lumber companies around the edges of the park. Anyone interested in adding a section talking about this? Cannot provide the scientific expertise to discuss this, but can take photos. The one of Johnston Ridge does not convey the moonscape still present in parts of the park. 72.102.189.120 (talk) 02:35, 28 July 2010 (UTC)Bill
- Photographs that you take yourself are welcome. It is easiest if you create an account but it is possible to proceed without an account also. Please see Wikipedia:Files for upload. Consider uploading to Wikimedia Commons where they can be used by Wikipedias in other languages. Walter Siegmund (talk) 04:03, 28 July 2010 (UTC)
ə́Raúl Julian de Pedro Martinez de æAndino ɐMontes Urrutiaɪ̈ɔ̹ —Preceding unsigned comment added by 70.45.44.232 (talk) 23:26, 27 September 2010 (UTC)
which two plates collided?
north american plate and the eurasian plate —Preceding unsigned comment added by 196.201.16.210 (talk) 10:32, 21 October 2010 (UTC)
- North American Plate and Juan de Fuca Plate, as shown on the map in the article. Mikenorton (talk) 10:36, 21 October 2010 (UTC)
Contradiction
Here its written that MSH is a Stratovolcano but in the entry "lava dome" its written that its a lava dome. someone know what's right? maybe both? המתלמד (talk) 15:55, 9 December 2010 (UTC)
- No MSH IS a stratovolcano also known as a "Composite volcano" because it is composed of layers of ash, pyroclastics and lavas. The lava dome is currently growing inside the ampitheatre caldera that formed as a result of the 18th May explosion.The Geologist (talk) 11:24, 11 April 2012 (UTC)
Different earthquakes cause 1980explosion/eruption?
In the 1rst paragraph u said an 5.0 earthquake on the richter scale triggered the earthquake but then later u said it was a 5.1 —Preceding unsigned comment added by 168.150.169.66 (talk) 00:41, 25 March 2011 (UTC)
- Thanks for spotting that, I've changed the 5.0 to 5.1 in the lede, because that matches the sources. Mikenorton (talk) 07:13, 25 March 2011 (UTC)
Mushroom cloud picture
I think this picture would be a useful addition to the article. It shows the full profile of the initial mushroom cloud. Within a couple of months I may be able to upload a high resolution version made from a dozen different negatives stitched seamlessly together. This crude version is all I have for now. (Another composite from these same negatives was printed in a National Geographic book in the 1980s.) The photographer has agreed to make the negatives available for reprocessing with modern digital technology. It should make a spectatular image; in the meantime this low-resolution image is uniquely informative. HowardMorland (talk) 02:59, 3 May 2011 (UTC)
- Gorgeous photo! I absolutely agree. Awickert (talk) 03:21, 3 May 2011 (UTC)
- Holy moly. Pfly (talk) 04:30, 3 May 2011 (UTC)
- I added the picture to the article. HowardMorland (talk) 17:16, 10 May 2011 (UTC)
- Holy moly. Pfly (talk) 04:30, 3 May 2011 (UTC)
Amazing!KF5LLG (talk) 12:25, 6 December 2011 (UTC)
Graphic clutter
I think the overall appearance of this article is becoming degraded by too many images. Granted many if not most are important to the text but things are getting crowded. I'm to cowardly to be the one too choose which should stay and with should go but I hope someone has the guts. –droll [chat] 18:01, 10 May 2011 (UTC)
Edit request from Durahan26, 10 August 2011
Under "Modern eruptive period" you have the following sentence. "The removal of the north side of the mountain reduced St. Helens' height by about 1,300 feet (400 m) and left a crater one to 2 miles (3.2 km) wide and 0.5 miles (800 m) deep, with its north end open in a huge breach. The eruption killed 57 people, nearly 7,000 big game animals (deer, elk, and bear), and an estimated 12 million fish from a hatchery.[7]" Please change the "and left a crater one to 2 miles (3.2 km) wide" to "and left a crater 1 to 2 miles (3.2 km) wide". Might as well keep things consistent and use the number "1" instead of the letters "one." Thanks. Durahan26 (talk) 05:16, 10 August 2011 (UTC)
- Done Now is left a crater 1 mile (1.6 km) to 2 miles (3.2 km) wide --Jnorton7558 (talk) 05:25, 10 August 2011 (UTC)
Cause of earthquake
The intro text says "The earthquake was caused by a sudden surge of magma from the Earth's mantle.[3]". However, the archived reference table does not address this particular issue. How sure are we of this? I would have thought a fault movement would be the most likely cause. Anyway, the article does need a reference which deals with this question. Macdonald-ross (talk) 09:46, 15 December 2011 (UTC)
- You're right, that's not supported by source #3. I've moved the citation to the end of the previous sentence, which it's fine for, and added a 'citation needed' tag after the 'sudden surge of magma' sentence. I've had a good look around for a reference that gives this as the origin, but I've failed to find any. Mikenorton (talk) 17:33, 15 December 2011 (UTC)
- I have no information regarding a fault. The USGS and other volcanologists are of the opinion that the earthquake was caused by magma moving under the volcano, which could be also have been due to gases causing an over-pressure. This shook the volcano, causing the northern flank to fail along a developing failure plane releasing the over-pressure on the meteoric water which were also super-heated and these flashed into steam causing the lateral blast which in turn released the pressure on the magma reservoir (we tend to talk about reservoirs rather than a chamber because a chamber is either enclosed or only has one entry/exit point where as a reservoir has an independent entry point and a separate exit point), and this caused the plinian eruption. Incidentally for those in the USA the world uses Universal Co-ordinated Time - UTC and scientists use that not local time. This eruption occurred at 15:32 hrs UTC (08:32 PDT or LOCAL time).The Geologist (talk) 11:24, 11 April 2012 (UTC)
broken image link
The following link at the top of the "human history" section is broken:
Does anyone know how to fix it? Thanks.DavidRF (talk) 20:46, 28 December 2011 (UTC)