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- 1 Basalt
- 2 Transitional alkalic basalts
- 3 Recent changes
- 4 Small usage fix
- 5 Extremely confusing
- 6 What about it's uses?
- 7 Basalts' Uses
- 8 Traprock
- 9 More data needed
- 10 Commom uses
- 11 Columnar Basalt and Trap Rock quite different
- 12 Hexagonal Columns
- 13 Hacked with Sex
- 14 Higher Resolution Image Available
- 15 Silica content
Basalt is an extrusive igneous rock, sometimes porphyritic, and is often both fine-grained and dense. Basalt in the tops of subaerial lava flows and cinders will often be highly vesiculated, imparting a lightweight "frothy" texture to the rock. The term basalt is often casually applied to shallow intrusive rocks with a composition typical of basalt, but rocks of this composition with a phaneritic groundmass should generally be referred to as gabbro. The crustal portions of oceanic tectonic plates are predominantly made of basalt. Frankly, I do not get a word of what it means. Thankfully I know what Basalt is.
There you go. Hopefully even oompa loompas can read it and know what it is now.Rolinator 09:12, 22 January 2006 (UTC)
Basalt (IPA: /ˈbæsɒlt, bəˈsɒlt/) is a common gray to black extrusive volcanic rock. It is usually fine-grained due to rapid cooling of lava on the Earth's surface. Basalt isn't extrusive. The word "Basalt" is based on the chemial composition and grainsize, not if it was formed on the surface or underground. It isn't usually fine-grained, by defintion it is fine-grained. If it was medium/coarse grained it would be a dolerite/gabbro.
Transitional alkalic basalts
Image:Volcanic system of Iceland-Map-en.svg Iceland: Lava from the Katla and the Hekla volcanic systems result in transitional alkalic basalts and the central volcanos ones result in tholeiitic basalts. Question: Is transitional alkalic basalts the same as high alumina basalt? Thx for an answer :) --Chris.urs-o (talk) 19:36, 2 April 2010 (UTC)
- Don't you just love scientific terminology. I had a look at this when the question was raised elsewhere (I can't remember either where that was or whether I got round to replying (apparently the answers are by you at Talk:Basalt and no)). From what I gathered, they were considered by some to be the same but not by everyone, which isn't very helpful. Transitional I take to mean transitional between tholeiitic and alkaline. High alumina basalt was a term introduced by Kuno, who interpreted them to be primary melts of mantle material at depths intermediate between those at which tholeiite and alk-basalt magmas were formed. Others have reckoned that they are more likely to be a result of differentiation of a primary magma at depth. Brody & Marsh reckon that they are primary melts, but of quartz-eclogite from the subducting slab - they also point out that it has been shown experimentally that the High-Al basalts can never have been in equilibrium with either an olivine-bearing magma or source rock. I think that this was where I gave up last time :-). This more recent note by Draper , does at least define High-Al basalts as aluminium rich tholeiites (which others would probably call transitional I'm guessing). I just found another ref that suggests that some HAB magmas originate by partial melting at the base of continental crust above a mantle upwelling in a rift setting (I have full text access for this one, unfortunately the abstract doesn't go into any detail). I'm not sure if any of this helps. Cheers, Mikenorton (talk) 11:43, 17 April 2010 (UTC)
This page has improved a lot in the last week. Looks good now.Rolinator 07:47, 3 November 2006 (UTC)
Small usage fix
Changed "comprised predominantly of basalt" to "composed predominantly of basalt." A thing is not comprised of its parts; a thing comprises its parts. 22.214.171.124 21:30, 28 March 2007 (UTC)Stephen Kosciesza
- Thanks for taking the time to justify your changes, it is appreciated by those of us who watchlist these articles. The Merriam-Webster Online Dictionary entry for "comprise" has a useful note on usage. Based on the note, it would appear that "comprised" is commonly used in this sense, although likely to be criticized as wrong by many (like you). I'm OK with using "comprise" that way, I see it all the time in scientific papers, but I'm happy to accept "composed" as more correct usage.
- By the way, you've been making many small but useful conrtributions to Wikipedia over the past months, might I recommend signing up for an acount? See WP:ACCOUNT for info on the numerous benefits of having an account. No pressure, it's up to you. Thanks. --Seattle Skier (talk) 23:01, 28 March 2007 (UTC)
Just a point that this article states that Boninite is usually found in back-arc basins. It should be FORE-ARC basins and it forms when the arc is closer to the subduction zone —Preceding unsigned comment added by 126.96.36.199 (talk) 11:16, 16 November 2010 (UTC)
I'm trying to do a project on basalt and I hardly know what's being said. Some of us are still in high school, you know. BlackSlivers 00:08, 20 June 2007 (UTC)
The following sentence seems awkard to me: Pliny used the word basalt and it is said to have had an Ethiopian origin, meaning a black stone. Even though Pliny has a link, the author uses the name as if anyone reading this article is sure to know who Pliny is and why he was important. I feel it should have had some kind of comment appended to it such as: Pliny, the world's oldest rock hound in the 1920's,................. I humbly submint this comment for peer review and suggest it only in the hope that it will make the article more easliy readabale. No malice was intended.188.8.131.52 04:53, 21 September 2007 (UTC)ID 2007-09-21
What about it's uses?
Don't get me wrong, I like to read about how the stone is formed. But I guess I feel like this article overlooks the practical uses of basalt as tile. I'd fix it myself, but I'm horrible at gathering information in an easy to read way. But it'd be nice to have a section about the various uses of basalt, as well as it's weaknesses/strengths as a material. —Preceding unsigned comment added by 184.108.40.206 (talk) 03:37, 18 September 2007 (UTC)
I also agree with the previous comment about the fact that the artical needs a section about the rocks' uses. I'm currently doing a project on Rocks for school & I've chosen Basalt as one of my subjects. I have been asked to find out about its formation, uses & where its found. However, I cant complete the 'uses' section because of this. I have tried looking for it over the internet & Im sure that it will take me ages to do! So please could you include a uses section in the future - thanks. - Mrsir2 —Preceding unsigned comment added by 220.127.116.11 (talk) 14:29, 6 October 2007 (UTC)
What is being said?
Basalt is an extrusive igneous rock -- this means that Basalt is one member of a class of objects. What distinguishes basalt from the other members of this class? Are no other rocks extrusive and igneous? I have no idea what is being said, and I am not in high school, I am merely a high school science teacher. Billt4 (talk) 01:33, 14 June 2008 (UTC) —Preceding unsigned comment added by Billt4 (talk • contribs) 21:29, 13 June 2008 (UTC)
More data needed
How about information on the rock, like (average) density (and comparison with that of granite, for example), and hardness. Average crystal sizes of various forms of basalt would be interesting.
I also would be highly interested in (human) uses of basalt. Again, comparison with stones with which most people are familiar (granite, marble) would be helpful.
ALSO -- I don't believe that the Columbia Basin Basalts extend to Yellowstone National Park as the picture indicates. The Columbia Basalts don't cross the Continental Divide. The pictures of columnar jointing are weak -- try using Google to find some nice shots from the Columbia Basin. Why not add photos of the Deccan Traps and Siberian Traps, too -- the three known places of fissure volcanism.
To answer questions -- average density? Denser than most rocks, including granite. Hardness -- comperable to Mohs? I'd guess an 8. Uses of Basalt? Try googling basalt waste isolation project. Or google "leverite" -- where you just "leave 'er right there." Many uses include aesthetics because of striking jointing. Just a run of the "mil" scientist here, so take very little for what it's worth.
Columnar Basalt and Trap Rock quite different
I, for one, would like to see an article for trap rock kept separate from basalt in general. For one, not all trap rock is basalt, let alone columnar basalt. Trap rock is manifest in three forms: basalt (which is usually extrusive), diabase (which is always intrusive), and hornfels (which can be formed at the surface or in an intrusive setting). Additionally, trap rock can exhibit any of the following qualities: stacked, jointed, or columnar.
In a nut shull, 'trap rock' is just another way of describing most blocky volcanic rocks. It has particular relevance to quarrying since trap rock in its varying forms is crushed to make road and railroad beds. lithium6ion (talk) 22:07, 9 August 2009 (UTC)
What is this line supposed to mean: "These structures are often erroneously described as being predominantly hexagonal. In reality, the mean number of sides of all the columns in such a structure is indeed six (by geometrical definition), but polygons with three to twelve or more sides can be observed" - does someone have a different definition of "predominantly" than I do? They're described as being predominantly hexagonal because most of them are hexagonal. Also, what's this about "the mean number [...] is indeed six (by geometrical definition)." How does 'geometrical definition' dictate that it has to be six? It could easily be four, or three. It's six because of the physical process and the physical properties of the material. 18.104.22.168 (talk) 02:44, 29 July 2012 (UTC)
Hacked with Sex
Something somewhere has been hacked to add the emboldened text to this page's entry. Don't have sufficient Wiki-Fu to do more than bring it to your attention. -- 22.214.171.124 (talk) 04:32, 4 October 2012 (UTC)
Basalt which erupts under open air (that is, subaerially) forms three distinct types of lava or volcanic deposits: scoria; ash or cinder (breccia); and lava flows and then whenever people go in there they get have burned and then when they are having sex its weaker sex.
- Odd as that was zapped within a minute of its addition by cluebot hours before your post. Vsmith (talk) 13:23, 4 October 2012 (UTC)
Higher Resolution Image Available
This image has come to my attention: http://people.sc.fsu.edu/~jburkardt/latex/ajou_2009_death_map/causeway2.png
If I can obtain permission from the photographer (which appears to be this Simon Ward) to use this image, should it be used here? (Asking as I am not sure whether this image is as appropriate as I think it is, and would like second opinions)
Ultimately I am seeking to see whether it would be suitable to replace the current image of Columnar Basalt, http://en.wikipedia.org/wiki/File:Giants_causeway_closeup.jpg.
- In my personal opinion images shouldn't be watermarked on Wikipedia. The author of the image gets all the credit when his image is viewed full screen or on Commons. Otherwise we might as well wait until the next Wikipedian visits that outcrop. --Tobias1984 (talk) 18:50, 6 May 2013 (UTC)
- Yes, good replacement choice, if, as others suggest, you can get him to submit it without the water mark. -126.96.36.199 (talk) 03:33, 7 May 2013 (UTC)
Could someone help me with this. At the beginning of the article it says that Basalt contains less than 20% Quartz.In the drop down menus at the foot of the page it says that Basalt is Mafic and has a 45 to 52% SiO2 content is this because the Si O2 in the Feldspar etc is included. — Preceding unsigned comment added by Ruskin (talk • contribs) 09:58, 9 June 2013 (UTC)
- One way of expressing the chemical composition of a rock is to list it as percentages of separate oxides. The difference that you noted is because the total SiO2 content of a basalt includes contributions from all the silicates, particularly feldspar, olivine, amphiboles and pyroxenes. Mikenorton (talk) 10:34, 9 June 2013 (UTC)
- Also the 20 % Quartz are volume (this example 20 cm³ / 100 cm³) and the 45 to 52 % SiO2 are mass (45 to 52 g / 100 g) --Tobias1984 (talk) 14:50, 9 June 2013 (UTC)