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Might want to put a reference toValvasor into the history as well.(17th century)

From the wiki page:Valvasor was a pioneer of study of karst phenomena. Upon the proposal of Edmond Halley, who was not only an astronomer but also a geophysicist, and in 1687 his extensive treatise on the hydrology of the intermittent Lake Cerknica won him a Fellowship of the Royal Society.—Precedingunsigned comment added by89.143.14.254 (talk)11:10, 17 May 2011 (UTC)[reply]

I'm not actually sure if the region in the specific sense extends south from Slovenia. Thekrš in general certainly does, butKras? --Shallot 15:46, 26 Apr 2004 (UTC)

I uploaded some pictures from Italian Karst intoCommons:Category:Karst--Alex brollo05:49, 14 December 2005 (UTC)[reply]

Not terribly knowledgeable about Karsts myself. I live in Cambodia, where we have many "tower karsts" throughout the southern part of the country. This article, however, largely only refers to the karst formations found in mid-latitude regions, and not to tower karsts and their formation (which you find only in Tropical zones I believe).

ANy experts out there want to try updating with information tower karsts?

• Have slightly revised text to be a little more encompassing, but no one region really is featured. Perhaps the entire article needs expansion with sections on tropical karst, alpine karst, etc...?Ian mckenzie20:50, 14 September 2006 (UTC)[reply]

There are topographic features that result from the development of karst, but anything below ground is out of the domain of "topography". If explainations of karst formations and caves are to be given, I reckon the page be moved tokarst. Cheers,Daniel Collins16:14, 20 March 2006 (UTC).[reply]

I agree, this article covers more than just the topography but also details about formation, features, and dangers within karst areas. good thought! GEO310LindseyGEO310Lindsey (talk)18:30, 7 October 2010 (UTC)[reply]

Isn't the Nullarbor Plain in Australia Karst? It is the worlds biggest hunk of limestone!It also has a lot of limestone caves.

I thought I'd ask here first rather than just putting possibly inaccurate information into the article.

I've done some revising and rewriting, but more is needed. I took out some stuff that is more thoroughly examined elsewhere (incaves andspeleothems, for example). Not sure whether explanations of karst pavement, clint/grike etc is appropriate here, or if separate pages for each makes more sense...Ian mckenzie22:54, 13 September 2006 (UTC)[reply]

67.180.143.138, I've reverted your alterations back to the original, as your version put inordinate attention on pronouncing the Chinese word rather than the simple point that other languages have different terms for karst. Also, as this is an English site, it is relevant to point out that there is no equivalent word in English, as a prelude to the next sentence (the international usage of the German term). BTW, I took the spelling of the word 'yienjung' fromKarst in China, an English language book published by the Chinese Academy of Geological Sciences in 1976.Ian mckenzie18:03, 8 December 2006 (UTC)[reply]

According to the Australian Wilderness Society, the Nullarbor Plain is indeed the world's largest Karst Landscape. I would suggest that perhaps whoever edits the information should add this information into the wiki.—The precedingunsigned comment was added by203.161.90.95 (talk)17:19, 25 February 2007 (UTC).[reply]

Does theChalk stream belong in this topographical classification?Verne Equinox18:42, 15 April 2007 (UTC)[reply]

Someone needs to find published material which states whether it belongs. --SEWilco (talk)15:51, 3 January 2008 (UTC)[reply]

I would appreciate information on the dynamics of the hydrological systems in caves and tunnels, and on such dramatical events as the onset of the rainy season in, say, Guatemala, the sudden increase of the water flow, the visibility and audibility of the subterranean changes above, on the surface, etc.77.162.130.13917:40, 19 June 2007 (UTC)[reply]

I have removed the Gibraltar reference and excellent photograph, as a "monolithic limestone promontory" is not in itself a karst feature.Ian mckenzie03:55, 9 July 2007 (UTC)[reply]

I have removed the statement that underground drainage isthe 'defining characteristic' of karst landscapes. Although obviously very common, I have not read anywhere that this is essential to the definition. There are lots of recently-deglaciated limestones that exhibit surficial karst where underground drainage is unknown, unproven, or simply not present. In fact, one might argue that cavernous areas where surface karst is not evident isnot a karst landscape.Ian mckenzie (talk)18:43, 2 January 2008 (UTC)[reply]

Karstified geological formations do require internal drainage. The drainage channels however can be very small and do not need to be human-explorable caves. For karst landscapes, I would agree that recently exposed rocks can have surface dissolution features (ie rillen karren) but that is not an adequate definition for the landscape to be considered karstified.

I am wondering if some coordinated reorganization of this entry would clarify the global relationship between:- 'karst' from a PROCESS based geomorphological understanding which does implicitly require increased permeability by dissolution opening up internal drainage channels (which can be mm in diameter and therefore not necessarily human enterable caves. - 'karst topography' based on observation of individual FEATURES independent of how they formed, or what they will form into. In this case, karst topography could only include unconfined geological settings, and/or landscapes with surface dissolution features even though below the surface there might not be any existing or potential for internal drainage.

The issue with feature based definitions is that multiple processes can give rise to morphometrically indistinguishable features, there is no consideration of landscape evolution, and in the absence of observation of the feature then there is a misclassification. Two good examples of why feature based definitions are not defensible are: a very large area over Mammoth Cave in Kentucky has no karst topography, and therefore would not be karst despite the cave underneath ( a false negative classification); lava tubes are cave like holes and therefore are karst even though they form by categorically distinct hydrogeochemical processes (a false positive classification). We do however call lava tubes pseudo-karst because they can function as hydrogeological conduits, and their internal climate and biology can be broadly parallel.

I suggest that a re-organization of the entry on karst might be able to provide a clear process based definition of karst, but also do justice to the role of karst landscapes and surface features. Opinion? Ideas? Feedback? It would be really nice to have some discussion on this since I suspect there are a large number of karst and cave loving Wikipedians. I will confess that I am relative new to Wikipedia and so I hope this is the right place to get a discussion going. Cheers. Trish BeddowsGgpab (talk)01:53, 3 January 2008 (UTC)[reply]

• Hi Trish; fancy meeting you here! Not sure I'd agree that rillen karren on its own is not 'karst topography'. But, this can be resolved simply by including a credible citation or two for the notion that there must be underground drainage in order for topography to be 'karst'. Or, simply remove (as I have) the word 'definitive' if there's no such citation available.Ian mckenzie (talk)05:08, 3 January 2008 (UTC)[reply]

• We don't create definitions, we report what the definitions are. Find sources which define karst. --SEWilco (talk)15:47, 3 January 2008 (UTC)[reply]

I have reverted the thumbnail resizing by Attilios, because I felt it detracted from the article... but am willing to be corrected if in fact there is a 'standard' size that (s)he is trying to adhere to.Ian mckenzie (talk)03:12, 6 January 2008 (UTC)[reply]

If my addition of "List of notable pseudokarst areas" is OK, I think it would be better to group the general karst discussion with the "List of notable karst areas" and move the "Pseudokarst" area down below that, grouping it with it's list of notable areas.JulianDave (talk)19:21, 20 February 2008 (UTC)[reply]

Disappearing streams anddisappearing valleys (among other red-links) need to be mentioned.--Ace Telephone (talk)05:55, 29 February 2008 (UTC)[reply]

There is a karst area inTuhala, Estonia. I've added it to the link and can fix pictures if anyone wanna fix a stub/article.CarlJohanSveningsson (talk)—Precedingcomment was added at16:54, 9 June 2008 (UTC)[reply]

Related to the section#Grouping karst and pseudokarst above, I think that the lists in this article should be separated and given their own article(s). Given that there are countless regions in the world that can be considered notable karst areas, the list could get big enough to swamp the article and detract from its content; in fact I think it's already gone so far as to do this.

Would anyone have any objections to the creation of a separateList of karst regions andList of pseudokarst regions? Or should the list of pseudokarts regions be included as an additional heading on the list of karst regions page?Fattonyni (talk)13:41, 4 May 2009 (UTC)[reply]

I think that is a good idea. Lists of areas will only become more unmanageable.JulianDave (talk)23:18, 1 June 2009 (UTC)[reply]

I think that one of the photographs in the leading paragraph should be of the original Slovene/Triestine Karst (well not exactly original but original in the sense that this is where the term originates). The Karst/Kras/Carso is one of the defining features of western Slovenia and Trieste and maybe its importance should be highlighted.—Precedingunsigned comment added by217.203.146.154 (talk)23:21, 12 August 2009 (UTC)[reply]

Given the WV page (http://en.wikipedia.org/wiki/West_Virginia) says it is one of the most karistic areas in the world, shouldn't there be some mention of it here?

20:55, 7 January 2012 (UTC)Matt— Precedingunsigned comment added by173.255.161.106 (talk)

This chinese terminology appears to be quite common, particularly when describing karsts in the tropical zone. Is there a reason why the terms are not mentioned in the article?Mikenorton (talk)17:20, 26 February 2012 (UTC)[reply]

So, did UT Austin give Wikipedia permission to copy the first paragraph on this page verbatim from their website, or does that kind of plagiarism just go unnoticed here in the land where anyone can edit?— Precedingunsigned comment added by50.183.5.202 (talk)21:59, 19 June 2014 (UTC)[reply]

It's not a verbatim quote, but a close paraphrase. And, ironically, the UT document is itself a close paraphrase of the American Geological Institute'sGlossary of Geology. What this says is not that the world is full of plagiarists, but that there is fair agreement on the short definition of karst, and there's only so many slight variations of how that short definition is expressed. --Kent G. Budge (talk)04:55, 26 December 2020 (UTC)[reply]

According to[1] there are karsts on Titan. This might do for some section about off-Earth formations --70.51.203.69 (talk)07:37, 21 June 2015 (UTC)[reply]

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I just read through the document cited for the statement that 50% of hydrocarbon reservoirs are karsts, and it does indeed contain that statement, but the statement simply isn't true and is not footnoted in the document cited. I'm not sure what to do with the sentence in the article...

• The peer reviewed paper"Petroleum geological features and exploration prospect of deep marine carbonate rocks in China onshore: A further discussion" ([2]) states that "Marine carbonate reservoirs take a dominant position in the world oil and gas production. According to the statistics of IHS in 2000, marine carbonate hydrocarbon resources account for about 70% of the total in the world, and the proved recoverable oil and gas reserves account for 50% of the total. In 2011, the oil and gas output of marine carbonate reservoirs accounted for about 63% of the total oil and gas output of the world.", so the 50% figure seems to have some relevance, but refers to carbonate deposits rather carbonate topography.Langcliffe (talk)20:18, 11 July 2018 (UTC)[reply]

Agreed. The source says only that 50% of reservoirs are in carbonate rocks and that "much" is trapped in karstic porosity -- a very different statement from what appears in the lead. Modifying accordingly. --Kent G. Budge (talk)05:26, 26 December 2020 (UTC)[reply]

I hope this is in the right place. As a non expert reader there are references in this article that in my opinion made it unnecessarily difficult to read. They mainly discuss southern slavic linguistic and research history topics and highlight their importance, making etymological claims that seem at a short glance to be not substantially backed by sources. I can imagine that, like in many fields of research, it should be appreciated when somebody brings in overlooked research and synthesises formerly disconnected knowledge (between different research traditions for example...) but I feel like it is slightly off topic in several places throughout the article and maybe should get its own article or be moved to the end of the article2A02:120B:C3DC:7480:1D11:81D9:92CA:2C20 (talk)03:45, 5 June 2021 (UTC)[reply]

I've flagged this section, since it seems inappropriate on two counts. First, as noted in the improvement flag, it lacks worldwide perspective, since the list is restricted to North America. Second, karst aquifers are not uncommon, and a complete listing of such aquifers worldwide would be lengthy and put undue weight on this particular aspect of karsts. I'm not against a separate list article of karst aquifers, but only if it is expanded to a worldwide list.

However, I thought I should look for consensus here before completely removing this section. --Kent G. Budge (talk)15:41, 8 October 2021 (UTC)[reply]

• I agree that this section is inappropriate in this article for the reasons that you have given. I can, however, see it as a separate article. If people then want to develop such articles for the country of their choice, fair enough. I don't think that I could be arsed to do one for the UK, though.Langcliffe (talk)

  I boldly added the section. You both have given sound rational for removing it and I agree.--John Cline (talk)20:32, 8 October 2021 (UTC)[reply]

Kent, I agree with your comments.GeoWriter (talk)20:59, 8 October 2021 (UTC)[reply]

John, I encourage you to mention two or three of the best examples of karst aquifers in the article text, if they aren't already. And I really don't object to a list article on karst aquifers -- list articles can be useful collections of information. --Kent G. Budge (talk)23:47, 8 October 2021 (UTC)[reply]

Thank you Kent, I'll look at the hydrology section and see where a good mention may fit. I agree with you that ultimately a well developed list is the best way to fit this information into Wikipedia. I will work to that end soon. I want you to know that I appreciate the collegiality demonstrated in your manner. I look forward to future collaboration and wish you the very best.--John Cline (talk)07:20, 9 October 2021 (UTC)[reply]

The article needs a section on geography: where on the Earth are karst topographies found? I have read that China has more than the rest of the world combined; this is one of the things that could appear in such a section.Zaslav (talk)21:11, 28 January 2023 (UTC)[reply]

There is a section on Karst Areas which lists some karst areas including "The South China Karst in the provinces of Guizhou, Guangxi, and Yunnan provinces is a UNESCO World Heritage Site." It also providesa a link to alist of karst areas.Langcliffe (talk)21:35, 28 January 2023 (UTC)[reply]

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