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Communication

Water in Descriptions of Global Geoparks: Not Less Important than Geology?

by
Dmitry A. Ruban
1,2
1
K.G. Razumovsky Moscow State University of Technologies and Management (the First Cossack University), Zemlyanoy Val 73, Moscow 109004, Russia
2
Southern Federal University, 23-ja linija Street 43, Rostov-on-Don 344019, Russia
Water 2019, 11(9), 1866; https://doi.org/10.3390/w11091866
Submission received: 19 August 2019 / Revised: 3 September 2019 / Accepted: 6 September 2019 / Published: 8 September 2019
(This article belongs to the Section Water Resources Management, Policy and Governance)

Abstract

:
Water is an important landscape element of protected areas, but its significance to geoparks (parks representing geological heritage) is still unclear. The content of the official, standardized descriptions of the UNESCO global geoparks (144 in total) was analyzed in order to understand the consideration of water by geopark creators/managers. It was found that water objects (seas/oceans, rivers, and lakes are most common) are mentioned in 55% of these descriptions, and 47% of the latter bear photos of water objects. Moreover, water is generally strongly related to geological heritage (in 80% of cases). These findings imply a significant attention to hydrodiversity in geoparks (apparently, official descriptions reflect global geopark practice and intentions). This attention does not differ between Europe, Southeast Asia, and Latin America. It has increased in the 2010s relatively to the 2000s. The registered consideration of water in geoparks can be explained differently, and one plausible hypothesis links it to an increasing willingness of geopark creators/managers to demonstrate the natural integrity of geological heritage landscapes. Such attention to water is suitable to deliver the knowledge of this integrity to tourists, but it increases the risks of visitor distraction from geological heritage, shifting to easy-to-understand and beautiful water objects.

Graphical Abstract

1. Introduction

In many protected areas such as national parks and biosphere reserves, water objects are of special importance. On the one hand, they sustain unique ecosystems that require conservation [1,2] and on the other hand, they add aesthetic value to landscapes attracting visitors and, thus, facilitating tourism [3]. Moreover, water resources are essential to the functioning of protected areas [4,5,6]. This evidence is related to traditional, ‘all-inclusive’ protected areas aimed at conservation and recreational use of landscapes and ecosystems. A new type of nature-based establishment has appeared recently, namely the geopark. Geoparks are areas of different size (from very small to almost country-scale) bearing unique geological features (geological heritage) that need efficient conservation and permitting development of scientific, educational, and tourism activities. The idea of geoparks is explained, particularly, in the works of Farsani et al. [7,8] Henriques and Brilha [9], Jones [10], Lazzari and Aloia [11], Mc Keever and Zouros [12], Nikolova and Sinnyovsky [13], Ruban [14], Ruban and Yashalova [15], and Stoffelen [16]. Geoparks are not protected areas sensu stricto because geological heritage serves more to exploitation than to conservation there, however balancing these activities and the contribution to local sustainable development are cornerstones of each geopark. Thus, many (if not all) geoparks can be considered as protected areas de facto.
The most important geoparks representing geological features of global uniqueness are members of the UNESCO Global Geoparks network, which includes about 150 geoparks in dozens of countries and is continuing to gain importance. The international growth of the geopark movement has posed new questions. First, geoparks often occupy territories where non-geological elements of nature (soils, water bodies, endangered species, ecosystems, etc.) also occur, and these are very often of heritage value. On the one hand, their consideration is necessary to diversify conservation and recreation activities in geoparks while on the other hand, these ‘auxiliary’ natural elements have to be protected from excessive exploitation of geological heritage resource. For instance, water resources have become the subject of analysis in the Langkawi geopark in Malaysia [17], the Majella geopark in Italy [18], and the Luoping Biota geopark in China [19]. More generally, it is possible to state that geoparks represent geological heritage landscapes (sensu [20]), i.e., landscapes dominated by unique geological features, but not restricted to them. Undoubtedly, water is a very important element of geopark landscapes, and the societal impact of these establishments (Figure 1) can be also referred to it. Geoparks are essentially social projects linked to sustainable development, and water is a vital resource of the latter. Tourist activities in geoparks may lead to significant depletion or pollution of water. Finally, water can be related to geology directly (e.g., river incision with canyon formation, tufa deposits of waterfalls, salt deposition in hyper-saline lakes, etc.).
The role of water in geoparks has been considered occasionally in previous works (e.g., [17,18,19]), but evidence is scarce, often local, and remains dispersed in the literature. Undoubtedly, the noted issue is very important and needs careful investigation. The objective of the present paper is to provide the first analysis of water consideration in official descriptions of all UNESCO global geoparks. The other geopark networks (e.g., the European network) and lower-status geoparks (e.g., national) are not considered because of limited and often incomplete knowledge of them. In this study, attention is paid to how water is treated by geopark creators/managers. Indeed, water bodies can be found in many such establishments and their importance is indisputable, but it is of crucial importance to understand how significant these are thought to be. In other words, this study focuses on managerial opinions, which may or may not reflect the true relevance of water to geological heritage.

2. Materials and Methods

The object of analysis is the entity of official descriptions of the UNESCO global geoparks [21]. These descriptions are generally standardized and reflect the state of a given geopark, its main geological and other natural features, and societal context. Their utility to various analyses has been proven by previous studies [14,15]. Particularly, such descriptions permit the understanding of how geopark resources and peculiarities are treated by their creators/managers, how these are ranked, and how these are promoted. In other words, these descriptions clarify the concept of each given geopark, its functioning, and intentions. For instance, if water is included in such a description, this means that its relevance to the geopark purpose is well-understood and well-accepted. Undoubtedly, not in all cases is water thought to be so important if even available and unique. It should be added that the presence of water can be guessed on the basis of a given official geopark description (e.g., when island is mentioned). However, this is impossible in some cases, and, thus, to avoid biased interpretation of the water landscape, only direct consideration of water objects is taken into account. Missing any important information is recompensed significantly by the above-mentioned analysis of photos. For instance, sea is often well-visible on photos in the case of islands, and, thus, water objects are considered anyway.
This study is based on the content analysis of the official global geopark descriptions. Each geopark description is checked in order to find the information about water objects (= water bodies). Although such objects often overlap with geomorphological features, the latter are understood as landforms and not considered in the present analysis. The very presence of water itself is registered. For instance, if the word “river” or “lake” is found in the description, this means it is considered a water object. Three main, objective parameters are recorded, namely type of water objects (seas, rivers, lakes, waterfalls, etc.), relevance of these objects to geological heritage (Table 1), and presence of water objects on photos included in descriptions (some descriptions are provided without photos). This information is then summarized. The type of water objects can be easily detected by words used in the description. Fortunately, complexities of water body definitions do not affect the available descriptions. This means their authors (presumably, geopark representatives) write about rivers, lakes, springs, etc. naming these hydrological phenomena simply and correctly. However, water objects are not specified in some cases, therefore, types cannot be established. To interpret the relevance of water objects to geological heritage, the general context of use of water-related words in phrases is analyzed by simple templates provided in Table 1. Finally, visibility of water on photos that accompany many descriptions is a condition by which to judge these photos relevant to water consideration in a given geopark description.
In the present study, only water objects of the geological present are analyzed, not ancient bodies (palaeoriver, palaeolakes, etc.) interpreted for the geological past and belonging directly to geological heritage. Attention is paid to water in only the liquid state (including hot water in springs and geothermal fields), i.e., glaciers and snowfields are not analyzed; these constitute the other natural elements of geological heritage landscapes and deserve separate discussion. Moreover, frozen water is tied stronger to geological environment than liquid water, and, thus, the relevant objects can be directly related to geological heritage.
The information gathered this way is further compiled to form a kind of database that can be analyzed quantitatively. First, the number of global geoparks with official descriptions mentioning water objects and/or photos representing them is measured. Second, the relative frequency of consideration of the principal water objects is established. The types of water objects are detected on the basis of the compiled information. Third, the preferred relevance of water to geological heritage is established. Fourth, possible differences in water consideration between geoparks of the principal regions of the world are traced. Currently, global geoparks are concentrated in Europe, Southeast Asia, and Latin America, and these are the principal regions. Fifth, changes in the attention to water in global geoparks through time are established. For this purpose, the year of the first geopark designation is considered, although this information is rather heterogeneous in the available descriptions, and the relevant interpretations should be carried out with a certain caution.

3. Results

Water objects are considered in the official descriptions of many UNSECO global geoparks, although the context of this consideration differs (Table 2). From a total of 144 available descriptions, 79 deal with water (55%) and 67 contain photos representing water objects (47%). Most frequently, consideration of rivers, sea/oceans, and lakes is found (Figure 2). Less attention is paid to springs and waterfalls, which is strange because these objects are not only aesthetically attractive, but also tied closely to unique geological processes. Anyway, the official descriptions of the UNESCO global geoparks reflect hydrodiversity very well. Another notable peculiarity of many descriptions is consideration of water objects not as a separate, hydrological category, but among geomorphological features. This seems to be unusual as if to restrict geomorphological features to landforms. Interestingly, some descriptions accompanied with photos of water objects do not mention these in the text, and the shown water objects seem to be more impressive than the promoted geological features. This means such photos have been chosen chiefly out of ’purely’ aesthetic reasons; these often represent spectacular coastlines, lakes, and waterfalls.
In 41% of cases, the relevance of water to geological heritage is high, i.e., water objects are thought to be constituents of the geological heritage itself. The medium and low relevance is less significant (39% and 29%, respectively). This means that the global geopark creators/managers tend to consider water in geoparks seriously, i.e., without detachment from geologically unique features (the coupled high and medium relevance constitutes 80% of cases). However, an alternative explanation is also possible: geopark managers/creators do not pay attention (or do not have experience) to separate geological and non-geological landscape elements and tend to label many of them as ‘geological’ without the necessary care.
The geographical distribution of global geoparks with official descriptions considering water objects does not show any differentiation (Figure 3). In Europe, the number of such geoparks reaches 57%, and the values in Southeast Asia and Latin America are 53% and 50%, respectively. This means the differences between major traditions of geopark establishment (apparently, more attention is paid to geology in Europe and more attention is paid to natural context of geological phenomena in Southeast Asia) do not affect consideration of water. There is a weak, but well-visible temporal trend of increase in water consideration. For geoparks designated before 2011, water objects are considered in 50% of cases, but this value rises to 60% for geoparks designated later. This implies a certain increase in attention to non-geological elements of geoparks and their relation to geological heritage.

4. Discussion and Conclusions

The results of the undertaken analysis imply that water objects are important natural elements of the UNESCO global geoparks, as one can judge on the basis of their official descriptions (and these objects may be even more important if considering hydrodiversity which is not mentioned in the official descriptions). Moreover, water is closely associated with unique geological phenomena. In other words, water objects are thought to be among the very important constituents of geological heritage landscapes. It is possible to propose three hypotheses to explain this observation. First, water objects are too numerous in territories where geoparks have been created and the geological activity of seas, rivers, and lakes is too intense there, making it impossible to ignore these objects. Second, water is in focus because it adds aesthetic value to landscape which is important to both geopark creators/managers and geopark visitors. Third, attempts to demonstrate the natural integrity of geoparks results in the search for non-geological natural elements, and water bodies are among the best candidates. Most probable, all these hypotheses are plausible in different cases. However, the strengthened emphasis on geodiversity and geological heritage landscape integrity [22,23,24] and, particularly, links between water and geology in landscape systems [25,26,27] stimulate geopark practitioners to focus on water bodies. If so, the third hypothesis may provide a kind of universal explanation. This hypothesis is also proved by some results of the present study, i.e., by the absence of geographical differentiation in water consideration (Figure 3) and the increase in this consideration over time (see above). However, the registered consideration of water objects is somewhat haphazard, which is expected as geoparks are essentially aimed more at geology than the rest of nature.
The main outcome of this study, i.e., the signification attention to water objects in the UNESCO Global Geoparks network, requires discussion of the advantages and disadvantages of the situation where this attention affects geopark management. The advantage is evident: global geoparks contribute to the understanding of nature integrity (Figure 1). This is necessary owing to two circumstances. First, an emphasis on only geology would limit comprehension of the relevance of old rocks and fossils to the modern world. Second, such an emphasis would make the knowledge available in geoparks too specific to attract enough visitors (motivation is a significant challenge in geotourism [28]). However, there is also a serious disadvantage, which is as follows. The majority of tourists, including geotourists (except for relatively rare geoscience professionals, students, and amateurs) do not have enough geological knowledge, and they have been not trained for perception of geological features that are masked by other landscape elements and often need special interpretation [29,30,31,32]. In contrast, tourists do not need any special knowledge to judge on rivers, lakes, or waterfalls, and the natural beauty of water objects is a significant attractor of visitors [33,34,35]. In such a case, co-management of ‘purely’ geological and hydrological features and their co-promotion through web-pages, brochures, panels, etc. complicates the attraction to geological heritage in geoparks. In other words, geoparks become more natural than geological. This problem becomes even bigger when water is considered in a haphazard manner as occurs in the official descriptions of the global geoparks, especially on photos included in these descriptions. The resulting effect is distraction from geology, which contradicts the very purpose of geoparks aimed essentially at geological heritage.
Regarding the above-said, it is impossible to recommend geopark practice for either full-scale consideration of water objects or total rejection of non-geological landscape elements. Individual solutions should be found in each given case. For instance, water objects can be promoted in-situ, but not advertised ex-situ or their strong links to geological heritage should be emphasized. However, it is worth noting that attempts to reflect nature integrity in such highly specific establishments as geoparks can be both successful and risky. It is also important to consider the uniqueness, i.e., heritage value of geological and water objects on the areas where geoparks are planned. Water heritage is an important topic of modern research [36,37]. Where water objects are more valuable than geological features, it is questionable how reasonable is geopark creation. If hydrological and geological features are of comparable uniqueness, another kind of protected area can be proposed.
The results of the present analysis of water consideration in the official descriptions of the UNESCO global geoparks, i.e., the content analysis of the fixed managerial opinions, enable three principal conclusions to be drawn. First, geopark creators/managers pay significant attention to water and tend to relate it to geological heritage. Second, this attention does not differ geographically on the global scale, but increases over time. Third, the registered situation has advantage and disadvantage, and geopark practitioners should think deeply how to deal with water in order to demonstrate nature integrity and to avoid distraction of visitors from geological heritage. The present study provides a pilot frame of judgments. Further investigations should provide a deeper understanding of the problem. For instance, geopark creators/managers could be interviewed in order to understand their attitudes toward aquatic heritage and water management.

Funding

This research received no external funding.

Acknowledgments

The author gratefully thanks the journal editors and the anonymous reviewers for thorough examination of this paper and helpful suggestions, as well as M.H. Henriques (Portugal) for literature support.

Conflicts of Interest

The author declares no conflict of interest.

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Figure 1. The relevance of water to the global geopark essence.
Figure 1. The relevance of water to the global geopark essence.
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Figure 2. Principal water objects considered in the official descriptions of the global geoparks.
Figure 2. Principal water objects considered in the official descriptions of the global geoparks.
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Figure 3. Water objects considered in the official descriptions of the global geoparks in the principal regions.
Figure 3. Water objects considered in the official descriptions of the global geoparks in the principal regions.
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Table 1. Gradation of the relevance of water objects to geological heritage in the official descriptions of the UNESCO global geoparks (proposed by the author).
Table 1. Gradation of the relevance of water objects to geological heritage in the official descriptions of the UNESCO global geoparks (proposed by the author).
RelevanceExplanationExamples of Phrasing in Geopark Description
LowCo-occurrence with unique geological phenomena1. Besides geological heritage features such as rare minerals and fossils, this geopark also hosts spectacular waterfalls and lakes.
2. The geological heritage includes stratotypes of Cretaceous units and folded rocks. A river crosses the territory of this geopark.
MediumUnique geological phenomena linked to water activity1. The geopark’s geological heritage includes Triassic reefs and deep gorges cut by rivers.
2. Unique Devonian rock exposures are available along the coast because of marine abrasion.
HighWater objects as unique geological phenomena1. The geological heritage of this geopark consists of igneous rocks, impact crater, and two hyper-saline lakes.
2. Waterfalls, carbonate mounds, and ancient volcano edifices are unique geological features of this geopark.
Note: the examples are not extracts from the real descriptions of the UNESCO global geoparks, and they are proposed to illustrate phrasing typical for detection of each type of the relevance.
Table 2. Water objects considered as elements of the UNESCO global geoparks (state for August 2019; interpretation by the author on the basis of the official geopark descriptions [21]).
Table 2. Water objects considered as elements of the UNESCO global geoparks (state for August 2019; interpretation by the author on the basis of the official geopark descriptions [21]).
GeoparkCountryYear of DesignationWater Object(s) Specified in Official DescriptionRelevance to Geological HeritageWater Object(s) Photo in Official Description
Ore of the AlpsAustria2014WaterfallsLowNo
Styrian EisenwurzenAustria2004RiversMediumYes
Karawanken/KaravankeAustria/Slovenia2013NoNoNo
Famenne-ArdenneBelgium2018Karst riversMediumYes
AraripeBrazil2006NoNoNo
PercéCanada2018OceanMediumYes
StonehammerCanada2010NoNoYes
Tumbler RidgeCanada2014RiversMediumNo
KütralkuraChile2019RiversHighNo
Alxa DesertChina2009NoNoYes
ArxanChina2017Hot springs, crater lakes, riversHighYes
Dali-CangshanChina2014NoNoNo
DanxiashanChina2004RiversLowYes
DunhuangChina2015NoNoNo
FangshanChina2006NoNoYes
FuniushanChina2006NoNoNo
Guangwushan-NuoshuiheChina2018NoNoYes
HexigtenChina2005NoNoNo
Hong KongChina2011SeaLowYes
Huanggang DabieshanChina2018NoNoNo
HuangshanChina2004Not specifiedLowNo
JingpohuChina2006LakesHighYes
JiuhuashanChina2019Not specifiedHighNo
KeketuohaiChina2017NoNoNo
LeiqiongChina2006Maar lakes, seaHighYes
Leye FengshanChina2010Karst rivers and springsHighYes
LonghushanChina2008RiversLowYes
LushanChina2004Rivers, lakeLowYes
Mount KunlunChina2014NoNoNo
NingdeChina2010RiverMediumYes
Qinling ZhongnanshanChina2009Not specifiedLowNo
SanqingshanChina2012NoNoNo
ShennongjiaChina2013NoNoNo
ShilinChina2004NoNoYes
SongshanChina2004NoNoNo
TainingChina2005NoNoYes
TaishanChina2006NoNoNo
TianzhushanChina2011NoNoNo
Wangwushan-DaimeishanChina2006RiverMediumNo
WudalianchiChina2004Cold mineral springsHighNo
XingwenChinaOfficial description not accessible
YandangshanChina2005Sea, waterfallsHighNo
YanqingChina2013NoNoNo
YimengshanChina2019NoNoYes
YuntaishanChina2004RiversHighYes
ZhangjiajieChina2004Not specifiedHighNo
Zhijindong CaveChina2015River, lakeHighNo
ZigongChina2008NoNoNo
PapukCroatia2007Karst springsHighYes
Vis ArchipelagoCroatia2019SeaMediumYes
TroodosCyprus2015NoNoNo
Bohemian ParadiseCzechia2005NoNoNo
OdsherredDenmark2014SeaMediumYes
ImbaburaEcuador2019Lakes, waterfalls, hot springsHighYes
RokuaFinland2010Bogs, lakesMediumYes
BeaujolaisFrance2018RiverLowNo
Causses du QuercyFrance2017NoNoNo
ChablaisFrance2012Lakes, mineral watersHighYes
Haute-ProvenceFrance2004NoNoNo
LuberonFrance2004Not specifiedLowNo
Massif des BaugesFrance2011Lakes, waterfallsMediumNo
Monts d’ArdècheFrance2014NoNoNo
Bergstraße-OdenwaldGermany2004NoNoNo
Harz, Braunschweiger LandGermany2004NoNoNo
Swabian AlbGermany2004NoNoNo
TERRA.vitaGermany2004NoNoNo
VulkaneifelGermany2004Crater bogs and lakesHighYes
Muskauer Faltenbogen/Luk MuzakowaGermany/Poland2011Cold mineral springsHighYes
Chelmos VouraikosGreece2009Cold springs, river, lakes, underground lakesHighNo
Lesvos IslandGreece2004Thermal springsHighNo
PsiloritisGreece2004NoNoNo
SitiaGreece2015NoNoNo
Vikos - AoosGreece2010RiversMediumNo
Bakony-BalatonHungary2012Karst water, thermal waterHighYes
Novohrad-NógrádHungary/Slovakia2010Not specifiedHighNo
KatlaIceland2011Sea, waterfalls, ice-dammed lakesHighYes
ReykjanesIceland2015Geothermal fieldsHighYes
BaturIndonesia2012Fumaroles, hot springs, lakeHighNo
Ciletuh-PalabuhanratuIndonesia2018Hot springs, geysers, oceanHighYes
Gunung SewuIndonesia2015River, lake, seaMediumYes
Rinjani-LombokIndonesia2018Caldera lakeHighYes
Qeshm IslandIranOfficial description not accessible
Burren & Cliffs of MoherIreland2011Sea, seasonal lakesHighYes
Copper CoastIreland2004SeaMediumYes
Marble Arch CavesIreland/UK2004LakesLowYes
Adamello-BrentaItaly2008NoNoNo
Alpi ApuaniItaly2011RiversLowNo
BeiguaItaly2005NoNoYes
Cilento, Vallo di Diano e AlburniItaly2010NoNoYes
MadonieItaly2004NoNoYes
Parco Geominerario della SardegnaItaly2007NoNoYes
PollinoItaly2015NoNoNo
Sesia Val GrandeItaly2013NoNoNo
Rocca di CerereItaly2004Not specifiedLowNo
Tuscan Mining ParkItaly2010NoNoYes
AsoJapan2014NoNoNo
ItoigawaJapan2009NoNoYes
Izu PeninsulaJapan2018Hot springsHighYes
Mt. ApoiJapan2015NoNoYes
MurotoJapan2011SeaMediumYes
Oki IslandsJapan2013SeaMediumYes
San’in KaiganJapan2010NoNoNo
Toya-UsuJapan2009Not specified, hot springsLowYes
Unzen Volcanic AreaJapan2009NoNoYes
LangkawiMalaysia2007Sea, riversLowYes
Comarca MineraMexicoOfficial description not accessible
Mixteca AltaMexico2017NoNoNo
M’GounMorocco2014NoNoNo
De HondsrugNetherlands2013NoNoNo
Gea NorvegicaNorway2006NoNoYes
MagmaNorway2006NoNoYes
TrollfjellNorway2019SeaLowYes
Colca y Volcanes de AndaguaPeru2019NoNoNo
AçoresPortugal2013Offshore hydrothermal fieldsHighNo
AroucaPortugal2009NoNoNo
Naturtejo da Meseta MeridionalPortugal2006NoNoNo
Terras de CavaleirosPortugal2014Rivers, artificial lakeLowYes
HategRomania2005NoNoYes
CheongsongSouth Korea2017Mineral springHighYes
Jeju IslandSouth Korea2010NoNoNo
MudeungsanSouth Korea2018WaterfallsHighNo
IdrijaSlovenia2013Not specifiedLowNo
Basque CoastSpain2010SeaLowYes
Cabo de Gata-NíjarSpain2006SeaMediumYes
Central CataloniaSpain2012NoNoNo
Conca de Tremp-MontsecSpain2018NoNoNo
Courel MountainsSpain2019RiversMediumYes
El HierroSpain2014SeaLowYes
Lanzarote and Chinijo IslandsSpain2015Not specifiedLowYes
Las LorasSpain2017RiversMediumNo
Molina and Alto TajoSpain2014NoNoNo
Sierra Norte de SevillaSpain2011WaterfallsMediumNo
Sierras SubbéticasSpain2006NoNoNo
Sobrarbe-PirineosSpain2006RiversMediumNo
Villuercas Ibores JaraSpain2011NoNoNo
Ngorongoro LengaiTanzania2018LakesHighNo
SatunThailand2018SeaMediumYes
Kula VolcanicTurkey2013NoNoNo
English RivieraUK2007SeaMediumYes
Forest FawrUK2005LakesLowYes
GeoMônUK2009SeaLowNo
North Pennines AONBUK2004RiversLowNo
North-West HighlandsUK2004NoNoYes
ShetlandUK2009SeaMediumYes
Grutas del PalacioUruguay2013RiversMediumNo
Dong Van Karst PlateauVietnam2010NoNoNo
Non nuoc Cao BangVietnam2018Rivers, lakes, underground rivers, waterfallHighYes

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MDPI and ACS Style

Ruban, D.A. Water in Descriptions of Global Geoparks: Not Less Important than Geology? Water 2019, 11, 1866. https://doi.org/10.3390/w11091866

AMA Style

Ruban DA. Water in Descriptions of Global Geoparks: Not Less Important than Geology? Water. 2019; 11(9):1866. https://doi.org/10.3390/w11091866

Chicago/Turabian Style

Ruban, Dmitry A. 2019. "Water in Descriptions of Global Geoparks: Not Less Important than Geology?" Water 11, no. 9: 1866. https://doi.org/10.3390/w11091866

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