Geomorphosite

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The Simien Mountains National Park in Ethiopia hosts a rich array of geomorphosites Semien Mountains 9.jpg
The Simien Mountains National Park in Ethiopia hosts a rich array of geomorphosites
The Lonar Lake in Buldhana district, Maharashtra, India Lonar Crater Lake.jpg
The Lonar Lake in Buldhana district, Maharashtra, India
Hoodoos in Bryce Canyon National Park, Utah USA 10654 Bryce Canyon Luca Galuzzi 2007.jpg
Hoodoos in Bryce Canyon National Park, Utah
Monte Testaccio in Rome Testaccio monte dei cocci 051204-12-13.JPG
Monte Testaccio in Rome

A geomorphosite, or geomorphological heritage site, is a landform or an assemblage of landforms that have a scientific, educational, historic-cultural, aesthetic or socio-economic value. [3] [4]

The Frank Slide is a geomorphosite Frank Slide, Canada.jpg
The Frank Slide is a geomorphosite

Geomorphosites are included among the geoheritage sites (geosites) and may comprise landforms (or sites of former landforms) that have been hidden or destroyed due to human activities, [6] [7] as well as anthropogenic landforms [8] [9] of archaeological or historical interest. [10]

Iguazu Falls on the border of Argentina and Brasil Cataratas.jpg
Iguazu Falls on the border of Argentina and Brasil

The value of a geomorphosite, for purposes of analysis, comparison and protection, can be qualitatively assessed using several methods. [11] Some of these methods are based only on expert judgements and a few evaluation criteria, while others involve assigning a qualitative score to each relevant characteristic of a site (e.g. its scientific importance, educational value etc.) and then weighting and summing (or ranking) the scores to obtain the site's overall value (or rank).

The concept of geomorphosite has its roots in Western scientific thought. In recent decades, natural heritage conservation has increasingly focused on preserving representative examples of specific natural phenomena. [12] This shift aligns with the growing influence of scientific approaches and economic rationalism, which often prioritize objective, data-driven arguments over those perceived as emotional or subjective. However, this representative methodology may not be suitable, for instance, for sites considered sacred by faith communities, as these locations are unique and hold profound spiritual significance that transcends scientific categorization. [12] A solution to this problem may be to consider multiple value dimensions of a geomorphosite and to include into the evaluation process the interested stakeholders and right holders (e.g. indigenous communities), which also ensures a greater degree of objectivity in the evaluation itself. [13]

Uluru, one of the largest and best known inselbergs in the world, which constitute a fundamental landform in the traditional belief belief of Anangu people. It was added to the UNESCO World Heritage List in 1987 ULURU.jpg
Uluru, one of the largest and best known inselbergs in the world, which constitute a fundamental landform in the traditional belief belief of Aṉangu people. It was added to the UNESCO World Heritage List in 1987
Mount Langshan in Xinning County, Hunan, China, part of the China Danxia collection of landforms that entered the World Heritage List in 2010 . Mount Langshan in Hunan, Picture49.jpg
Mount Langshan in Xinning County, Hunan, China, part of the China Danxia collection of landforms that entered the World Heritage List in 2010 .

Related Research Articles

<span class="mw-page-title-main">Geomorphology</span> Scientific study of landforms

Geomorphology is the scientific study of the origin and evolution of topographic and bathymetric features generated by physical, chemical or biological processes operating at or near Earth's surface. Geomorphologists seek to understand why landscapes look the way they do, to understand landform and terrain history and dynamics and to predict changes through a combination of field observations, physical experiments and numerical modeling. Geomorphologists work within disciplines such as physical geography, geology, geodesy, engineering geology, archaeology, climatology, and geotechnical engineering. This broad base of interests contributes to many research styles and interests within the field.

<span class="mw-page-title-main">Landform</span> Feature of the solid surface of a planetary body

A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins.

<span class="mw-page-title-main">Pyrénées National Park</span> French national park in Hautes-Pyrénées and Pyrénées-Atantiques

Pyrénées National Park is a French national park located within the departments of Hautes-Pyrénées and Pyrénées-Atlantiques. The park is located along the border of France and Spain along the Pyrenees Mountains, with a scenic landscape offering a variety of outdoor activities including hiking, skiing, mountain climbing and observing wildlife.

<span class="mw-page-title-main">Bioindicator</span> Species that reveals the status of an environment

A bioindicator is any species or group of species whose function, population, or status can reveal the qualitative status of the environment. The most common indicator species are animals. For example, copepods and other small water crustaceans that are present in many water bodies can be monitored for changes that may indicate a problem within their ecosystem. Bioindicators can tell us about the cumulative effects of different pollutants in the ecosystem and about how long a problem may have been present, which physical and chemical testing cannot.

<span class="mw-page-title-main">Geodiversity</span>

Geodiversity is the variety of earth materials, forms and processes that constitute and shape the Earth, either the whole or a specific part of it. Relevant materials include minerals, rocks, sediments, fossils, soils and water. Forms may comprise folds, faults, landforms and other expressions of morphology or relations between units of earth material. Any natural process that continues to act upon, maintain or modify either material or form represents another aspect of geodiversity. However geodiversity is not normally defined to include the likes of landscaping, concrete or other significant human influence.

<span class="mw-page-title-main">Lesvos Petrified Forest</span> Petrified wood forest found on the island of Lesbos, Greece

The Lesvos Petrified Forest is a petrified wood forest on the island of Lesbos, Greece.

<span class="mw-page-title-main">Geotourism</span> Tourism associated with geological attractions and destinations

Geotourism is tourism associated with geological attractions and destinations. Geotourism deals with the abiotic natural and built environments. Geotourism was first defined in England by Thomas Alfred Hose in 1995.

<span class="mw-page-title-main">Riffle</span> Shallow landform in a flowing channel

A riffle is a shallow landform in a flowing channel. Colloquially, it is a shallow place in a river where water flows quickly past rocks. However, in geology a riffle has specific characteristics.

<span class="mw-page-title-main">Jebel Irhoud</span> Archaeological site in Morocco

Jebel Irhoud or Adrar n Ighoud, is an archaeological site located just north of the town of Tlet Ighoud in Youssoufia Province, approximately 50 km (30 mi) south-east of the city of Safi in Morocco. It is noted for the hominin fossils that have been found there since the discovery of the site in 1961. Originally thought to be Neanderthals, the specimens have since been assigned to Homo sapiens and, as reported in 2017, have been dated to roughly 300,000 years ago.

The Patrick Burn Formation is a Silurian aged geologic formation outcropping near Lesmahagow in Lanarkshire in the Scottish Lowlands. Fossils are known from the formation, including from the Birk Knowes locality.

Geoheritage is the geological aspect of natural and cultural heritage. A geosite is a particular geological heritage asset. It is a heritage category comparable to other forms of natural heritage, such as biodiversity.

<span class="mw-page-title-main">Andagua volcanic field</span> Volcanic field in Peru

The Andagua volcanic field is a volcanic field in southern Peru which includes a number of cinder cones, lava domes and lava flows which have filled the Andagua Valley. The volcanic field is part of a larger volcanic province that clusters around the Colca River and is mostly of Pleistocene age, although the Andagua sector also features volcanic cones with historical activity, with the last eruption about 370 years ago. Eruptions were mostly effusive, generating lava flows, cones and small eruption columns. Future eruptions are possible, and there is ongoing fumarolic activity. Volcanic activity in the field has flooded the Andahua valley with lava flows, damming local watersheds in the Laguna de Chachas, Laguna Mamacocha and Laguna Pumajallo lakes and burying the course of the Andagua River. The Andahua valley segment of the larger volcanic province was declared a geopark in 2015.

Miñiques is the name of a lake and a volcano in Chile. It lies south of Laguna Miscanti and at the foot of the Cerro Miscanti volcano. The lake is fed from Laguna Miscanti by seepage and its waters are brackish.

<span class="mw-page-title-main">Church and Convent of Our Lady of Mount Carmel</span>

The Church and Convent of Our Lady of Mount Carmel is a 17th-century Roman Catholic church and former convent in Salvador, Bahia, Brazil. The church is dedicated to Our Lady of Mount Carmel. The complex is adjacent to the Church of the Third Order of Mount Carmel. The Church and Convent of Our Lady of Mount Carmel was listed as a historic structure by National Institute of Historic and Artistic Heritage (IPHAN) in 1938 and is part of the Historic Center of Salvador UNESCO World Heritage Site.

<span class="mw-page-title-main">Lioz</span>

Lioz, also known as Royal Stone, is a type of limestone, originating in Portugal, from the Lisbon region. It is famed for its use as an ornamental stone, resulting in its proliferation in palaces, cathedrals, and important civic buildings throughout Portugal and the former Portuguese Empire. Owing to its historical relevance, lioz was designated a Global Heritage Stone Resource.

<i>Vespersaurus</i> Genus of noasaurine theropod dinosaur

Vespersaurus is a genus of noasaurid theropod dinosaur from the Cretaceous Rio Paraná Formation in the Paraná Basin, Brazil. The type and only species is V. paranaensis, which would have lived in the giant prehistoric Botucatu Desert.

<span class="mw-page-title-main">May Hib'o</span> Exclosure for woodland restoration in Ethiopia

May Hib’o is an exclosure located in the Dogu'a Tembien woreda of the Tigray Region in Ethiopia. The exclosure holds a 70-metre long cave.

Geoconservation is the practice of recognising, protecting and managing sites and landscapes which have value for their geology or geomorphology. The conservation of these geological sites is through government agencies and local geological societies in areas such as Europe and Africa. The designation of these sites is done through an analysis of the site, and the production of proper management infrastructure. The principles of geoconservation are to create a means of protection for the sites, and assess their value to the geological community. Typically the conservation of geodiversity at a site or within a landscape takes place alongside that of biodiversity.

The Brymbo Fossil Forest is a palaeobotanical site near Brymbo, Wrexham County Borough, Wales. It is known as a significant area of Early Carboniferous fossils, and is a Site of Special Scientific Interest.

References

  1. Mauerhofer, Lukas; Reynard, Emmanuel; Asrat, Asfawossen; Hurni, Hans (2018-12-01). "Contribution of a Geomorphosite Inventory to the Geoheritage Knowledge in Developing Countries: the Case of the Simien Mountains National Park, Ethiopia". Geoheritage. 10 (4): 559–574. Bibcode:2018Geohe..10..559M. doi:10.1007/s12371-017-0234-3. ISSN   1867-2485.
  2. Del Monte, M.; Fredi, P.; et, al. (2013-12-30). "Geosites within Rome City center (Italy): a mixture of cultural and geomorphological heritage". Geografia Fisica e Dinamica Quaternaria. 36 (2): 241–257. doi:10.4461/GFDQ.2013.36.20. ISSN   0391-9838.
  3. Panizza, Mario (2001-01-01). "Geomorphosites: Concepts, methods and examples of geomorphological survey". Chinese Science Bulletin. 46 (1): 4–5. Bibcode:2001ChSBu..46S...4P. doi:10.1007/BF03187227. ISSN   1861-9541. S2CID   94082658.
  4. Reynard, Emmanuel. "Geomorphosites: Definitions and characteristics". ResearchGate . Retrieved 14 August 2022.
  5. Morino, Costanza; Coratza, Paola; Soldati, Mauro (2022). "Landslides, a Key Landform in the Global Geological Heritage". Frontiers in Earth Science. 10. Bibcode:2022FrEaS..10.4760M. doi: 10.3389/feart.2022.864760 . hdl: 11380/1274358 . ISSN   2296-6463.
  6. Clivaz, Mélanie; Reynard, Emmanuel (2018-12-01). "How to Integrate Invisible Geomorphosites in an Inventory: a Case Study in the Rhone River Valley (Switzerland)". Geoheritage. 10 (4): 527–541. Bibcode:2018Geohe..10..527C. doi:10.1007/s12371-017-0222-7. ISSN   1867-2485. S2CID   131909317.
  7. Pica, Alessia; Luberti, Gian Marco; Vergari, Francesca; Fredi, Paola; Monte, Maurizio Del (2017-09-01). "Contribution for an Urban Geomorphoheritage Assessment Method: Proposal from Three Geomorphosites in Rome (Italy)". Quaestiones Geographicae. 36 (3): 21–36. Bibcode:2017QGeo...36c..21P. doi: 10.1515/quageo-2017-0030 . hdl: 11573/1012514 . S2CID   54893540.
  8. Szabó, József; Dávid, Lóránt; Lóczy, Dénes, eds. (2010). Anthropogenic Geomorphology. doi:10.1007/978-90-481-3058-0. ISBN   978-90-481-3057-3. S2CID   251582329.
  9. Howard, Jeffrey (2017), Howard, Jeffrey (ed.), "Anthropogenic Landforms and Soil Parent Materials", Anthropogenic Soils, Progress in Soil Science, Cham: Springer International Publishing, pp. 25–51, doi:10.1007/978-3-319-54331-4_3, ISBN   978-3-319-54331-4 , retrieved 2022-08-14
  10. Filippo, Brandolini; Cremaschi, Mauro; Manuela, Pelfini (2019-12-01). "Estimating the Potential of Archaeo-historical Data in the Definition of Geomorphosites and Geo-educational Itineraries in the Central Po Plain (N Italy)". Geoheritage. 11 (4): 1371–1396. Bibcode:2019Geohe..11.1371F. doi:10.1007/s12371-019-00370-5. ISSN   1867-2485. S2CID   182383348.
  11. Mucivuna, Vanessa Costa; Reynard, Emmanuel; Garcia, Maria da Glória Motta (2019-12-01). "Geomorphosites Assessment Methods: Comparative Analysis and Typology". Geoheritage. 11 (4): 1799–1815. Bibcode:2019Geohe..11.1799M. doi:10.1007/s12371-019-00394-x. ISSN   1867-2485. S2CID   199668533.
  12. 1 2 Kiernan, Kevin (2015-06-01). "Landforms as Sacred Places: Implications for Geodiversity and Geoheritage". Geoheritage. 7 (2): 177–193. Bibcode:2015Geohe...7..177K. doi:10.1007/s12371-014-0128-6. ISSN   1867-2485.
  13. Cameron, Enrico (2024-02-20). "Objectivity in Geosites Inventorying and Assessment Methods". Geoheritage. 16 (1): 30. Bibcode:2024Geohe..16...30C. doi:10.1007/s12371-024-00938-w. ISSN   1867-2485.
  14. "China Danxia World Heritage Site". whc.unesco.org. Retrieved 2025-01-17.

Further reading