A gilgai is a small, ephemeral lake formed from a depression in the soil surface in expanding clay soils. Additionally, the term "gilgai" is used to refer to the overall micro-relief in such areas, consisting of mounds and depressions, not just the lakes themselves. The name comes from an Australian Aboriginal word meaning small water hole. These pools are commonly a few metres across and less than 30 cm (12 in) deep, however in some instances they may be several metres deep and up to 100 m (330 ft) across. Gilgais are found worldwide wherever cracking clay soils and pronounced wet and dry seasons are present. Gilgais are also called "melonholes, crabholes, hogwallows or puff and shelf formations".
| Attributes | Values |
|---|
| rdf:type
| |
| rdfs:label
| - Gilgai (de)
- Gilgai (en)
- Gilgai (es)
|
| rdfs:comment
| - Gilgai sind kleine, ephemere, feuchte Bodenstellen, Lachen, Wasserlöcher bzw. Seen, die sich in wannenartigen Bodenvertiefungen gebildet haben. Sie finden sich vor allem in warmen Klimazonen und werden von quellfähigen Tonböden unterlagert. Im weitergehenden Sinne werden als Gilgai sämtliche Mikroreliefformen bezeichnet, die eine aus seichten Wannen und anliegenden flachen Erhebungen bestehende Morphologie aufweisen. Gilgai sind somit eine Sammelbezeichnung für Oberflächenformen mit regelmäßigen Strukturen, die durch jahreszeitlich bedingte Feuchtigkeitswechsel entstehen. (de)
- A gilgai is a small, ephemeral lake formed from a depression in the soil surface in expanding clay soils. Additionally, the term "gilgai" is used to refer to the overall micro-relief in such areas, consisting of mounds and depressions, not just the lakes themselves. The name comes from an Australian Aboriginal word meaning small water hole. These pools are commonly a few metres across and less than 30 cm (12 in) deep, however in some instances they may be several metres deep and up to 100 m (330 ft) across. Gilgais are found worldwide wherever cracking clay soils and pronounced wet and dry seasons are present. Gilgais are also called "melonholes, crabholes, hogwallows or puff and shelf formations". (en)
- Un gilgai es un pequeño y efímero lago de forma circular formado en una depresión en la superficie de un suelo muy rico en arcilla o vertisol. Estos suelos se expanden y contraen fácilmente dado lugar a elevaciones y hundimientos del terreno que adquieren formas regulares geométricas. Asimismo se aplica el término a los microrrelieves superficiales en el mismo tipo de terrenos, consistentes en montículos y depresiones, no solo los lagos. El nombre procede de una palabra aborigen australiana que significa "pequeño agujero con agua". Estas balsas se encuentran generalmente a pocos metros entre ellas y tienen menos de 30 cm de profundidad; sin embargo, en algunas circunstancias, pueden tener varios metros de profundidad y encontrarse a 100 m una de otra. (es)
|
| foaf:depiction
| |
| dcterms:subject
| |
| Wikipage page ID
| |
| Wikipage revision ID
| |
| Link from a Wikipage to another Wikipage
| |
| sameAs
| |
| dbp:wikiPageUsesTemplate
| |
| thumbnail
| |
| caption
| - A gilgai landscape, Queensland (en)
|
| height
| |
| has abstract
| - Gilgai sind kleine, ephemere, feuchte Bodenstellen, Lachen, Wasserlöcher bzw. Seen, die sich in wannenartigen Bodenvertiefungen gebildet haben. Sie finden sich vor allem in warmen Klimazonen und werden von quellfähigen Tonböden unterlagert. Im weitergehenden Sinne werden als Gilgai sämtliche Mikroreliefformen bezeichnet, die eine aus seichten Wannen und anliegenden flachen Erhebungen bestehende Morphologie aufweisen. Gilgai sind somit eine Sammelbezeichnung für Oberflächenformen mit regelmäßigen Strukturen, die durch jahreszeitlich bedingte Feuchtigkeitswechsel entstehen. (de)
- Un gilgai es un pequeño y efímero lago de forma circular formado en una depresión en la superficie de un suelo muy rico en arcilla o vertisol. Estos suelos se expanden y contraen fácilmente dado lugar a elevaciones y hundimientos del terreno que adquieren formas regulares geométricas. Asimismo se aplica el término a los microrrelieves superficiales en el mismo tipo de terrenos, consistentes en montículos y depresiones, no solo los lagos. El nombre procede de una palabra aborigen australiana que significa "pequeño agujero con agua". Estas balsas se encuentran generalmente a pocos metros entre ellas y tienen menos de 30 cm de profundidad; sin embargo, en algunas circunstancias, pueden tener varios metros de profundidad y encontrarse a 100 m una de otra. Los gilgais se encuentran en todo el mundo donde haya vertisoles, que son suelos negros, con un alto contenido en un tipo de arcilla denominado montmorillonita, muy expansiva, y con estaciones húmeda y seca muy diferenciadas. La contracción y expansión continuadas forman microlomas y microdepresiones que en el caso de los gilgais forman círculos parecidos a los que se forman en los o suelos helados, donde los ciclos de hielo-deshielo dan lugar a . (es)
- A gilgai is a small, ephemeral lake formed from a depression in the soil surface in expanding clay soils. Additionally, the term "gilgai" is used to refer to the overall micro-relief in such areas, consisting of mounds and depressions, not just the lakes themselves. The name comes from an Australian Aboriginal word meaning small water hole. These pools are commonly a few metres across and less than 30 cm (12 in) deep, however in some instances they may be several metres deep and up to 100 m (330 ft) across. Gilgais are found worldwide wherever cracking clay soils and pronounced wet and dry seasons are present. Gilgais are also called "melonholes, crabholes, hogwallows or puff and shelf formations". Gilgais are thought to form in vertisols through repeated cycles of swelling of the clay when wet and subsequent shrinkage upon drying. This action, known as argillipedoturbation, causes the soil to crack when dry and loose soil material then fills these cracks. When the soil swells upon subsequent re-wetting the soil pressure cannot be dispersed into the now-full cracks and the soil is forced sideways causing a mound to form between cracks and a depression to form at the location of the crack. The process is then further exaggerated by the depressions holding water and thus becoming wetter and swelling more than the mounds, causing even greater shrinkage and cracking. In addition, the cracks channel water deeply into the soil causing even greater swelling and subsequent cracking of the depression areas. Each cycle of swelling, shrinkage and cracking becomes more exaggerated and the landscape eventually becomes covered by a repeated pattern of mounds and depressions. The depressions hold surface water during the wet seasons. Australia has an abundance of cracking clay soils and a large areas dominated by very pronounced wet and dry seasons providing ideal circumstances for the formation of gilgais. Areas outside Australia that also have the necessary conditions for gilgai formation include central Russia and several parts of the United States, including South Dakota and Texas. Gilgais are structurally similar to the patterned ground of frigid regions, however periglacial soil polygons are formed by repeated freeze-thaw cycles rather than the soil moisture cycles that create gilgai. Gilgais were an important source of water for Indigenous Australians and enabled people to seasonally forage over areas that lacked permanent water. Similarly, they allowed the stock of early Australian pastoralists to seasonally graze these areas. The introduction of water wells and pumps has reduced the value of gilgais to humans as a source of water. Gilgais are now generally considered a nuisance by farmers. The movement of soil associated with gilgai formation damages infrastructure including building foundations, roads and railway lines and the undulations produced interfere with crop harvesting. The presence of seasonal water in grazing land makes it more difficult to control stock and provides a water supply for "vermin" such as feral pigs and kangaroos. Gilgais remain of great ecological significance as a source of water for animal and plant life. Crayfish burrow in the wet basins and ants build up the mounds, magnifying the formations through bioturbation. (en)
|
| fullheight
| |
| fullwidth
| |
| gold:hypernym
| |
| prov:wasDerivedFrom
| |
| page length (characters) of wiki page
| |
| foaf:isPrimaryTopicOf
| |
| is Link from a Wikipage to another Wikipage
of | |
| is Wikipage redirect
of | |
| is foaf:primaryTopic
of | |
![[RDF Data]](/fct/images/sw-rdf-blue.png)
![[cxml]](/fct/images/cxml_doc.png)
![[csv]](/fct/images/csv_doc.png)
![[text]](/fct/images/ntriples_doc.png)
![[turtle]](/fct/images/n3turtle_doc.png)
![[ld+json]](/fct/images/jsonld_doc.png)
![[rdf+json]](/fct/images/json_doc.png)
![[rdf+xml]](/fct/images/xml_doc.png)
![[atom+xml]](/fct/images/atom_doc.png)
![[html]](/fct/images/html_doc.png)
