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azonOnto:roleName "Inna"@pl ],
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azonOnto:description "El Fuerte de Samaipata is a red sandstone rock with high porosity. It contains iron compounds, which affect both its colour and resistance to weathering. It is a rock uplift exposed to destructive atmospheric factors: chemical, mechanical, and physical. Most processes are initiated in the presence of water in various forms (rainfall, fog and condensation). Wind and associated abrasion processes are also highly destructive. All these factors affect the intensive weathering of the rock. There are deep cracks in sandstone in many places. The largest run diagonally from the north-west to the south-east. The rock is covered with reliefs of varying heights. Due to the presence of artificial (reliefs with symbolic decoration) and natural depressions, there are numerous deposits where water, loose rock fragments, and organic material deposited by the wind collect. The accumulation of humidity and organic material creates favourable conditions for the development of lichens, and as a consequence of their soil-forming activity, also the growth of higher vegetation and mosses. These plants are strongly rooted. Attempts to remove them can damage the rock, and root expansion leads to the cracking and breaking of the rock. The growth of numerous types of fungi, algae, and lichens including Lecanora, Cladonia, Aspicilia, Xanthoria, and Rhizocarpon is observed on most of the rock surface. Lichens cause moisture in the sandstone to be retained, create colourful spots on the entire surface of El Fuerte, and the acids they produce cause rapid progressive chemical erosion of the rock. Lichens have a particularly destructive effect, as they form spots that are crusty and very stiff. Their presence causes not only drastic colour changes, but also the transformation of the stone structure and, as a consequence, the powdering and flaking of the surface attacked by them. This type of lichen is observed on the surface of El Fuerte in the northern part, and is particularly abundant in one of the most valuable parts of the monument - within the relief that depicts the “Big Snake” (the rattlesnake) and on the surface of what is known as the “Choir of Priests”."@en ;
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azonOnto:name "Republic of Bolivia"@en ;
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azonOnto:name "Boliwia"@pl ;
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azonOnto:name "CC BY-ND-NC 4.0"^^xsd:string ;
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azonOnto:name "Politechnika Wrocławska"^^xsd:string ] ;
azonOnto:publicationPlace "Wrocław"^^xsd:string ;
azonOnto:publicationYear 2020 ;
azonOnto:publisher "Architectus"^^xsd:string ;
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azonOnto:name "Petrographic, mineralogical, and climatic analyses, and risk maps for conservation strategies"^^xsd:string ;
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azonOnto:scientificDiscipline "Dziedzina nauk inżynieryjno-technicznych / architektura i urbanistyka (2018)"@pl ;
azonOnto:seriesName "Architectus Numer 2(62)/2020"^^xsd:string ;
azonOnto:submitter [ a azonOnto:Person ;
azonOnto:name "Aleksandra Brzozowska-Jawornicka"^^xsd:string ] ;
azonOnto:title "El Fuerte de Samaipata. Green plant zones and Zones of intensive occurrence of lichens, fungi, and algae"@pl ;
azonOnto:titleVariant "El Fuerte de Samaipata. Green plant zones and Zones of intensive occurrence of lichens, fungi, and algae"@pl,
"El Fuerte de Samaipata. Strefy roślinności zielonej i strefy intensywnego występowania porostów, grzybów i glonów"@pl .
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