Großer Block von aa-Lava, der aus der Strömung des Vulkans Chinyero von 1909 hervorragt und möglicherweise durch Erstarrung und Kompression der Lavaoberfläche gebildet wurde

• Bildanbieter: Michael David Murphy / Alamy Stock Foto
• Bild-ID: 2T4J27J
• Dateigröße: 130 MB (5,8 MB Komprimierter Download)
• Freigaben (Releases): Model - nein | Eigentum - nein
• Format: 8256 x 5504 px | 69,9 x 46,6 cm | 27,5 x 18,3 inches | 300dpi
• Aufnahmedatum: 2. Juni 2023
• Ort: Chinyero, Tenerife, Canary Islands, Spain

Weitere Informationen

Volcanic eruptions on the island of Tenerife tend to occur with a frequency of between 100-200 years. These eruptions are mostly monogenetic events from strombolian type cones situated in the mountainous areas in the north-west and north-east of the island. These eruptions tend to produce basaltic aa lavas which can travel several km downslope and localised scoriaceous pyroclastics close to the cones. Pahoeohoe lavas do occur but appear to be much less common than aa types. More evolved phonolitic eruptions, both lavas and explosive pyroclastics, tend to occur high up on the island, associated with the Teide complex, but are much less frequent than the monogenetic basaltic eruptions and there are no historical examples of evolved explosive eruptions.

Stockbilder mithilfe von Tags suchen

• 1909 ausbruch
• aa
• basalt
• basaltisch
• block
• blockig
• canarias
• chinyero vulkan
• fließt
• flluss
• historischer ausbruch
• kanaren
• láva
• lava fließt
• lava flow
• lavastrom von 1909
• oib
• oxidiert
• ozeanischer inselbasalt
• rotem
• rubbly
• spanie
• teneriffa
• vulkanei
• vulkanisches
• zusammenpressen