Abstract
The Maltese Islands present interesting and varied karst landforms concentrated in a small land area. Sinkholes or dolines are no exception with over 50 structures being recorded in Malta and Gozo. Their formation is generally the result of subsidence , collapse or dissolution of the limestone or a combination of more than one factor. Il-Maqluba , a Quaternary collapse sinkhole, is the most spectacular on mainland Malta displaying sheer vertical walls extending for about 30 m. Il-Qawra sinkhole, of Miocene origin, forms part of a cluster of four large sinkholes located along the western coast of Gozo, Malta’s sister island. With a diameter of over 350 m and characterised by interesting geology and geomorphology, its formation is still a matter of debate.
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Notes
- 1.
The English translation for this name is ‘The Storm Street’.
- 2.
This is the highest level of protection afforded to any site. The scale ranges from 1 to 4.
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Calleja, I., Tonelli, C. (2019). Dwejra and Maqluba: Emblematic Sinkholes in the Maltese Islands. In: Gauci, R., Schembri, J. (eds) Landscapes and Landforms of the Maltese Islands. World Geomorphological Landscapes. Springer, Cham. https://doi.org/10.1007/978-3-030-15456-1_11
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