A reef knoll is a landform built from a large accumulated mass of calcareous material laid down on an ancient sea floor, composed of the fossil rich remains of corals, sponges, calcareous algae and other reef building organisms whose dense skeletal material let the structure resist ocean currents and stand as a freestanding mound. Reef knolls are classified as either bioherms, organic sedimentary rock bodies enclosed within rock of a different origin, or biostromes, distinctly bedded or broadly lens shaped sedimentary landforms. Well known examples in England include Thorpe Cloud, Bunster Hill, Chrome Hill and Parkhouse Hill along the Derbyshire and Staffordshire border, where the surrounding softer rock has eroded away to expose the resistant knolls, along with further examples in the Yorkshire Dales near Thorpe, Malham and Settle.
Connections
In Discipline
Source Reef knoll (Wikipedia)
Sources
Reef knoll (Wikipedia)
In Discipline: Geomorphology, Lead sentenceQuote, In Discipline: Geomorphology, Lead sentence
A reef knoll is a landform that comprises an immense pile of calcareous material that had previously accumulated on an ancient sea floor.
View the Source Reader Challenges (0)
No disputes yet. Spotted an error or a better source? Open the first one.
Sign in to dispute this or suggest a correction.