See cliffing in All languages combined, or Wiktionary
{ "etymology_templates": [ { "args": { "1": "en", "2": "cliff", "3": "ing" }, "expansion": "cliff + -ing", "name": "suffix" } ], "etymology_text": "From cliff + -ing.", "head_templates": [ { "args": { "1": "-" }, "expansion": "cliffing (uncountable)", "name": "en-noun" } ], "lang": "English", "lang_code": "en", "pos": "noun", "senses": [ { "categories": [ { "kind": "other", "name": "English entries with incorrect language header", "parents": [ "Entries with incorrect language header", "Entry maintenance" ], "source": "w" }, { "kind": "other", "name": "English terms suffixed with -ing", "parents": [], "source": "w" }, { "kind": "other", "name": "Pages with 1 entry", "parents": [], "source": "w" }, { "kind": "other", "name": "Pages with entries", "parents": [], "source": "w" } ], "examples": [ { "ref": "2005, Maurice L. Schwartz, Encyclopedia of coastal science, Springer, page 613:", "text": "Cliffing of this kind is repaired if there is an abundant supply of sediment to restore the profile, permitting mangroves to spread again, but if there is a sediment deficit a mangrove cliff will persist and recede until the mangrove terrace has been completely removed.", "type": "quote" }, { "ref": "2006, K. Bharatdwaj, Physical Geography: Hydrosphere, Discovery Publishing House, page 157:", "text": "When the alternate bands of hard and soft rock dip upstream in the longitudinal course of the river and if the caprock is resistant the underlying soft rocks are eroded more rapidly due to cliffing and thus the resistant rock beds form precipituous wall-like scarps which allow the river water to fall downstram vertically and ultimately a stupendous waterfall is formed.", "type": "quote" }, { "ref": "2011, Eric C. F. Bird, Coastal Geomorphology: An Introduction, John Wiley and Sons:", "text": "Cliffing (scarping) of the seaward margins of coastal dunes and the absence of new fore dunes (or the formation of new fore dunes lasting at most a few years) is very widespread around the world’s coastline, a consequence of the modern prevalence of beach erosion (Figure 9.2).", "type": "quote" } ], "glosses": [ "The formation of cliffs." ], "id": "en-cliffing-en-noun-CWl5w~L6", "links": [ [ "formation", "formation" ], [ "cliff", "cliff" ] ], "synonyms": [ { "word": "scarping" } ], "tags": [ "uncountable" ] } ], "word": "cliffing" }
{ "etymology_templates": [ { "args": { "1": "en", "2": "cliff", "3": "ing" }, "expansion": "cliff + -ing", "name": "suffix" } ], "etymology_text": "From cliff + -ing.", "head_templates": [ { "args": { "1": "-" }, "expansion": "cliffing (uncountable)", "name": "en-noun" } ], "lang": "English", "lang_code": "en", "pos": "noun", "senses": [ { "categories": [ "English entries with incorrect language header", "English lemmas", "English nouns", "English terms suffixed with -ing", "English terms with quotations", "English uncountable nouns", "Pages with 1 entry", "Pages with entries", "Quotation templates to be cleaned" ], "examples": [ { "ref": "2005, Maurice L. Schwartz, Encyclopedia of coastal science, Springer, page 613:", "text": "Cliffing of this kind is repaired if there is an abundant supply of sediment to restore the profile, permitting mangroves to spread again, but if there is a sediment deficit a mangrove cliff will persist and recede until the mangrove terrace has been completely removed.", "type": "quote" }, { "ref": "2006, K. Bharatdwaj, Physical Geography: Hydrosphere, Discovery Publishing House, page 157:", "text": "When the alternate bands of hard and soft rock dip upstream in the longitudinal course of the river and if the caprock is resistant the underlying soft rocks are eroded more rapidly due to cliffing and thus the resistant rock beds form precipituous wall-like scarps which allow the river water to fall downstram vertically and ultimately a stupendous waterfall is formed.", "type": "quote" }, { "ref": "2011, Eric C. F. Bird, Coastal Geomorphology: An Introduction, John Wiley and Sons:", "text": "Cliffing (scarping) of the seaward margins of coastal dunes and the absence of new fore dunes (or the formation of new fore dunes lasting at most a few years) is very widespread around the world’s coastline, a consequence of the modern prevalence of beach erosion (Figure 9.2).", "type": "quote" } ], "glosses": [ "The formation of cliffs." ], "links": [ [ "formation", "formation" ], [ "cliff", "cliff" ] ], "tags": [ "uncountable" ] } ], "synonyms": [ { "word": "scarping" } ], "word": "cliffing" }
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This page is a part of the kaikki.org machine-readable English dictionary. This dictionary is based on structured data extracted on 2024-11-06 from the enwiktionary dump dated 2024-10-02 using wiktextract (fbeafe8 and 7f03c9b). The data shown on this site has been post-processed and various details (e.g., extra categories) removed, some information disambiguated, and additional data merged from other sources. See the raw data download page for the unprocessed wiktextract data.
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