See subgraywacke in All languages combined, or Wiktionary
{ "etymology_templates": [ { "args": { "1": "en", "2": "sub", "3": "graywacke" }, "expansion": "sub- + graywacke", "name": "prefix" } ], "etymology_text": "From sub- + graywacke.", "forms": [ { "form": "subgraywackes", "tags": [ "plural" ] } ], "head_templates": [ { "args": { "1": "~" }, "expansion": "subgraywacke (countable and uncountable, plural subgraywackes)", "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 prefixed with sub-", "parents": [], "source": "w" }, { "kind": "other", "name": "Pages with 1 entry", "parents": [], "source": "w" }, { "kind": "other", "name": "Pages with entries", "parents": [], "source": "w" }, { "kind": "topical", "langcode": "en", "name": "Minerals", "orig": "en:Minerals", "parents": [ "Matter", "Mineralogy", "Chemistry", "Nature", "Geology", "Sciences", "All topics", "Earth sciences", "Fundamental" ], "source": "w" }, { "kind": "topical", "langcode": "en", "name": "Rocks", "orig": "en:Rocks", "parents": [ "Geology", "Natural materials", "Earth sciences", "Materials", "Nature", "Sciences", "Manufacturing", "All topics", "Human activity", "Fundamental", "Human behaviour", "Human" ], "source": "w" } ], "glosses": [ "The most common type of sandstone, intermediate in composition between orthoquartzite and graywacke, typically composed of 30% to 65% quartz and chert, less than 15% clay matrix, more than 25% unstable materials such as feldspar grains and rock fragments, and voids or mineral cement exceeding the amount of clay matrix, and being lighter colored and better sorted, and with less matrix, than graywacke." ], "id": "en-subgraywacke-en-noun--LRuU5qI", "links": [ [ "mineralogy", "mineralogy" ], [ "sandstone", "sandstone" ], [ "orthoquartzite", "orthoquartzite" ], [ "graywacke", "graywacke" ] ], "raw_glosses": [ "(mineralogy) The most common type of sandstone, intermediate in composition between orthoquartzite and graywacke, typically composed of 30% to 65% quartz and chert, less than 15% clay matrix, more than 25% unstable materials such as feldspar grains and rock fragments, and voids or mineral cement exceeding the amount of clay matrix, and being lighter colored and better sorted, and with less matrix, than graywacke." ], "tags": [ "countable", "uncountable" ], "topics": [ "chemistry", "geography", "geology", "mineralogy", "natural-sciences", "physical-sciences" ] } ], "word": "subgraywacke" }
{ "etymology_templates": [ { "args": { "1": "en", "2": "sub", "3": "graywacke" }, "expansion": "sub- + graywacke", "name": "prefix" } ], "etymology_text": "From sub- + graywacke.", "forms": [ { "form": "subgraywackes", "tags": [ "plural" ] } ], "head_templates": [ { "args": { "1": "~" }, "expansion": "subgraywacke (countable and uncountable, plural subgraywackes)", "name": "en-noun" } ], "lang": "English", "lang_code": "en", "pos": "noun", "senses": [ { "categories": [ "English countable nouns", "English entries with incorrect language header", "English lemmas", "English nouns", "English terms prefixed with sub-", "English uncountable nouns", "Pages with 1 entry", "Pages with entries", "en:Minerals", "en:Rocks" ], "glosses": [ "The most common type of sandstone, intermediate in composition between orthoquartzite and graywacke, typically composed of 30% to 65% quartz and chert, less than 15% clay matrix, more than 25% unstable materials such as feldspar grains and rock fragments, and voids or mineral cement exceeding the amount of clay matrix, and being lighter colored and better sorted, and with less matrix, than graywacke." ], "links": [ [ "mineralogy", "mineralogy" ], [ "sandstone", "sandstone" ], [ "orthoquartzite", "orthoquartzite" ], [ "graywacke", "graywacke" ] ], "raw_glosses": [ "(mineralogy) The most common type of sandstone, intermediate in composition between orthoquartzite and graywacke, typically composed of 30% to 65% quartz and chert, less than 15% clay matrix, more than 25% unstable materials such as feldspar grains and rock fragments, and voids or mineral cement exceeding the amount of clay matrix, and being lighter colored and better sorted, and with less matrix, than graywacke." ], "tags": [ "countable", "uncountable" ], "topics": [ "chemistry", "geography", "geology", "mineralogy", "natural-sciences", "physical-sciences" ] } ], "word": "subgraywacke" }
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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 2024-12-01 from the enwiktionary dump dated 2024-11-21 using wiktextract (95d2be1 and 64224ec). 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.
If you use this data in academic research, please cite Tatu Ylonen: Wiktextract: Wiktionary as Machine-Readable Structured Data, Proceedings of the 13th Conference on Language Resources and Evaluation (LREC), pp. 1317-1325, Marseille, 20-25 June 2022. Linking to the relevant page(s) under https://kaikki.org would also be greatly appreciated.