See fjordic on Wiktionary
{ "etymology_templates": [ { "args": { "1": "en", "2": "fjord", "3": "ic" }, "expansion": "fjord + -ic", "name": "suffix" } ], "etymology_text": "From fjord + -ic.", "head_templates": [ { "args": { "1": "-" }, "expansion": "fjordic (not comparable)", "name": "en-adj" } ], "hyphenation": [ "fj‧ord‧ic" ], "lang": "English", "lang_code": "en", "pos": "adj", "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 -ic", "parents": [], "source": "w" }, { "kind": "other", "name": "Pages with 1 entry", "parents": [], "source": "w" }, { "kind": "other", "name": "Pages with entries", "parents": [], "source": "w" } ], "examples": [ { "ref": "2010, M. E. Inall, P. A. Gillibrand, “The Physics of Mid-latitude Fjords: A Review”, in J. A. Howe, W. E. N. Austin, M. Forwick, M. Paetzel, editors, Fjord Systems and Archives (Geographical Society Special Publication; no. 344), London: The Geological Society, →ISBN, page 17:", "text": "Why should the flow of water within a fjord be of interest to the geologist? After all, fjordic geomorphology has changed little over the last few thousand years. One reason is that attention has recently focused on fjords as archives of Holocene climate change.", "type": "quote" } ], "glosses": [ "Relating to fjords." ], "id": "en-fjordic-en-adj-D1OO~BEJ", "links": [ [ "fjord", "fjord" ] ], "tags": [ "not-comparable" ] } ], "sounds": [ { "ipa": "/ˈfiːɔːdɪk/", "tags": [ "Received-Pronunciation" ] }, { "ipa": "/fiˈɔːdɪk/", "tags": [ "Received-Pronunciation" ] }, { "ipa": "/fjɔːdɪk/", "tags": [ "Received-Pronunciation" ] }, { "ipa": "/fiˈɔ(ə)ɹdɪk/", "tags": [ "General-American" ] }, { "ipa": "/fjɔ(ə)ɹdɪk/", "tags": [ "General-American" ] } ], "word": "fjordic" }
{ "etymology_templates": [ { "args": { "1": "en", "2": "fjord", "3": "ic" }, "expansion": "fjord + -ic", "name": "suffix" } ], "etymology_text": "From fjord + -ic.", "head_templates": [ { "args": { "1": "-" }, "expansion": "fjordic (not comparable)", "name": "en-adj" } ], "hyphenation": [ "fj‧ord‧ic" ], "lang": "English", "lang_code": "en", "pos": "adj", "senses": [ { "categories": [ "English adjectives", "English entries with incorrect language header", "English lemmas", "English terms suffixed with -ic", "English terms with quotations", "English uncomparable adjectives", "Pages with 1 entry", "Pages with entries" ], "examples": [ { "ref": "2010, M. E. Inall, P. A. Gillibrand, “The Physics of Mid-latitude Fjords: A Review”, in J. A. Howe, W. E. N. Austin, M. Forwick, M. Paetzel, editors, Fjord Systems and Archives (Geographical Society Special Publication; no. 344), London: The Geological Society, →ISBN, page 17:", "text": "Why should the flow of water within a fjord be of interest to the geologist? After all, fjordic geomorphology has changed little over the last few thousand years. One reason is that attention has recently focused on fjords as archives of Holocene climate change.", "type": "quote" } ], "glosses": [ "Relating to fjords." ], "links": [ [ "fjord", "fjord" ] ], "tags": [ "not-comparable" ] } ], "sounds": [ { "ipa": "/ˈfiːɔːdɪk/", "tags": [ "Received-Pronunciation" ] }, { "ipa": "/fiˈɔːdɪk/", "tags": [ "Received-Pronunciation" ] }, { "ipa": "/fjɔːdɪk/", "tags": [ "Received-Pronunciation" ] }, { "ipa": "/fiˈɔ(ə)ɹdɪk/", "tags": [ "General-American" ] }, { "ipa": "/fjɔ(ə)ɹdɪk/", "tags": [ "General-American" ] } ], "word": "fjordic" }
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This page is a part of the kaikki.org machine-readable All languages combined 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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