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- Q5115859 subject Q8470037.
- Q5115859 subject Q8487923.
- Q5115859 abstract "The Chuckanut Formation in northwestern Washington (named after the Chuckanut Mountains, near Bellingham), its extension in southwestern British Columbia (the Huntingdon Formation), and various related formations in central Washington (including the Swauk, Roslyn, Manastash, and Chumstick) are fluvial sedimentary formations of Eocene age, deposited from about 54 Ma (millions of years ago) to around 42 to 34 Ma. The nature of the deposits and included plant fossils indicate a low-lying coastal plain with a subtropical climate; the nature of the sediments indicates metamorphic sources in northeastern Washington.".
- Q5115859 thumbnail Sablaites_campbelli_fossils.JPG?width=300.
- Q5115859 wikiPageExternalLink ofr791149.
- Q5115859 wikiPageExternalLink b36605724.pdf.
- Q5115859 wikiPageExternalLink ger_washington_geology_1997_v25_no3.pdf.
- Q5115859 wikiPageExternalLink Monger_JWH1994_pt4.pdf.
- Q5115859 wikiPageExternalLink www.northwestgeology.com.
- Q5115859 wikiPageExternalLink v75%20p211%20Mustoe%20and%20Girouard.PDF.
- Q5115859 wikiPageExternalLink 403.
- Q5115859 wikiPageExternalLink ger_washington_geology_2001_v29_no1-2.pdf.
- Q5115859 wikiPageWikiLink Q1223.
- Q5115859 wikiPageWikiLink Q1493735.
- Q5115859 wikiPageWikiLink Q1510360.
- Q5115859 wikiPageWikiLink Q170479.
- Q5115859 wikiPageWikiLink Q17512613.
- Q5115859 wikiPageWikiLink Q1946537.
- Q5115859 wikiPageWikiLink Q223044.
- Q5115859 wikiPageWikiLink Q24639.
- Q5115859 wikiPageWikiLink Q284777.
- Q5115859 wikiPageWikiLink Q30.
- Q5115859 wikiPageWikiLink Q3123499.
- Q5115859 wikiPageWikiLink Q338199.
- Q5115859 wikiPageWikiLink Q35409.
- Q5115859 wikiPageWikiLink Q374835.
- Q5115859 wikiPageWikiLink Q40614.
- Q5115859 wikiPageWikiLink Q430267.
- Q5115859 wikiPageWikiLink Q47069.
- Q5115859 wikiPageWikiLink Q47089.
- Q5115859 wikiPageWikiLink Q5083.
- Q5115859 wikiPageWikiLink Q5113.
- Q5115859 wikiPageWikiLink Q5115863.
- Q5115859 wikiPageWikiLink Q5473520.
- Q5115859 wikiPageWikiLink Q736917.
- Q5115859 wikiPageWikiLink Q7377.
- Q5115859 wikiPageWikiLink Q7620999.
- Q5115859 wikiPageWikiLink Q76274.
- Q5115859 wikiPageWikiLink Q8470037.
- Q5115859 wikiPageWikiLink Q8487923.
- Q5115859 comment "The Chuckanut Formation in northwestern Washington (named after the Chuckanut Mountains, near Bellingham), its extension in southwestern British Columbia (the Huntingdon Formation), and various related formations in central Washington (including the Swauk, Roslyn, Manastash, and Chumstick) are fluvial sedimentary formations of Eocene age, deposited from about 54 Ma (millions of years ago) to around 42 to 34 Ma.".
- Q5115859 label "Chuckanut Formation".
- Q5115859 depiction Sablaites_campbelli_fossils.JPG.
