Klastline Formation
{{Short description|Geological formation in British Columbia}}
{{Infobox Rockunit
| name = Klastline Formation
| image = File:Klastline Formation cones.jpg
| caption = Glacially modified pyroclastic cones of the Klastline Formation
| type = Geological formation{{Cite report|last1=Souther|first1=J. G.|author-link1=Jack Souther|title=The Late Cenozoic Mount Edziza Volcanic Complex, British Columbia|work=Geological Survey of Canada|publisher=Canada Communication Group|series=Memoir 420|year=1992|pages=22, 28, 191, 246, 267|isbn=0-660-14407-7|doi=10.4095/133497|doi-access=free}}
| age = Pleistocene
{{Fossil range|0.774|0.118}}
| period = Pleistocene
| prilithology = Alkali basalt
| namedfor = Klastline River
| namedby = Souther et al.{{cite web|url=https://weblex.canada.ca/html/007000/GSCC00053007723.html|title=Klastline Formation|work=Lexicon of Canadian Geologic Units|publisher=Government of Canada|access-date=2023-09-21}}
| region = British Columbia
| coordinates = {{coord|57.5|N|130.6|W|display=inline,title}}{{cite thesis|last1=Edwards|first1=Benjamin Ralph|degree=PhD|title=Field, kinetic, and thermodynamic studies of magmatic assimilation in the Northern Cordilleran Volcanic Province, northwestern British Columbia|publisher=University of British Columbia|year=1997|page=10|isbn=0-612-25005-9}}
| unitof = Mount Edziza volcanic complex
| subunits = Junction Member, Village Member{{cite journal|last1=Spooner|first1=Ian S.|last2=Osborn|first2=Gerald D.|last3=Barendregt|first3=R.|last4=Irving|first4=E.|url=http://www.acadiau.ca/~ispooner/pdfs_of_papers/Stikine%20River%20PAleomag%20Paper%20CJES.pdf|title=A Middle Pleistocene (isotope stage 10) glacial sequence in the Stikine River valley, British Columbia|journal=Canadian Journal of Earth Sciences|publisher=NRC Research Press|pages=1429−1431|volume=33|year=1996|issue=10 |doi=10.1139/e96-107 |bibcode=1996CaJES..33.1428S |access-date=2023-09-20}}
| underlies = Big Raven Formation
| overlies = Edziza Formation
| thickness =
| extent =
| area =
| map =
| map_caption =
}}
The Klastline Formation is a stratigraphic unit of Pleistocene age in northwestern British Columbia, Canada.
Description
The Klastline Formation is part of the Mount Edziza volcanic complex. This is the second largest eruptive centre in the Northern Cordilleran Volcanic Province, attaining a volume of {{Convert|670|km3|mi3|abbr=off}} and an area of {{Convert|1000|km2|mi2|abbr=off}}.{{cite journal|title=Distribution, nature, and origin of Neogene–Quaternary magmatism in the northern Cordilleran volcanic province, Canada|last1=Edwards|first1=Benjamin R.|last2=Russell|first2=James K.|journal=Geological Society of America Bulletin|publisher=Geological Society of America|page=1284|volume=112|issue=8|year=2000|issn=0016-7606|doi=10.1130/0016-7606(2000)112<1280:dnaoon>2.0.co;2|bibcode=2000GSAB..112.1280E }} It consists of shield volcanoes, stratovolcanoes, cinder cones and lava domes that have formed in the last 12 million years.{{cite gvp|vn=320060|vtab=Subfeatures|title=Edziza: Synonyms & Subfeatures|archive-date=2021-08-10|access-date=2023-09-07}}
The Klastline Formation was emplaced during the fourth magmatic cycle of the Mount Edziza volcanic complex. It consists of volcanic rocks that were issued from at least three eruptive centres on the northern and eastern sides of the Mount Edziza volcanic complex which produced minor lava fountains and small pyroclastic cones. Lava of the Klastline Formation temporarily blocked streams adjacent to the volcanic complex which resulted in the creation of lava dammed lakes.
Lithology
The Klastline Formation consists primarily of alkali basalt flows interbedded with sand and gravel. It contains two named subunits; the Village Member which consists of regular columnar basalt jointing, and the Junction Member which is characterized by swirly jointed basalt. A sedimentary sequence referred to as the Days Ranch Member is preserved between various remnants of the Village Member. It consists of well-sorted sand and gravel.
Distribution
The Klastline Formation has a volume of {{Convert|5.4|km3|mi3|abbr=off}}, making it one of the least voluminous geological formations of the Mount Edziza volcanic complex. It occurs along the valleys of Kakiddi Creek and the Klastline River where it forms isolated, usually flat-topped erosional remnants with {{Convert|6|to|12|m|ft|adj=on|abbr=off}} high escarpments. Klastline Cone on the western side of Kakiddi Valley was the main source of the Klastline Valley flows. Remnants of Klastline Formation basalt flows south of Buckley Lake form scattered outcrops and likely issued from a low, grassy hill surrounded by younger Big Raven Formation basalt flows. A {{Convert|55|km|mi|adj=mid|-long|abbr=off}} sequence of Klastline Formation basalt flows is exposed along the Stikine River downstream from the Klastline River confluence.
Age
The Klastline Formation was probably deposited over a long period of eruptive activity during the Middle to Late Pleistocene.{{cite book|last1=Smellie|first1=John L.|last2=Edwards|first2=Benjamin R.|title=Glaciovolcanism on Earth and Mars: Products, Processes and Palaeoenvironmental Significance|publisher=Cambridge University Press|year=2016|page=44|isbn=978-1-107-03739-7}} K–Ar dating of a large remnant of Klastline Formation basalt in Klastline Valley has yielded an age of 0.62 ± 0.04 million years. This age is consistent with its stratigraphic position between the Edziza and Kakiddi formations, which have ages of 0.9 million years and 0.3 million years, respectively. A K–Ar date of 0.33 ± 0.03 million years has been obtained from the top of a Village Member basalt flow on the Tahltan River, suggesting that Klastline volcanism may have been coeval with that of the Kakiddi Formation. Village Member basalt about {{Convert|2|km|mi|abbr=off}} downstream from the mouth of the Tahltan River on the east bank of the Stikine River has yielded a similar Ar–Ar date of 0.30 ± 0.10 million years.
See also
References
{{reflist|30em}}
{{Mount Edziza volcanic complex}}
Category:Geologic formations of the Mount Edziza volcanic complex
Category:Pleistocene British Columbia