Open main menu
Home
Random
Recent changes
Special pages
Community portal
Preferences
About Wikipedia
Disclaimers
Incubator escapee wiki
Search
User menu
Talk
Dark mode
Contributions
Create account
Log in
Editing
Flood basalt
(section)
Warning:
You are not logged in. Your IP address will be publicly visible if you make any edits. If you
log in
or
create an account
, your edits will be attributed to your username, along with other benefits.
Anti-spam check. Do
not
fill this in!
{{Short description|Very large volume eruption of basalt lava}} [[Image:3-Devils-grade-Moses-Coulee-Cattle-Feed-Lot-PB110016.JPG|thumb|[[Moses Coulee]] in the US showing multiple flood basalt flows of the [[Columbia River Basalt Group]]. The upper basalt is Roza Member, while the lower [[canyon]] exposes Frenchmen Springs Member basalt]] A '''flood basalt''' (or '''plateau basalt'''<ref name=Jackson1997fb>{{cite book |editor1-last=Jackson |editor1-first=Julia A. |title=Glossary of geology. |date=1997 |publisher=American Geological Institute |location=Alexandria, Virginia |isbn=0922152349 |edition=Fourth |chapter=flood basalt}}</ref>) is the result of a giant [[volcanic eruption]] or series of [[eruption]]s that covers large stretches of land or the [[ocean]] floor with [[basalt]] [[lava]]. Many flood basalts have been attributed to the onset of a [[hotspot (geology)|hotspot]] reaching the surface of the Earth via a [[mantle plume]].<ref name="RichardsDucan1989">{{Cite journal |author=Mark A. Richards |author2=Robert A. Duncan |author3=Vincent E. Courtillot |year=1989 |title=Flood Basalts and Hot-Spot Tracks: Plume Heads and Tails |journal=Science Magazine |volume=246 |issue=4926 |pages=103β107 |bibcode=1989Sci...246..103R |doi=10.1126/science.246.4926.103 |pmid=17837768 |s2cid=9147772}}</ref> [[List of flood basalt provinces|Flood basalt provinces]] such as the [[Deccan Traps]] of India are often called ''[[Trap rock|traps]]'', after the Swedish word ''trappa'' (meaning "staircase"), due to the characteristic stairstep [[geomorphology]] of many associated landscapes. [[Michael R. Rampino]] and [[Richard Stothers]] (1988) cited eleven distinct flood basalt episodes occurring in the past 250 million years, creating [[large igneous province]]s, [[lava plateau]]s, and [[mountain range]]s.<ref>{{cite journal |author=Michael R. Rampino |author2=Richard B. Stothers|title=Flood Basalt Volcanism During the Past 250 Million Years|doi=10.1126/science.241.4866.663|year=1988|journal=Science|volume=241|issue=4866|pages=663β668|pmid=17839077|bibcode=1988Sci...241..663R|s2cid=33327812|url=https://zenodo.org/record/1230982}} [http://pubs.giss.nasa.gov/docs/1988/1988_Rampino_Stothers_1.pdf PDF via NASA]{{dead link|date=June 2021|bot=medic}}{{cbignore|bot=medic}}</ref> However, more have been recognized such as the large [[Ontong Java Plateau]],<ref>{{cite journal|title=The Ontong Java Plateau|author1=Neal, C.|author2=Mahoney, J.|author3=Kroenke, L.|url=http://www3.nd.edu/~icpmslab/pdfs/OJP_Paper.pdf|year=1997|journal=Large Igneous Provinces: Continental, Oceanic, and Planetary Flood Volcanism, Geophysical Monograph 100|url-status=dead|archive-url=https://web.archive.org/web/20170101204714/http://www3.nd.edu/~icpmslab/pdfs/OJP_Paper.pdf|archive-date=2017-01-01}}</ref> and the [[Chilcotin Group]], though the latter may be linked to the [[Columbia River Basalt Group]]. Large igneous provinces have been connected to five [[mass extinction]] events,<ref name="VolumeRateCO2">{{cite journal |last1=Jiang |first1=Qiang |last2=Jourdan |first2=Fred |last3=Olierook |first3=Hugo K. H. |last4=Merle |first4=Renaud E. |last5=Bourdet |first5=Julien |last6=Fougerouse |first6=Denis |last7=Godel |first7=Belinda |last8=Walker |first8=Alex T. |date=25 July 2022 |title=Volume and rate of volcanic {{CO2}} emissions governed the severity of past environmental crises |journal=[[Proceedings of the National Academy of Sciences of the United States of America]] |volume=119 |issue=31 |pages=e2202039119 |doi=10.1073/pnas.2202039119 |doi-access=free |pmid=35878029 |pmc=9351498 |bibcode=2022PNAS..11902039J }}</ref> and may be associated with [[bolide]] impacts.<ref>{{Cite journal | doi = 10.1016/0031-9201(93)90011-W| title = A possible K-T boundary bolide impact site offshore near Bombay and triggering of rapid Deccan volcanism| journal = Physics of the Earth and Planetary Interiors| volume = 76| issue = 3β4| pages = 189| year = 1993| last1 = Negi | first1 = J. G. | last2 = Agrawal | first2 = P. K. | last3 = Pandey | first3 = O. P. | last4 = Singh | first4 = A. P. |bibcode = 1993PEPI...76..189N }}</ref>
Edit summary
(Briefly describe your changes)
By publishing changes, you agree to the
Terms of Use
, and you irrevocably agree to release your contribution under the
CC BY-SA 4.0 License
and the
GFDL
. You agree that a hyperlink or URL is sufficient attribution under the Creative Commons license.
Cancel
Editing help
(opens in new window)