Jump to content
Science Forums

Interesting Geology


Turtle

Recommended Posts

If I could hang around Turtle more, I know I'd be the smarter for it...

:phones::wave2::please: :agree: :bounce: :roll: :fever: :singer: :hihi: :bounce: :spin: :clue: ;)

 

you are too kind rac san. :bow: if i were the apologizing kind, i might apologize for being so reclusive. :lol: que sera sera. :)

 

i bookmarked this link for some one or another of these geology themed threads but alas i forget which. in any case i'll put it here as we have been on about volcanos of late. enjoy. :clue: :spin: :turtle:

 

Geologic Investigations Map I-2800: This Dynamic Planet

This Dynamic Planet

World Map of Volcanoes, Earthquakes, Impact Craters, and Plate Tectonics

Third Edition (Published 2006)

 

By Tom Simkin,1 Robert I. Tilling,2 Peter R. Vogt3,1 Stephen H. Kirby,2 Paul Kimberly,1 and David B. Stewart2

Cartography and graphic design by Will R. Stettner,2 with contributions by Antonio Villaseñor,4 and edited by Katharine S. Schindler2

 

1Smithsonian Institution, 2U.S. Geological Survey, 3U.S. Naval Research Laboratory, 4Institute of Earth Sciences Jaume Almera, Spanish National Research Council

...

Below: Thumbnail image of the front of the map, which measures 58 by 45 inches, and a figure representative of the materials on the reverse side of the map

 

Link to comment
Share on other sites

Me and a buddy went hiking along the Columbia River Gorge.. There are so many interesting geologic formations!

 

and so may great hikes available to explore.

We did the Wygant on the latest excursion.. a pretty rough trail and rather difficult.

 

The Columbia River - Mitchell Point, Oregon

 

this image is from racoon san's link. :(

 

 

on first seeing it and some of the other photos there, i thought they were photos rac took himself. so apparently not but perhaps he will favor us with some if he has them. :P ;)

 

so, to the interesting parts at a turtle's pace! . . . :) there exist on continents today fewer than half-a-dozen such rock formations as those of the columbia plateau & gorge. it is a standing joke among some friends that i drove up the gorge with years ago to say "what kind of rock is that", and then all shout in unison, "BASALT!" you might well imagine what it might be like to be confined with me in a small space for several hours if the joke is not apparent enough. :eek: :D

 

so it's all basalt and one gigantomundous set of eruptions of lava along seams miles long, rather than erupting vents as in my nearby green mountain which lies less than 20 miles wnw of the terminus of the columbia basalts in the columbia river gorge. here we go thens. :thumbs_up

 

Flood basalt - Wikipedia, the free encyclopedia

A flood basalt or trap basalt is the result of a giant volcanic eruption or series of eruptions that coats large stretches of land or the ocean floor with basalt lava. Flood basalts have occurred on continental scales (large igneous provinces) in prehistory, creating great plateaus and mountain ranges. Flood basalts have erupted at random intervals throughout geological history and are clear evidence that the Earth undergoes periods of enhanced activity rather than being in a uniform steady state....

 

The Columbia River flood Basalt Province : Current status

Résumé / Abstract

The Columbia River flood basalt province is smaller by an order of magnitude than the Deccan, Karoo, Paraná, and Siberian continental flood basalt provinces. Its smaller size, relative youth (17-6 Ma), excellent exposure, and easy accessibility have allowed development of a flow-by-flow stratigraphy in which ' many flows can be traced across the Columbia Plateau, often linked directly to their strongly oriented feeder dikes in the southeast quadrant. The detailed stratigraphy provides a precise record of the changes in magma composition and volume with time and demonstrates more clearly here than in other provinces that single fissure eruptions had volumes in excess of 2,000 km3 and flowed across the plateau for distances up to 600 km with negligible changes in chemical or mineralogical composition. Current evidence suggests that the Columbia River flood basalts resulted from impingement of a small mantle plume, the Yellowstone hotspot, on the base of the lithosphere near the Nevada-Oregon-Idaho border at 16.5 Ma and that the main focus of eruption then moved rapidly north to the Washington-Oregon-Idaho border from where the main eruptions occurred. ...

 

note: there is some new evidence that the siberian flood basalts resulted from antipodal focussing of a very large meteor impact, the crater of which now lies beneath the antarctic ice, and that interesting story is in one of our "impact" threads here. :thumbs_do

Link to comment
Share on other sites

note: there is some new evidence that the siberian flood basalts resulted from antipodal focussing of a very large meteor impact, the crater of which now lies beneath the antarctic ice, and that interesting story is in one of our "impact" threads here. ;)

 

so doing some outside reading i came across some of the material i mentioned about antipodal focussing and discovered that it is considered a possibility that the columbia flood basalts were initiated by a large impactor.

 

so what the rock is antipodal focussing? :phones: funny you should ask. :)

 

Shock Dynamics: Antipodal effects

 

so here is the bit, an abstract only, mentioning the possibility of an impact triggering the columbia flood basalts. note that at the necessary position, the antipode, no impact crater evidence is yet found. (boldenation mine.) . . . . :doh: ;) :hihi:

 

Energy Citations Database (ECD) - - Document #10197028

We suggest that the most likely result of the focusing for a sufficiently large impact, consistent with features observed in the geological record, would be a flood basalt eruption at the antipode followed by hotspot volcanism. A direct prediction of this model would be the existence of undiscovered impact structures whose reconstructed locations would be antipodal to flood basalt provinces. One such structure would be in the Indian Ocean, associated with the Columbia River Basalts and Yellowstone; another would be a second K/T impact structure in the Pacific Ocean, associated with the Deccan Traps and Reunion.
Link to comment
Share on other sites

i earlier misspoke when i put the terminus of the columbia flood basalts 20 miles ese of green mountain; in fact the basalts extend all the way to the coast. here is a map & some explanatory material. ;)

 

CVO Website - Columbia River Flood Basalts - Map

 

i also plotted the antipode of the columbia flood basalts, starting from the more-or-less geometric center of gravity of the flood basalts extent shown on the map above; centered near Umatilla. i used this mapping tool: >> Antipodes Map - Antipodal location for any map point

mind that it takes a veeeerrry large asteroid to have the energy for antipodal focussing to result in volcanism. the crater under the ice in Antartica suspected of initiating the Siberian flood basalts is on the order of 300 miles across. :doh: :phones: :) >> Meteor Impact Crater Discovered Under Antarctic Ice

i say Winston! :hihi:

 

Link to comment
Share on other sites

Join the conversation

You can post now and register later. If you have an account, sign in now to post with your account.

Guest
Reply to this topic...

×   Pasted as rich text.   Paste as plain text instead

  Only 75 emoji are allowed.

×   Your link has been automatically embedded.   Display as a link instead

×   Your previous content has been restored.   Clear editor

×   You cannot paste images directly. Upload or insert images from URL.

Loading...
×
×
  • Create New...