RussCheshire, to Scotland
@RussCheshire@mastodon.scot avatar

North Britain Palaeogene Dyke Suite (Arran Tertiary Dyke Swarm) (66 - 23.03 mya) cutting through Auchenhew Mudstone Formation (252.2 - 237 mya). On the horizon, Ailsa Craig - an igneous pluton also dating from the Palaeogene period.

#Arran #Scotland #Geology #Geomorphology

RebelGeo, to Geology
@RebelGeo@mastodon.social avatar
RussCheshire, to Scotland
@RussCheshire@mastodon.scot avatar

Metamorphic rocks eroded by abrasion and water, Claonaig shore.

#Argyll #Scotland #Geology #Geomorphology

maitri, to science
@maitri@c.im avatar

It occurs to me that, since the demise of Twitter and the half-hearted move to Mastodon, most of my communication on social media is only with people I know. My brain is currently actively calculating if this is a good or a bad thing.

I do miss old Science Twitter, however. Is that still a thing here or elsewhere in another form? Is everyone partying without me? Leads welcomed.

lucvantilborgh,
@lucvantilborgh@mastodon-belgium.be avatar

@maitri
Following hashtags is a way of connecting here. Some tags that might interest you...

mattotcha, to random
@mattotcha@mastodon.social avatar
studiohaverstraat, to Geology
@studiohaverstraat@mapstodon.space avatar

I don't know if #meandermonday is a thing, otherwise we could start it. This is meandering Sandelva near Fredvang, Moskenesøya, Norway. #meander #geology #geomorphology #norway #lofoten

mrutzinger, to geopolitics German
GregCocks, to Geology
@GregCocks@techhub.social avatar

Major Fluvial Erosion And A 500-Mt Sediment Pulse Triggered By Lava-Dam Failure, Río Coca, Ecuador

https://doi.org/10.1002/esp.5751 <-- shared paper

photos - Former location of the Cascada San Rafael lava-dam waterfall and knickpoint on the Río Coca, viewed facing upstream. (a) Pre-collapse morphology of the waterfall, in 2012 (image from Ecuador Ministry of Tourism). Accommodation space upstream of the lava dam was filled with sediment. (b) The site was on 2 February 2020, shortly after a sinkhole (upstream of lava dam) captured the river. Dashed line shows the approximate location of the unconformable contact between the lava flow and underlying volcaniclastic avalanche deposits. (c) The site was on 22 February 2021 during the incipient collapse of the remaining arched edifice of the lava flow. (d) Later on 22 February 2021 after full collapse of the lava arch. (e) The site on 25 February 2021, shortly after the river overtopped and eroded through the debris dam. Photographs in (b) through (e) provided by the Corporacion Electrica del Ecuador.
map and chart - (a) Detailed map of the study reach (shown within box in Figure 1a), with river kilometres (rkm) shown referring to distance downstream of the Coca Codo Sinclair (CCS) dam and diversion intake. (b) Subsurface geologic cross-section of the study reached from rkm 0 to 22 (annotated using field observations of the authors and borehole information from INECEL [Instituto Ecuatoriano de Electrificacion], 1992). Dashed line shows the riverbed profile as of 2 December 2022, 1,034 days after the failure of the Cascada San Rafael knickpoint. Prior to the loss of the knickpoint in February 2020, the accommodation space upstream of the Cascada San Rafael had entirely filled with sediment. Geologic units are abbreviated as volcaniclastic breccia (Br), cohesive volcaniclastic avalanche deposits (CoAv), loose volcaniclastic avalanche deposits (LoAv), ancient alluvial deposits (All), lacustrine sediments (Lac), debris-flow deposits (Deb, a thin deposit around rkm 8–8.5). Lava flow, recent alluvial deposits and Mesozoic bedrock are also shown.
photo - waterfall, Río Coca, Ecuador before failure & erosion

Andbaker, to science
@Andbaker@aus.social avatar

Are you at an Australian beach or walking the coastline? Can you help collect citizen science data by taking a photo with your smartphone?

I'm sharing this article in the @theconversationau on behalf of my UNSW colleague Mitch Harley of CoastSnap fame.

"Become a beach scientist this summer and help monitor changing coastlines"
https://theconversation.com/become-a-beach-scientist-this-summer-and-help-monitor-changing-coastlines-214307

Andbaker, to science
@Andbaker@aus.social avatar

Are you at an Australian beach or walking the coastline? Can you help collect citizen science data by taking a photo with your smartphone.

I'm sharing this article in the @theconversationau on behalf of my UNSW colleague Mitch Harley of CoastSnap fame.

"Become a beach scientist this summer and help monitor changing coastlines"
https://theconversation.com/become-a-beach-scientist-this-summer-and-help-monitor-changing-coastlines-214307

RebelGeo, to random
@RebelGeo@mastodon.social avatar
GregCocks, (edited ) to Archaeology
@GregCocks@techhub.social avatar
GregCocks, to geopolitics
@GregCocks@techhub.social avatar

The Ural Mountains [geology / remote sensing]

https://earthobservatory.nasa.gov/images/87198/the-ural-mountains <-- shared technical article

[(1) I am currently reading the Russia chapter of Tim Marshall’s book, “Prisoners Of Geography”, he explains - amongst many other things - how the Ural’s play SUCH an important part in the areas geopolitics and ‘military’ history, and (2) geology reflected in hydrology, fluvial and geomorphology is a specific technical interest of mine, especially with the now readily availability of remote sensing data]

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GregCocks, to Geology
@GregCocks@techhub.social avatar
GregCocks, to geopolitics
@GregCocks@techhub.social avatar
niklas, to Geology
@niklas@niklas.social avatar

One of my favourite EO places on Earth: Yana river in Siberia! Look at this meandering giant. You can observe many geomorphic features here, like depositions, oxbow lakes, scars, cut-offs, etc. You can look into centuries of history here…

mrutzinger, to random German

Quantifying slope movements: Tree trunk tracking using long-range stationary 4D laser scanning point clouds

archeaids, to random
@archeaids@mastodon.online avatar

Annotated. There's a 52.5 ft difference between the Pleistocene high points & the river. You can see dissection of the uplands (lower left). The lateral channel migrations are tricky. The lower 1 is transitioning to a point bar migration, with the other 2 close behind.

archeaids, to random
@archeaids@mastodon.online avatar

A lot of movement by Bayou Macon since it occupied the old Red River course. Not sure what is going on top center (red). There's a 13' change. It looks to me like the area between there & the west side might have been an old Pleistocene channel.

archeaids, to random
@archeaids@mastodon.online avatar

Saucier (1994, Plate 9) shows the area as (Pve 4) Pleistocene Early Wisconsin age valley trains, (Hpa 4) Red River point bar & meander deposits, & (Hb) backswamp.

archeaids, to random
@archeaids@mastodon.online avatar

3D LiDAR of part of the Crowville, LA, quad showing Pleistocene uplands & Holocene lowlands. The valley, now occupied by Bayou Macon, once was point bars & meanders of the Red River, & exhibit classic meander scars & dynamics. Note the meander abutting the Pleistocene.

pomarede, to space
@pomarede@mastodon.social avatar
pomarede,
@pomarede@mastodon.social avatar

Check out this jaw-dropping cover of the Nature Journal published in 2011

Europa's Great Lakes - Watery origins for surface chaos on Jupiter's icy moon

Credit image: Britney E. Schmidt & Deadpixel VFX/Jackson School of Geosciences/UTIG/Vetlesen Foundation/NASA.

https://nature.com/nature/volumes/479/issues/7374

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