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Another timelapse looking over Lake Ontario from my back yard as the storm rolls out. I love the "popcorn clouds!" (the ones that start out as a little puff of vapour then grow into giant fluff balls... they're near the end of the video) The music is a remix I did of "A Drowning" by How to Destroy Angels. (I stretched out the end so the music ended less abruptly as it is only part of the song)
Trying to find the beauty in the breakup. (Breakup is the ugly thing that happens after you've had snow in Alaska all winter & then it begins to thaw.) Took a walk around the yard with the 12-year old to find some life & color.
Taken in spring 2009 right after the breakup. I'm sure I have some other photos from this time somewhere in my files. It was a bit more of a physical breakup this year, with all the pieces coming up onto MacDonald Island from the Athabasca River. It was amazing to walk around it and see all the large chunks of ice on the shore.
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Disappointments are very hard to explain. It comprises of the things that you thought would happen but didn’t. The things that you expected to realize, but didn’t. Those are the many disappointments of life. You think as if you are in control, but you’re not. You set your...
Pesée de Figo avant embarquation dans un CASA de l'armée de l'Air à destination de MARIPASOULA dans le cadre de l'opération ALATALE NUI.
French Armed Forces and Gendarmerie during a joint operation against illegal mining 150 km southwest of Cayenne in the Dorlin area of French Guiana – The operation was intended to secure the area and breakup the illegal mining camps, over 150 Soldiers and Gendarmerie took part in the operations deploying from the 9e Régiment d’infanterie de marine (9e RIMa) base of camp Lunier – 11th July 2012
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Shania on Oprah talking about the breakup of her marriage and Mutt's betrayal. And about her new book "From this Moment On"
And this is where it broke down the third time! This photo presages my second least-favourite moment of the trip, where we were all packed into a single canoe, and I had no legroom and both feet trapped under the seat in front, so I couldn't move them at all for over an hour.
(If you're wondering, the first least-favourite moment was going to the loo later the same night, after someone discovered a 4-inch monkey spider living in one of the cubicles.)
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Channel sandstone in the Triassic of North Carolina, USA.
The Newark Supergroup is a thick, geographically-widespread stratigraphic unit in eastern America. It is Late Triassic to Early Jurassic in age and represents sediments and some lava flows that filled up old rift valleys roughly paralleling the modern-day Eastern Seaboard of America. The rift basins formed in the Triassic when the ancient Pangaea supercontinent attempted to break apart, but failed. A successful breakup of Pangaea occurred during the Jurassic. Most of the basin-filling rocks are terrestrial redbeds - hematite-rich siliciclastic sedimentary rocks, such as conglomerate, sandstone, siltstone, and shale, deposited in nonmarine environments.
Seen here is a sandstone outcrop along the shores of Jordan Lake, a manmade reservoir in North Carolina. In Triassic rift basin terminology, this is part of the Durham Sub-Basin of the Deep River Basin. The sedimentary rocks of this area were originally dismissed as "undifferentiated Triassic". Droughts and low water levels have exposed novel outcrops along Jordan Lake's shoreline. No formation names are available, but the rocks are part of the Chatham Group. The stratigraphic terminology used in the nearby Sanford Sub-Basin is too simple, so "lithofacies association" terminology is used instead in the Durham Sub-Basin.
The rocks here are part of "lithofacies association 2", which consists of coarser-grained arkosic, micaceous sandstones with reddish-colored finer-grained sediments on top (the latter are not visible here). Some sandstones here have what appear to be fossil bone fragments, but they are really corroded basement clasts.
"Arkosic" refers to the common presence of potassium feldspar sediment grains. These rocks are also fairly rich in biotite mica. The sand is "immature", which generally refers to sedimentary deposits that have a high clay content, are poorly sorted, have many non-quartz minerals, and angular to subangular grain shapes.
Stratigraphy: Chatham Group, Newark Supergroup, Carnian to Norian Stages, Upper Triassic
Locality: shoreline outcrop along the eastern side of Jordan Lake, a little north of the Jordan Lake visitor center & south of Route 65 & west-southwest of Wilsonville, eastern Chatham County, central North Carolina, USA (35° 44’ 04.20” North latitude, 79° 01’ 07.03” West longitude)
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