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Once the Shoshone River exits Rattlesnake Mountain into the Big Horn Basin at Cody the river remains in a canyon that has the Cody bench (river terrace) on both sides. An angular unconformity between the Quaternary Cody Terrace Gravels and the red Triassic Chugwater Formation is exposed in the bend of the river on the canyon wall in the center of the image. The Cody Rodeo Arena can be seen on the Cody Bench just behind the exposed unconformity.
Geologically, an unconformity is an erosional or non-depositional surface separating two rock masses or strata of different ages, indicating that sediment deposition was not continuous. In other words, an unconformity indicates that 1- the older rock layer was exposed to erosion for an interval of time before deposition of the younger; 2- there was a period of non-deposition between the time the 2 sediment layers were deposited at least at that location or 3- a combination of both. An angular unconformity is an unconformity where horizontally parallel strata of sedimentary rock are deposited on tilted and eroded layers, producing an angular discordance with the overlying layers. This indicates that the older beds were titled or deformed tectonically, then truncated by erosion, before the younger beds were deposited. The entire package can be subsequently deformed after deposition of the younger beds so they are no longer parallel but the discordance with the older beds still remains. Generally, development of an unconformity is accompanied by or preceded by uplift of the rock units or strata that will be eroded, and/or the fall of relative sea level, thus exposing rock units or strata to erosion. The presence of an unconformity indicates a gap or vacuity in the chronostratigraphic record.
The rocks visible in the foreground from front to back are shales; limestone and cherts on the Permian Park City Formation (also known as the Phosphoria Formation), and the tan sandstones of the Pennsylvanian Tensleep Formation. On top of the cliffs both to the left and the right in the foreground are topped with Quaternary Travertine Deposits that are part of the Colter's Hell (Also know as the Demaris or Cody) hydrothermal (hot springs) area.
One of the world’s biggest Angular conference.
The beautiful city of Warsaw, amazing national stadium, 2 days, 15 talks, 5 workshops, Q&A session and much more!
Thank you to our wonderfull sponsors: Acaicoft, 7N, Twilio, SoftwareMill, SoftwarePlant, EDC Aviation Digital, Deloitte, CodiLime, Telerik, JetBrains, DataArt Poland. Thank you for the speakers, we are really appreciate that you came to Poland and share your knowledge! Thank you for communities from all over the world for your support. Thank you for ALL attendees!
The late afternoon sun caught my eye on the city council building highlinghting the 7 flashes of yellow features.
This is SOOC and just a lift on the midtones for the shadows on the RHS.
Numerically Odd Theme
Parallel Lines Challenge
One of the world’s biggest Angular conference.
The beautiful city of Warsaw, amazing national stadium, 2 days, 15 talks, 5 workshops, Q&A session and much more!
Thank you to our wonderfull sponsors: Acaicoft, 7N, Twilio, SoftwareMill, SoftwarePlant, EDC Aviation Digital, Deloitte, CodiLime, Telerik, JetBrains, DataArt Poland. Thank you for the speakers, we are really appreciate that you came to Poland and share your knowledge! Thank you for communities from all over the world for your support. Thank you for ALL attendees!
One of the world’s biggest Angular conference.
The beautiful city of Warsaw, amazing national stadium, 2 days, 15 talks, 5 workshops, Q&A session and much more!
Thank you to our wonderfull sponsors: Acaicoft, 7N, Twilio, SoftwareMill, SoftwarePlant, EDC Aviation Digital, Deloitte, CodiLime, Telerik, JetBrains, DataArt Poland. Thank you for the speakers, we are really appreciate that you came to Poland and share your knowledge! Thank you for communities from all over the world for your support. Thank you for ALL attendees!
for theme of the week "angularity".....taken at a family gathering to celebrate my brother and dad's birthdays, the inside of my brothers radiator !!
still getting to grips with the fuji....
One of the world’s biggest Angular conference.
The beautiful city of Warsaw, amazing national stadium, 2 days, 15 talks, 5 workshops, Q&A session and much more!
Thank you to our wonderfull sponsors: Acaicoft, 7N, Twilio, SoftwareMill, SoftwarePlant, EDC Aviation Digital, Deloitte, CodiLime, Telerik, JetBrains, DataArt Poland. Thank you for the speakers, we are really appreciate that you came to Poland and share your knowledge! Thank you for communities from all over the world for your support. Thank you for ALL attendees!
de la KDD del passat diumenge mentre xerràvem i provaba l'angular d'en Sergio,
la casualitat em va portar al lloc més monumental del barri vell de Girona, van ser uns minuts molt intensos i breus!
durante la KDD del domingo pasado, probando el angular de Sergio, en el sitio más monumental del barrio antiguo de Girona,
fueron unos minutos intensos y breves
Click 'L' please. :)
From my last trip to Detroit. Have a few I may post over the next few weeks now that I know which ones will not be in the show. Friday Fave mosaic coming later!
Annotations
Geological Features
A - angular unconformity
B - fault
Stratigraphy
1 - Quaternary Travertine: hot springs deposits
2a - Quaternary Unconsolidated Recent Terrace Gravels (includes sand silt and cobbles)
2b - Cody Terrace (Bench) Deposits (gravel, sand; cobbles; silt and calcareous cement)
3 - Eocene Willwood Formation: seen in this image on the distant horizon.
4- Triassic Chugwater formation: red siltstone, shale and fine-grained sandstone
5- Triassic Dinwoody Formation: tan to dark red shale, gypsum and thin-bedded limestones and dolomites
6- Permian Park City Formation (also called Phosphoria): light gray to black shales, limestones, dolomites and chert nodules.
7-Pennsylvian Tensleep Sandstone with thin interbeds of limestone and dolomites at the base
Once the Shoshone River exits Rattlesnake Mountain into the Big Horn Basin at Cody the river remains in a canyon that has the Cody bench (river terrace) on both sides. An angular unconformity between the Quaternary Cody Terrace Gravels and the red Triassic Chugwater Formation is exposed in the bend of the river on the canyon wall in the center of the image. The Cody Rodeo Arena can be seen on the Cody Bench just behind the exposed unconformity.
Geologically, an unconformity is an erosional or non-depositional surface separating two rock masses or strata of different ages, indicating that sediment deposition was not continuous. In other words, an unconformity indicates that 1- the older rock layer was exposed to erosion for an interval of time before deposition of the younger; 2- there was a period of non-deposition between the time the 2 sediment layers were deposited at least at that location or 3- a combination of both. An angular unconformity is an unconformity where horizontally parallel strata of sedimentary rock are deposited on tilted and eroded layers, producing an angular discordance with the overlying layers. This indicates that the older beds were titled or deformed tectonically, then truncated by erosion, before the younger beds were deposited. The entire package can be subsequently deformed after deposition of the younger beds so they are no longer parallel but the discordance with the older beds still remains.
Generally, development of an unconformity is accompanied by or preceded by uplift of the rock units or strata that will be eroded, and/or the fall of relative sea level, thus exposing rock units or strata to erosion. The presence of an unconformity indicates a gap or vacuity in the chronostratigraphic record.
The rocks visible in the foreground from front to back are shales; limestone and cherts on the Permian Park City Formation (also known as the Phosphoria Formation), and the tan sandstones of the Pennsylvanian Tensleep Formation. On top of the cliffs both to the left and the right in the foreground are topped with Quaternary Travertine Deposits that are part of the Colter's Hell (Also know as the Demaris or Cody) hydrothermal (hot springs) area.
Showroom
Crta. Santiago-Pontevedra a 9 Km. de Santiago de Compostela en dirección a Pontevedra. 15.866 Ameneiro-Teo (La Coruña) España.
Como eu havia prometido :)
Essa eu tirei pra Bianca, em homenagem a todos desprovidos de uma grande angular e que tem que se virar em chaleira, bola de engate de carro, espelho de elevador, etc.
A minha ficou no chinelo da dela, mas fiz o que pude. hehe
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Crta. Santiago-Pontevedra a 9 Km. de Santiago de Compostela en dirección a Pontevedra. 15.866 Ameneiro-Teo (La Coruña) España.
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Crta. Santiago-Pontevedra a 9 Km. de Santiago de Compostela en dirección a Pontevedra. 15.866 Ameneiro-Teo (La Coruña) España.
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Crta. Santiago-Pontevedra a 9 Km. de Santiago de Compostela en dirección a Pontevedra. 15.866 Ameneiro-Teo (La Coruña) España.
Showroom
Crta. Santiago-Pontevedra a 9 Km. de Santiago de Compostela en dirección a Pontevedra. 15.866 Ameneiro-Teo (La Coruña) España.
Showroom
Crta. Santiago-Pontevedra a 9 Km. de Santiago de Compostela en dirección a Pontevedra. 15.866 Ameneiro-Teo (La Coruña) España.
To see these in stereo, use the cross-eyed technique.
The highly inclined sedimentary rock units are part of the Twist Gulch Formation of Middle Jurassic age. They consist of fairly friable siltstones and fine grained sandstones. Laying unconformably on top of the Twist Gulch Formation are the lighter horizontal beds of the Mid-Paleocene Flagstaff Formation. These light colored beds are primarily sandstones.
Above the Flagstaff formation lie the Colton Formation, and the Green River Formation (upper Paleocene to Eocene).
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Crta. Santiago-Pontevedra a 9 Km. de Santiago de Compostela en dirección a Pontevedra. 15.866 Ameneiro-Teo (La Coruña) España.
GP-9 7554, in the service of the Penn Central Railroad, soaks up some sunshine in the New Haven engine yard, 1971.