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User / annkelliott / Sets / Red Rock Coulee, Alberta
Anne Elliott / 14 items

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Another landscape photo taken at Red Rock Coulee in SE Alberta. We left Calgary on Monday morning, 20 September 2013, and had to reach Elkwater in the Cypress Hills (not that far from the Saskatchewan border), several hours' drive away, where we were going to stay in a little rustic cabin for three nights. On the way there, we stopped at Red Rock Coulee, which is just 56 kms (35 mi) southwest of Medicine Hat. Actually, this particular photo was taken on Monday, 23 September 2013, when we called in again, this time walking down the hillside and into one of the coulees. While my friends searched for Lichens, I wandered around, taking photos of the scenery and anything else I came across. While we were down there, the sky had filled with some rather nice clouds, which I appreciated. However, the extremely high winds were not pleasant at all, to say the least! In fact, strong winds were everywhere in many parts of SE Alberta. I was expecting a lot of my photos to be very blurry, as I could barely keep my balance or hold my camera. Amazingly, most seem to be OK to use, from the very quick look I've taken so far. This is Rattlesnake territory, too, but fortunately we didn't come across any, thank goodness! At least, not here, but one was seen (not by me!) at the Pinhorn Grazing Lease, when we were monitoring the Yucca plants.

"The main feature of this natural landscape is the huge red boulders; some measuring 2.5 m across. They are scattered over a relatively small distance. Bedrock is close to the surface in this area, covered by only a thin layer of soil. Water erosion has carved the landscape over time and a badlands topography has formed in places. The bands of colour visible in the exposed bedrock are made of dark gray shales, greenish and gray sandstones, bentonitic clays and thin bands of ironstone.

The most striking features of this landscape are the round reddish boulders. These are sandstone concretions and at up to 2.5 m in diameter, they are among the largest in the world. The boulders were formed in prehistoric seas as layers of sand, calcite and iron oxide collected around a nucleus formed by shells, leaves or bones. The concretions grew larger as the circulating waters deposited more layers. The reddish colour comes from iron oxide." From Wikipedia.

en.wikipedia.org/wiki/Red_Rock_Coulee

N 14 B 6.4K C 18 E Sep 23, 2013 F Oct 1, 2013
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Another landscape photo taken at Red Rock Coulee in SE Alberta. We left Calgary on Monday morning, 20 September 2013, and had to reach Elkwater in the Cypress Hills (not that far from the Saskatchewan border), several hours' drive away, where we were going to stay in a little rustic cabin for three nights. On the way there, we stopped at Red Rock Coulee, which is just 56 kms (35 mi) southwest of Medicine Hat. Actually, this particular photo was taken on Monday, 23 September 2013, when we called in again, this time walking down the hillside and into one of the coulees. While my friends searched for Lichens, I wandered around, taking photos of the scenery and anything else I came across. These eroded, layered hills are similar to some of those seen in places like Drumheller and DInosaur Provincial Park. The extremely high winds were not pleasant at all, to say the least! In fact, strong winds were everywhere in many parts of SE Alberta. I was expecting a lot of my photos to be very blurry, as I could barely keep my balance or hold my camera. Amazingly, most seem to be OK to use, from the very quick look I've taken so far. This is Rattlesnake territory, too, but fortunately we didn't come across any, thank goodness! At least, not here, but one was seen (not by me!) at the Pinhorn Grazing Lease, when we were monitoring the Yucca plants.

"The main feature of this natural landscape is the huge red boulders; some measuring 2.5 m across. They are scattered over a relatively small distance. Bedrock is close to the surface in this area, covered by only a thin layer of soil. Water erosion has carved the landscape over time and a badlands topography has formed in places. The bands of colour visible in the exposed bedrock are made of dark gray shales, greenish and gray sandstones, bentonitic clays and thin bands of ironstone.

The most striking features of this landscape are the round reddish boulders. These are sandstone concretions and at up to 2.5 m in diameter, they are among the largest in the world. The boulders were formed in prehistoric seas as layers of sand, calcite and iron oxide collected around a nucleus formed by shells, leaves or bones. The concretions grew larger as the circulating waters deposited more layers. The reddish colour comes from iron oxide." From Wikipedia.

en.wikipedia.org/wiki/Red_Rock_Coulee

Something's wrong with Flickr (at least for me) today. This morning and this evening, I can't see any photos - mine or others. All the descriptions, comments, tags are visible, just no image.

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Tags:   Alberta Canada SE Alberta Red Rock Coulee nature landscape scenery unique rock layers erosion pattern texture bushes geology shale sandstone bentonitic clay ironstone

N 17 B 6.5K C 17 E Sep 23, 2013 F Sep 27, 2013
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Another landscape photo taken at Red Rock Coulee in SE Alberta. We left Calgary on Monday morning, 20 September 2013, and had to reach Elkwater in the Cypress Hills (not that far from the Saskatchewan border), several hours' drive away, where we were going to stay in a little rustic cabin for three nights. On the way there, we stopped at Red Rock Coulee, which is just 56 kms (35 mi) southwest of Medicine Hat. Actually, this particular photo was taken on Monday, 23 September 2013, when we called in again, this time walking down the hillside and into one of the coulees. While my friends searched for Lichens, I wandered around, taking photos of the scenery and anything else I came across. While we were down there, the sky had filled with some rather nice clouds, which I appreciated. However, the extremely high winds were not pleasant at all, to say the least! In fact, strong winds were everywhere in many parts of SE Alberta. I was expecting a lot of my photos to be very blurry, as I could barely keep my balance or hold my camera. Amazingly, most seem to be OK to use, from the very quick look I've taken so far. This is Rattlesnake territory, too, but fortunately we didn't come across any, thank goodness! At least, not here, but one was seen (not by me!) at the Pinhorn Grazing Lease, when we were monitoring the Yucca plants.

"The main feature of this natural landscape is the huge red boulders; some measuring 2.5 m across. They are scattered over a relatively small distance. Bedrock is close to the surface in this area, covered by only a thin layer of soil. Water erosion has carved the landscape over time and a badlands topography has formed in places. The bands of colour visible in the exposed bedrock are made of dark gray shales, greenish and gray sandstones, bentonitic clays and thin bands of ironstone.

The most striking features of this landscape are the round reddish boulders. These are sandstone concretions and at up to 2.5 m in diameter, they are among the largest in the world. The boulders were formed in prehistoric seas as layers of sand, calcite and iron oxide collected around a nucleus formed by shells, leaves or bones. The concretions grew larger as the circulating waters deposited more layers. The reddish colour comes from iron oxide." From Wikipedia.

en.wikipedia.org/wiki/Red_Rock_Coulee

Tags:   Alberta Canada SE Alberta Red Rock Coulee nature landscape scenery unique concretions reddish boulders sandstone up to 2.5 metres in diameter iron oxide round geology beauty in nature

N 3 B 1.8K C 7 E Sep 23, 2013 F Sep 26, 2013
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A photo I needed to add to my SE Alberta trip album. Wish I was able to ID Lichens, but eventually I will be able to get the names from the two friends I went with on the road trip. I know the red Lichen proved to be of interest to them. I wonder how many people take a closer look at the splashes of colour on rocks - lichens really are quite fascinating and beautiful : ) Taken on 23 September 2013, down one of the coulees at Red Rock Coulee.

ID, thanks to specialists Janet Marsh and Sandra Davis: Parasite Caloplaca epithallina growing on crust lichen & the surrounding lichen is Rhizoplaca melanophthalma.

Tags:   lichen Parasite Caloplaca epithallina growing on crust lichen Rhizoplaca melanophthalma

N 38 B 12.1K C 27 E Sep 23, 2013 F Sep 24, 2013
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Got home around 7:45 p.m. yesterday evening (Monday, 23 September 2013) from an amazing four day (three night) road trip down to SE Alberta with two friends. Our furthest destination was Elkwater in the Cypress Hills, but we did a lot of driving all over the SE part of the province. All new territory to me, so I was extremely lucky to get this chance. Both friends had been to this area before, but wanted to go back to see if they could add any new species of Lichen to those already on various lists for each area, and to simply explore this beautiful section on Alberta. Always exciting to see some new things, not to mention all new scenery for me : ) Was really concerned before we went, though, as I had been on antibiotics (which, normally, I never take) for the previous nine days and they were making me feel nauseous and generally sick, and I wasn't sure how I was going to manage the trip. Had to forget the last day of pills, as apart from the nausea, another side-effect was reddening of the skin, and my poor legs looked like they had suffered burns! Think they have also affected my eyes, too, which is really troubling. So thankful I still managed! What I would have missed! Now, of course, I have so many images to sort through and edit so that they can be passed on to various people, including some to Medicine Hat College.

We left Calgary on Monday morning, 20 September 2013, and had to reach Elkwater in the Cypress Hills (not that far from the Saskatchewan border), several hours' drive away, where we were going to stay in a little rustic cabin for three nights. On the way there, we stopped at Red Rock Coulee, and you can see just a tiny bit in my photo above. Actually, this particular photo was taken yesterday, Monday 23 September 2013, when we called in again, this time walking down the hillside and into one of the coulees. While my friends searched for Lichens, I wandered around, taking photos of the scenery and anything else I came across. While we were down there, the sky had filled with some rather nice clouds, which I appreciated. However, the extremely high winds were not pleasant at all, to say the least! In fact, strong winds were everywhere in many parts of SE Alberta. I was expecting a lot of my photos to be blurry, as I could barely keep my balance or hold my camera. Amazingly, most seem to be OK, from the very quick look I've taken so far. This is Rattlesnake territory, too, but fortunately we didn't come across any!

"The main feature of this natural landscape is the huge red boulders; some measuring 2.5 m across. They are scattered over a relatively small distance. Bedrock is close to the surface in this area, covered by only a thin layer of soil. Water erosion has carved the landscape over time and a badlands topography has formed in places. The bands of colour visible in the exposed bedrock are made of dark gray shales, greenish and gray sandstones, bentonitic clays and thin bands of ironstone.

The most striking features of this landscape are the round reddish boulders. These are sandstone concretions and at up to 2.5 m in diameter, they are among the largest in the world. The boulders were formed in prehistoric seas as layers of sand, calcite and iron oxide collected around a nucleus formed by shells, leaves or bones. The concretions grew larger as the circulating waters deposited more layers. The reddish colour comes from iron oxide." From Wikipedia.

en.wikipedia.org/wiki/Red_Rock_Coulee

Tags:   Alberta Canada SE Alberta Red Rock Coulee nature landscape scenery unique concretions reddish boulders sandstone up to 2.5 metres in diameter iron oxide round Explore interestingness# explore2013September25 Geology


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