Anne Elliott's photos with the keyword: badlands

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

This is what the weather was like on 15 July 2012, when five of us took a long drive NE of Calgary, to spend a few hours botanizing at Dry Island Buffalo Jump Provincial Park! The day started off overcast, then turned to drizzle, which then turned into non-stop rain. There is a gate at the top of this area, which is closed when it has been, or is raining, as everywhere turns into one slippery surface. Bentonite, ancient volcanic clay ash, is prolific, and when it gets wet, it becomes very, very slippery and treacherous. Our feet slid on the surface of the gravel road that we had to walk on, and we weren't able to leave the path to explore. The gate at the top was unfortunately closed, so we had to walk all the way down to the floor of the badlands - which meant, of course, that the return walk was all uphill, which I never do well with. I'm always so thankful for very patient friends! By the time we reached the bottom, the rain was heavy and after just a few minutes, I was soaked to the skin and remained that way for the rest of the day, ha. "Dry Island Buffalo Jump is so-named because of a flat-topped mesa called a "dry island" that rises 200 metres above the Red Deer River. In the distance you can see the grassy cliff-top of an ancient buffalo jump. Cree Indians hunted bison here by stampeding them over the high cliffs, providing enough meat, skins and other products to sustain them. The park is a mix of badlands and riparian forests where cacti and other plants typical of Alberta's grasslands are found in proximity to species normally associated with the Boreal Forest Natural Region. Prairie falcons nest on cliff faces in the park. Due to the high content of bentonite (a clay-like material) roads and trails in this area can become very slippery when wet, sometimes making them unsafe or impassable for both vehicle and foot traffic. As a result, the access road from the viewpoint to the park's day use area is often closed during wet conditions." albertaparks.ca/dry-island-buffalo-jump.aspx

This is what the weather was like on 15 July 2012, when five of us took a long drive NE of Calgary, to spend a few hours botanizing at Dry Island Buffalo Jump Provincial Park! The day started off overcast, then turned to drizzle, which then turned into non-stop rain. There is a gate at the top of this area, which is closed when it has been, or is raining, as everywhere turns into one slippery surface. Bentonite, ancient volcanic clay ash, is prolific, and when it gets wet, it becomes very, very slippery and treacherous. Our feet slid on the surface of the gravel road that we had to walk on, and we weren't able to leave the path to explore. The gate at the top was unfortunately closed, so we had to walk all the way down to the floor of the badlands - which meant, of course, that the return walk was all uphill, which I never do well with. I'm always so thankful for very patient friends! By the time we reached the bottom, the rain was heavy and after just a few minutes, I was soaked to the skin and remained that way for the rest of the day, ha. "Dry Island Buffalo Jump is so-named because of a flat-topped mesa called a "dry island" that rises 200 metres above the Red Deer River. In the distance you can see the grassy cliff-top of an ancient buffalo jump. Cree Indians hunted bison here by stampeding them over the high cliffs, providing enough meat, skins and other products to sustain them. The park is a mix of badlands and riparian forests where cacti and other plants typical of Alberta's grasslands are found in proximity to species normally associated with the Boreal Forest Natural Region. Prairie falcons nest on cliff faces in the park. Due to the high content of bentonite (a clay-like material) roads and trails in this area can become very slippery when wet, sometimes making them unsafe or impassable for both vehicle and foot traffic. As a result, the access road from the viewpoint to the park's day use area is often closed during wet conditions." albertaparks.ca/dry-island-buffalo-jump.aspx

This is what the weather was like on Sunday 15 July, when five of us took a long drive NE of Calgary, to spend a few hours botanizing at Dry Island Buffalo Jump Provincial Park! The day started off overcast, then turned to drizzle, which then turned into non-stop rain. There is a gate at the top of this area, which is closed when it has been, or is raining, as everywhere turns into one slippery surface. Bentonite, ancient volcanic clay ash, is prolific, and when it gets wet, it becomes very, very slippery and treacherous. Our feet slid on the surface of the gravel road that we had to walk on, and we weren't able to leave the path to explore. Yesterday, the gate at the top was unfortunately closed, so we had to walk all the way down to the floor of the badlands - which meant, of course, that the return walk was all uphill, which I never do well with. I'm always so thankful for very patient friends! By the time we reached the bottom, the rain was heavy and after just a few minutes, I was soaked to the skin and remained that way for the rest of the day, ha. Thanks so much, Sandy, for introducing us to a new, fascinating area of Alberta and for the ride - made a great day, despite the rain! "Dry Island Buffalo Jump is so-named because of a flat-topped mesa called a "dry island" that rises 200 metres above the Red Deer River. In the distance you can see the grassy cliff-top of an ancient buffalo jump. Cree Indians hunted bison here by stampeding them over the high cliffs, providing enough meat, skins and other products to sustain them. The park is a mix of badlands and riparian forests where cacti and other plants typical of Alberta's grasslands are found in proximity to species normally associated with the Boreal Forest Natural Region. Prairie falcons nest on cliff faces in the park. Due to the high content of bentonite (a clay-like material) roads and trails in this area can become very slippery when wet, sometimes making them unsafe or impassable for both vehicle and foot traffic. As a result, the access road from the viewpoint to the park's day use area is often closed during wet conditions." albertaparks.ca/dry-island-buffalo-jump.aspx Art (Leapfrog!) - wish I could send you a few days of this cool, rainy weather!