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No photo I have better shows off the Fraser River canyon than this one. 713 leads a super long southbound at Fountain, north of Lillooet.
My interview on Google Local Guide Connect
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this is another shot from yesterday's outing after my vist to corby crags i headed to the coast, with the tide being out i decided to go to holy island. the shot is of lindisfarne castle. the castle was built in the 16th century on top of a volcanic mound known as beblowe crag. thank you for taking the time to look. christian island gordon lightfoot
Hello everyone, I would like to invite you to subscribe to my new Instagram page, exclusively for photos, thank you very much, the profile name is Instagram: @guilhermeLeibantefoto
Sleat,heavy snow and rain ...that's Ogwen Valley for you . I adore this place ! So lovely to return xxx
Okrešelj (1400 m), Kamniško-Savinjske Alpe, Slovenija / Okrešelj (1400 m), Kamnik-Savinja Alps, Slovenia
pogled na Planjavu (2394 m), Kamniško sedlo (1864 m), Branu (2253 m) i Tursku goru (2251 m) u oblacima iz ledenjačkog amfiteatra Okrešlja / view towards Planjava (2394 m), Kamniško sedlo (1864 m), Brana (2253 m) and Turska gora (2251 m) in clouds from the glacial cirque Okrešelj
Think of all the beauty still left around you and be happy. -
Anne Frank
Thank you for your kind visit. Have a wonderful and beautiful day! xo💜💜
Blacktail Ponds Overlook is just off Hwy 89 about 20 miles north of Jackson, Wyoming....and in the morning hour it is a beautiful place to take in the majesty of nature.
A yardang is a streamlined protuberance carved from bedrock or any consolidated or semiconsolidated material by the dual action of wind abrasion by dust and sand, and deflation which is the removal of loose material by wind turbulence. Yardangs become elongated features typically three or more times longer than wide, and when viewed from above, resemble the hull of a boat. Facing the wind is a steep, blunt face that gradually gets lower and narrower toward the lee end.[2] Yardangs are formed by wind erosion, typically of an originally flat surface formed from areas of harder and softer material. The soft material is eroded and removed by the wind, and the harder material remains. The resulting pattern of yardangs is therefore a combination of the original rock distribution, and the fluid mechanics of the air flow and resulting pattern of erosion.