Guest
A walk in leavenworth located in the Cascade Mountains, in central Washington State. We can feel a little piece of Old Germany here. It was the perfect timing to see autumn foliage so let's see it together! This 4K 60fps video was taken with iPhone 11 Pro. You can see beautiful another autumn foliage walk here!! 【Autumn Foliage series】 VanDusen Botanical Garden, Vancouver Yaletown, Vancouver -- Leavenworth, Washington Leavenworth is a city in Chelan County, Washington, United States. It is part of the Wenatchee−East Wenatchee Metropolitan Statistical Area. The population was 1,965 at the 2010 census.[5] The entire town center is modeled on a Bavarian village as part of a civic initiative that began in the 1960s. The area is a major tourist destination during the wintertime. Leavenworth sits on the southeast side of the North Cascades collage, which is a group of terranes that accreted to North America all about the same time. Marine fossils indicate that the terranes were probably a group of islands originating in the South Pacific hundreds of million years ago. The terranes arrived at North America about 90 million years ago in the middle of the Cretaceous period. When they smashed into their new home, they were a puzzle of north-south slices. As accretion continued, they were cut into horizontal (east-west) slices. During the Eocene epoch, about 50 million years ago, the area was once again cut into vertical slices, creating among others, the Leavenworth fault and the Entiat fault. In between these two faults the Chiwaukum graben was created. This graben is about 12 miles wide and trends northwest from Wenatchee for about 50 miles. As the graben dropped, it immediately began to fill with clastic sediment from the surrounding hills, creating the Chumstick formation. About 30 million years ago in the Oligocene epoch, the Chiwaukum graben underwent compressional deformation creating several folds in the region that are visible today. Leavenworth is on the western edge of the graben; in fact, the Leavenworth fault runs through the western edge of town. The area to the west and southwest of Leavenworth was created in the middle Cretaceous period with the uplift of the Mt. Stuart batholith, forming the granite rock we see today in Icicle Ridge and Tumwater Mountain. During the Pleistocene and into the Holocene epoch, Leavenworth would have been a cold place to live. An alpine glacier originating from the southwest in the Mount Stuart range made its way to where the town is today. Leavenworth actually sits on the terminal moraine of that glacier. The residential parts of town display many glacial erratics that originated 20 miles up the Icicle Valley near Mount Stuart. quoted from ,_Washington -- If you enjoy, please subscribe(daily update!), like, comment, or share!! ========================================= ▶︎ Using GEAR iPhone 11 Pro Freefly Movi Cinema Robot ========================================= ▶︎ Other Videos 【US】 Beverly Hills 4K 60fps Santa Monica 4K 60fps Los Angeles(Downtown) 4K 60fps Hollywood 4K 60fps Las Vegas 4K 60fps Death Valley 4K 60fps 【Canada】 Vancouver 4K 60fps North Vancouver 4K 60fps
