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  2. Bedform - Wikipedia

    en.wikipedia.org/wiki/Bedform

    Current ripples preserved in sandstone of the Moenkopi Formation, Capitol Reef National Park, Utah, United States. A bedform is a geological feature that develops at the interface of fluid and a moveable bed, the result of bed material being moved by fluid flow. Examples include ripples and dunes on the bed of a river.

  3. Cross-bedding - Wikipedia

    en.wikipedia.org/wiki/Cross-bedding

    Cross-bedding is formed by the downstream migration of bedforms such as ripples or dunes [3] in a flowing fluid. The fluid flow causes sand grains to saltate up the stoss (upstream) side of the bedform and collect at the peak until the angle of repose is reached. At this point, the crest of granular material has grown too large and will be ...

  4. Sedimentary structures - Wikipedia

    en.wikipedia.org/wiki/Sedimentary_structures

    Flow regimes in single-direction (typically fluvial) flow, which at varying speeds and velocities produce different structures, are called bedforms. In the lower flow regime, the natural progression is from a flat bed, to some sediment movement (saltation etc.), to ripples, to slightly larger dunes. Dunes have a vortex in the lee side of the dune.

  5. The dunes are just the beginning of what’s so great about ...

    www.aol.com/dunes-just-beginning-great-great...

    The dunes are believed to be remnants of a massive lake, Laka Alamosa, that dried up roughly 440,000 years ago, according to the park’s website.Over time, the park says wind, water and sediment ...

  6. Love long walks on the beach or hikes in the woods? This ...

    www.aol.com/love-long-walks-beach-hikes...

    What does it cost to get into Indiana Dunes National Park? Park entry costs $25 for a private vehicle, $20 for a motorcycle, or $15 per person arriving by foot, bike or boat.

  7. Indiana Dunes National Park - Wikipedia

    en.wikipedia.org/wiki/Indiana_Dunes_National_Park

    Indiana Dunes National Park is a national park of the United States located in northwestern Indiana managed by the National Park Service. It was authorized by Congress in 1966 as the Indiana Dunes National Lakeshore and was redesignated as the nation's 61st national park on February 15, 2019. [ 2 ]

  8. Bed (geology) - Wikipedia

    en.wikipedia.org/wiki/Bed_(geology)

    Cross-beds, or "sets," are not layered horizontally and are formed by a combination of local deposition on the inclined surfaces of ripples or dunes, and local erosion. Graded beds show a gradual change in grain or clast sizes from one side of the bed to the other. A normal grading occurs where there are larger grain sizes on the older side ...

  9. Guide to Sleeping Bear Dunes National Lakeshore: How to ... - AOL

    www.aol.com/sleeping-bear-dunes-volunteers-carry...

    To put things in perspective, last year the park saw more than 1.5 million visitors, according to National Park Service statistics. ... How to prepare for Sleeping Bear Dunes National Lakeshore.