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  2. Pebble - Wikipedia

    en.wikipedia.org/wiki/Pebble

    Close view of pebbles [vague]. A pebble is a clast of rock with a particle size of 4–64 mm (0.16–2.52 in) based on the Udden-Wentworth scale of sedimentology.Pebbles are generally considered larger than granules (2–4 mm (0.079–0.157 in) in diameter) and smaller than cobbles (64–256 mm (2.5–10.1 in) in diameter).

  3. List of quarries in the United States - Wikipedia

    en.wikipedia.org/wiki/List_of_quarries_in_the...

    Thunderbird Archaeological District and Jasper quarry, near Limeton, Virginia, is an archaeological district described as consisting of "three sites—Thunderbird Site, the Fifty Site, and the Fifty Bog. It is located in Warren County Virginia, near modern-day Front Royal, in the Shenandoah River Valley.

  4. Quarry Trails Metro Park - Wikipedia

    en.wikipedia.org/wiki/Quarry_Trails_Metro_Park

    Around March 2022, construction of a rock-climbing wall began at the park, to be 160 feet tall and about 1/2-mile wide, utilizing stones leftover from the quarry site. [2] Designed by Via Ferrata Works, it will be the first urban via ferrata in the United States. [3] The attraction opened in May 2023. [4]

  5. River gravel - Wikipedia

    en.wikipedia.org/wiki/River_gravel

    River gravel is a name given to gravel composed of small pieces of rounded stone of various colors, usually no larger than a large coin. [1] It is named for the effect of many years of rounding of the edges of the stones due to a flow of water over it, as often takes place in a river . [ 2 ]

  6. Gravel - Wikipedia

    en.wikipedia.org/wiki/Gravel

    Gravel (largest fragment in this photo is about 40 mm (1.6 in)) Gravel (/ ˈ É¡ r æ v É™l /) is a loose aggregation of rock fragments.Gravel occurs naturally on Earth as a result of sedimentary and erosive geological processes; it is also produced in large quantities commercially as crushed stone.

  7. Geology of Ohio - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Ohio

    The overlying Devonian rocks include the Columbus Limestone to the east of the Findlay Arch and the Detroit River Group carbonates to the west. The angular unconformity between lower Silurian rocks is marked in some places by phosphate beds, that preserve bones and teeth. A cast of a Dunkleosteus fossil found near Cleveland, Ohio

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