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  2. 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 ]

  3. 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.

  4. Crushed stone - Wikipedia

    en.wikipedia.org/wiki/Crushed_stone

    Crushed limestone quarry near Bellefonte, Pennsylvania. Angular crushed stone is the key material for macadam road construction, which depends on the interlocking of the individual stones' angular faces for its strength. [1] As riprap; As railroad track ballast; As filter stone. As composite material (with a binder) in concrete, tarmac, and ...

  5. Yuhua Stone - Wikipedia

    en.wikipedia.org/wiki/YuHua_Stone

    Yuhua stones. The Yuhua stone (Chinese: 雨花石; pinyin: yuhua shi; lit. 'rain flower stone') is a special kind of stone found in Nanjing, China, due to the unique geology of the area. Yuhua stones, or pebbles, are of sedimentary origin and consist of minerals including quartz and other silicates.

  6. 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).

  7. Conglomerate (geology) - Wikipedia

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

    Two recognized types of intraformational conglomerates are shale-pebble and flat-pebble conglomerates. [6] A shale-pebble conglomerate is a conglomerate that is composed largely of clasts of rounded mud chips and pebbles held together by clay minerals and created by erosion within environments such as within a river channel or along a lake ...

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