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  2. The floor is lava - Wikipedia

    en.wikipedia.org/wiki/The_floor_is_lava

    In one version called "Hot Lava Monster", sometimes referred to as "Skies in the Ringuss", usually played on playgrounds, players must stay off the ground (sand, rubber, woodchips, etc.) and on the play equipment. The person who is playing the "monster" can be on the 'lava' with the objective of attempting to tag another player.

  3. Jacobsville Sandstone - Wikipedia

    en.wikipedia.org/wiki/Jacobsville_Sandstone

    Jacobsville Sandstone is a red sandstone formation, marked with light-colored streaks and spots, primarily found in northern Upper Michigan, portions of Ontario, and under much of Lake Superior. Desired for its durability and aesthetics, the sandstone was used as an architectural building stone in both Canada and the United States.

  4. Sandstone - Wikipedia

    en.wikipedia.org/wiki/Sandstone

    Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains, cemented together by another mineral. Sandstones comprise about 20–25% of all sedimentary rocks.

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  6. Core Keeper - Wikipedia

    en.wikipedia.org/wiki/Core_Keeper

    Core Keeper is a survival sandbox game developed by Pugstorm. The game features mechanics similar to other games in the sandbox genre such as Minecraft, Terraria and Stardew Valley, including mining, crafting, farming and exploration in a procedurally generated underground world.

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  8. Desert sand (color) - Wikipedia

    en.wikipedia.org/wiki/Desert_sand_(color)

    Desert is a color that resembles the color of the flat areas of a desert.. The first recorded use of desert as a color name in English was in 1920. [12]The normalized color coordinates for desert are identical to fallow, wood brown and camel, which were first recorded as color names in English in 1000, [13] 1886, [14] [a] and 1916, [16] respectively.

  9. Red beds - Wikipedia

    en.wikipedia.org/wiki/Red_beds

    Red beds (or redbeds) are sedimentary rocks, typically consisting of sandstone, siltstone, and shale, that are predominantly red in color due to the presence of ferric oxides. Frequently, these red-colored sedimentary strata locally contain thin beds of conglomerate , marl , limestone , or some combination of these sedimentary rocks.