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  2. Rock garden - Wikipedia

    en.wikipedia.org/wiki/Rock_garden

    The Japanese rock garden, or dry garden, often referred to as a "Zen garden", is a special kind of rock garden with a few large rocks, and gravel over most of the surface, often raked in patterns, and no or very few plants. Other Chinese and Japanese gardens use rocks, singly or in groups, with more plants, and often set in grass, or next to ...

  3. Glacial erratic boulders of the Puget Sound region - Wikipedia

    en.wikipedia.org/wiki/Glacial_erratic_boulders...

    The erratic lies in what is said to be the smallest King County park, 20 by 70 feet (6.1 m × 21.3 m) in extent, that barely contains the rock and sequoias. [18] The two lanes of Big Rock Road used to split into a wye around the rock, until a shopping center was built nearby in the 1990s. [17] [18

  4. Glacial erratic boulders of Island County, Washington

    en.wikipedia.org/wiki/Glacial_erratic_boulders...

    The Clinton erratic is a greenstone boulder with north-south glacial striations, at the corner of Conrad St and Berg Road above the ferry terminal in the town of Clinton. The rock and Coupeville's Big Rock were used to calibrate 36 Cl radiometric dating due to the well established date they were deposited and began to receive cosmic ray ...

  5. Glacial erratic boulders of King County, Washington - Wikipedia

    en.wikipedia.org/wiki/Glacial_erratic_boulders...

    The two lanes of Big Rock Road used to split into a wye around the rock, until a shopping center was built nearby in the 1990s. [14] [13. 8 feet (2.4 m) Big Rock Park erratic is a glacial erratic in the eponymous city park in Sammamish. Sammamish considered naming the park "Bigger Rock Park" to distinguish it from the identically named park in ...

  6. Glacial erratic - Wikipedia

    en.wikipedia.org/wiki/Glacial_erratic

    Multiple erratics on the terminal moraine of the Okanogan Lobe. The Cascade Mountains are in the background.. The term "erratic" is commonly used to refer to erratic blocks, which geologist Archibald Geikie describes as: "large masses of rock, often as big as a house, that have been transported by glacier ice, and have been lodged in a prominent position in the glacier valleys or have been ...

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