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  2. Yuseong Foot Spa - Wikipedia

    en.wikipedia.org/wiki/Yuseong_Foot_Spa

    A gazebo covers one end of the wading pool. The spring water in Yeusong Hot Spring originate from between 215 and 450 meters deep, are soft and mildly alkaline (pH 7.5 to 8.5) with a high mineral concentration including silicate (SiO2), known for softening the skin.

  3. Kah-Nee-Ta - Wikipedia

    en.wikipedia.org/wiki/Kah-Nee-Ta

    Kah-Nee-Ta Resort was started by a non-Indigenous doctor who owned land around the hot springs of the Warm Springs River. In 1961, the Tribes purchased the land back and started to rebuild the spa. The great flood of 1964 damaged the spa and the bridge accessing it. In 1964–1965, the Tribes built an Olympic-sized swimming pool, cottages ...

  4. Heosimcheong Spa - Wikipedia

    en.wikipedia.org/wiki/Heosimcheong_spa

    Heosimcheong Spa (Korean: 허심청) is a spa 10 km north of Dongnae District, Busan, South Korea. It is said to be the largest hot spring fed spa in Asia. [citation needed] It has facilities to accommodate 3000 guests on five floors. [1]

  5. The Omni Homestead Resort - Wikipedia

    en.wikipedia.org/wiki/The_Omni_Homestead_Resort

    The Homestead offers spa services to guests including massages, facial treatments, manicures and pedicures, and stays in the Serenity Garden, where guests can soak in pools fed by natural geothermal springs. Also located in the spa is the hotel's fitness center and indoor pool, open to any guests of the resort. [15]

  6. Cove Hot Springs Pool - Wikipedia

    en.wikipedia.org/wiki/Cove_Hot_Springs_Pool

    Cove Hot Springs Pool. Cove Hot Springs is a pool constructed over a natural hot spring in the Grande Ronde Valley of northeastern Oregon, U.S. [1] The 86 °F (30 °C) water flows at 300 US gallons (1,100 L) per minute which replaces the 15-by-15-foot (4.6 by 4.6 m) pool several times per day.

  7. Hot spring - Wikipedia

    en.wikipedia.org/wiki/Hot_spring

    A hot spring, hydrothermal spring, or geothermal spring is a spring produced by the emergence of geothermally heated groundwater onto the surface of the Earth. The groundwater is heated either by shallow bodies of magma (molten rock) or by circulation through faults to hot rock deep in the Earth's crust .

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