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  2. Cochabamba Water War - Wikipedia

    en.wikipedia.org/wiki/Cochabamba_Water_War

    The Cochabamba Water War, [2] also known as the Bolivian Water War, was a series of protests that took place in Cochabamba, Bolivia's fourth largest city, between December 1999 and April 2000 in response to the privatization of the city's municipal water supply company SEMAPA.

  3. Água de Alto - Wikipedia

    en.wikipedia.org/wiki/Água_de_Alto

    Água de Alto is situated on the southern coast of the island of São Miguel. It is located along the regional roadway E.R.1-1ª, that encircles the island, connecting the municipality of Vila Franca do Campo with Ponta Delgada by way of the community of Lagoa along the southern coast.

  4. Water distribution on Earth - Wikipedia

    en.wikipedia.org/wiki/Water_distribution_on_Earth

    Most water in Earth's atmosphere and crust comes from saline seawater, while fresh water accounts for nearly 1% of the total. The vast bulk of the water on Earth is saline or salt water, with an average salinity of 35‰ (or 3.5%, roughly equivalent to 34 grams of salts in 1 kg of seawater), though this varies slightly according to the amount of runoff received from surrounding land.

  5. Ciudad Mitad del Mundo - Wikipedia

    en.wikipedia.org/wiki/Ciudad_Mitad_del_Mundo

    Ciudad Mitad del Mundo as seen from the west from the 30-meter-high terrace of the museum The yellow line divides the 2 hemispheres. Older monument to the equator in Calacalí (2008) The Ciudad Mitad del Mundo ( Middle of the World City ) is a tract of land owned by the prefecture of the province of Pichincha , Ecuador .

  6. Water holding capacity - Wikipedia

    en.wikipedia.org/wiki/Water_holding_capacity

    Main page; Contents; Current events; Random article; About Wikipedia; Contact us; Pages for logged out editors learn more

  7. Greenland ice sheet - Wikipedia

    en.wikipedia.org/wiki/Greenland_ice_sheet

    The Greenland ice sheet is an ice sheet which forms the second largest body of ice in the world. It is an average of 1.67 km (1.0 mi) thick and over 3 km (1.9 mi) thick at its maximum. [2]

  8. North Atlantic Deep Water - Wikipedia

    en.wikipedia.org/wiki/North_Atlantic_Deep_Water

    During a positive NAO phase, conditions exist for strong winter storms to develop. These storms freshen the surface water, and their winds increase cyclonic flow, which allows denser waters to sink. As a result, the temperature, salinity, and density vary yearly. In some years these conditions do not exist and CLSW is not formed.

  9. Cabo da Roca - Wikipedia

    en.wikipedia.org/wiki/Cabo_da_Roca

    Cabo da Roca (Portuguese: [ˈkaβu ðɐ ˈʁɔkɐ]) or Cape Roca is a cape which forms the westernmost point of the Sintra Mountain Range, of mainland Portugal, of continental Europe, and of the Eurasian landmass. [1]