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  2. Body of water - Wikipedia

    en.wikipedia.org/wiki/Body_of_water

    Tide pool: a rocky pool adjacent to an ocean and filled with seawater. Tributary or affluent: a stream or river that flows into the main stem (or parent) river or a lake. Vernal pool: a shallow, natural depression in level ground, with no permanent above-ground outlet, that holds water seasonally. Wadi

  3. Fire hydrant - Wikipedia

    en.wikipedia.org/wiki/Fire_hydrant

    In warm areas, above-ground hydrants may be used with one or more valves in the above-ground portion. Unlike with cold-weather hydrants, it is possible to turn the water supply on and off to each port. This style is known as a "wet barrel" hydrant. Both wet- and dry-barrel hydrants typically have multiple outlets.

  4. Glossary of landforms - Wikipedia

    en.wikipedia.org/wiki/Glossary_of_landforms

    Tide pool – Rocky pool on a seashore, separated from the sea at low tide, filled with seawater; Tombolo – Deposition landform in which an island is connected to the mainland by a sandy isthmus; Volcanic arc – Chain of volcanoes formed above a subducting plate; Wave-cut platform – Narrow flat area created by erosion

  5. Retention basin - Wikipedia

    en.wikipedia.org/wiki/Retention_basin

    Storm water is typically channeled to a retention basin through a system of street and/or parking lot storm drains, and a network of drain channels or underground pipes.. The basins are designed to allow relatively large flows of water to enter, but discharges to receiving waters are limited by outlet structures that function only during very large storm eve

  6. Magma chamber - Wikipedia

    en.wikipedia.org/wiki/Magma_chamber

    Magma chambers above a subducting plate. Magma rises through cracks from beneath and across the crust because it is less dense than the surrounding rock. When the magma cannot find a path upwards it pools into a magma chamber. These chambers are commonly built up over time, [4] [5] by successive horizontal [6] or vertical [7] magma injections.

  7. Kuttam Pokuna - Wikipedia

    en.wikipedia.org/wiki/Kuttam_Pokuna

    A stone underground channel of 110 millimetres (4.5 in) wide, 130 millimetres (5 in) high and 2.4 metres (8 ft) feet, 230 millimetres (9 in) below the surface, connects both ponds. Because the opening into the channel is well above the bottom of the smaller pond, this would act as a filtering mechanism for the larger pond. [8]

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