Linked from

The 98 pages that link to Groundwater, each with the reason it gives.

• Fennoscandian ShieldRelated: Fractured shield bedrock governs groundwater storage and flow in many localities.

• Oasis agricultureRelated: It feeds many springs and wells used to irrigate oasis fields.

• River red gumRelated: Access to groundwater can help mature trees survive between floods.

• Point barRelated: Point-bar sands can form permeable pathways for groundwater movement.

• La Pampa ProvinceRelated: It is a vital resource for communities and production in La Pampa’s dry regions.

• Joshua Tree National ParkRelated: It sustains springs and palm oases where surface water is scarce.

• Kharga OasisRelated: Access to groundwater makes Kharga’s farms and communities possible.

• Al-Ahsa OasisRelated: Groundwater feeds the springs on which the oasis historically depended.

• Petrified woodRelated: Groundwater transports dissolved minerals through buried wood.

• Tap waterRelated: Wells and aquifers supply many local and municipal drinking-water systems.

• Jeita GrottoRelated: Groundwater dissolves and flows through the limestone passages of the grotto.

• K'gariRelated: Groundwater sustains island vegetation and feeds lakes and streams.

• Lake TritrivaRelated: Contact between groundwater and rising magma can trigger the explosions that excavate maars.

• Optymistychna CaveRelated: Its movement through gypsum drives dissolution and cave development.

• River sourceRelated: Groundwater can emerge as a spring that forms a river source.

• Subterranean biologyRelated: It is both habitat and transport network for subterranean aquatic life.

• Tunnel constructionRelated: Groundwater inflow can destabilize excavations and require drainage or pressure control.

• Acre-footRelated: Pumping and recharge estimates can be expressed as acre-feet.

• Badain Jaran DesertRelated: Groundwater is a leading explanation for how lakes persist in this arid landscape.

• Body of waterRelated: It forms subsurface water bodies and exchanges water with springs, rivers, and lakes.

• Candelaria CavesRelated: Groundwater dissolves limestone and helps shape cave passages.

• Chinhoyi CavesRelated: Groundwater fills the cave pool and moves through the surrounding limestone.

• Møns KlintRelated: Water moving through porous chalk can weaken slopes and help trigger collapses.

• Upland and lowlandRelated: Groundwater often flows from upland recharge areas toward lowland springs and wetlands.