Linked from

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

• Vadose zoneNarrower topic: The vadose zone is the unsaturated region above groundwater in an unconfined setting.

• Artesian wellNarrower topic: Artesian wells draw groundwater from a pressurized subsurface reservoir.

• Cave formationRelated: Groundwater transports dissolved carbon dioxide and carries away minerals released from cave walls.

• CenoteRelated: Groundwater fills many cenotes and links them to subterranean aquifers.

• Earth's crustRelated: Fractures and permeable layers in the crust control groundwater storage and movement.

• EarthworksRelated: Groundwater can destabilize excavations, soften subgrades, and complicate material handling.

• Geological mapRelated: Geological units and structures influence where groundwater is stored and how it moves.

• HydrosphereBroader topic: It is a major reservoir of liquid water hidden below land.

• Confined aquiferNarrower topic: The water stored and transmitted here is groundwater.

• Earth scienceRelated: Geologic and hydrologic knowledge guides its protection and sustainable use.

• Geologic mapRelated: Unit boundaries and structures help predict aquifers, barriers, and groundwater flow paths.

• Karakum DesertRelated: Subsurface water supports settlements and ecosystems in this arid region.

• Oxidation zoneRelated: Groundwater transports oxygen and dissolved reaction products through the ore.

• Pore waterNarrower topic: Groundwater occupies connected pores and fractures, forming a subsurface water resource.

• Riparian forestRelated: Shallow groundwater can sustain trees when rainfall and river levels fall.

• Septic systemRelated: Groundwater can be contaminated if septic effluent reaches it without sufficient treatment.

• Bridge foundationRelated: Groundwater affects excavation, soil strength, and construction around foundations.

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

• Natural resourceBroader topic: Aquifers supply drinking water and irrigation, but pumping can exceed replenishment.

• 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.

• Mineral waterNarrower topic: Many mineral waters begin as groundwater moving through mineral-bearing rock.

• 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.

• Gila RiverCompared with: Groundwater pumping can replace or supplement river water in the Gila basin.

• Guarani AquiferNarrower topic: The aquifer is a major regional store of this resource.

• 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.

• Fresh waterBroader topic: It is a major freshwater store below the land surface.

• LānaʻiNarrower topic: Limited freshwater supplies make groundwater central to Lānaʻi’s communities and land use.

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

• Underground lakeNarrower topic: Underground lakes are a visible, open-cavity form of subsurface water.

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