KnowraForeland basinLinked fromLinked fromThe 11 pages that link to Foreland basin, each with the reason it gives.All 11Broader topic 3Related 5Compared with 3Continental collisionRelated: The weight of collision-built mountains can depress adjacent continental crust.OrogenyRelated: The weight of an advancing orogen can create a basin that records its growth.Sedimentary basinBroader topic: It is a common basin type whose subsidence is driven by nearby mountain building.Back-arc basinCompared with: It develops through compression and loading rather than back-arc extension.Andean orogenyRelated: Andean loading helped create basins that preserve records of mountain growth and erosion.Tectonic subsidenceBroader topic: The weight of an advancing orogenic belt flexes the lithosphere and causes subsidence.Forearc basinCompared with: It develops beside an orogen, rather than between a trench and volcanic arc.FlyschRelated: Flysch commonly accumulates in the deep-water part of this mountain-front basin.Canadian RockiesRelated: The Rockies’ growth created adjacent basins that collected eroded mountain sediment.Oceanic basinCompared with: This basin forms beside mountains on a plate, not as a broad ocean-floor region.Structural basinBroader topic: It is a specific basin type formed by flexure next to a growing mountain belt.