Linked from

The 26 pages that link to Alluvial fan, each with the reason it gives.

• Sediment transportBroader topic: A sudden decrease in flow energy deposits transported sediment in a fan-shaped landform.

• FloodplainCompared with: Its sediment spreads outward from a slope break rather than along a river corridor.

• SedimentationBroader topic: Sediment settles as flowing water disperses across the fan surface.

• OasisRelated: Aquifers in alluvial fans can feed springs and wells near desert mountain fronts.

• River deltaCompared with: Both landforms spread sediment, but an alluvial fan forms on land rather than in a receiving water body.

• Tarim BasinRelated: Mountain streams deposit water and sediment at the basin’s desert margins.

• AlluviumBroader topic: This specific alluvial landform forms as streams abruptly lose speed at valley mouths.

• Sediment depositionBroader topic: The sudden drop in flow energy spreads sediment into a fan.

• AvulsionCompared with: Both systems shift depositional pathways, but avulsion is a channel change rather than a landform.

• Danube DeltaCompared with: Unlike an alluvial fan, the Danube Delta accumulates sediment at a river’s coastal mouth.

• Fluvial geomorphologyBroader topic: Its deposits reveal how rivers spread sediment as flow energy declines.

• Fluvial processesBroader topic: Abrupt changes in slope and flow spread river sediment across a fan.

• WadiRelated: Wadi floods often spread gravel and sand into fans at mountain fronts.

• ValleyRelated: Streams emerging from mountain valleys can deposit sediment at their mouths.

• BedformCompared with: Unlike a bedform, it is a depositional landform rather than a feature of a sediment bed.

• Siwalik HillsRelated: Ancient fans and river deposits built much of the hills’ sedimentary sequence.

• Kata TjutaRelated: Ancient alluvial deposits contributed material to the formation’s sedimentary rocks.

• River mouthCompared with: It resembles a delta but forms on land, not where a river enters a receiving water body.

• AggradationBroader topic: A sudden drop in flow competence causes sediment to accumulate and build the fan.

• Death Valley National ParkRelated: Streams from the park’s mountains build fans along the basin margins.

• Dadès GorgesRelated: Side valleys feed sediment fans into the Dadès valley.

• Dry lakeRelated: Floods at basin margins can carry sediment onto dry lake floors.

• Mallos de RiglosRelated: Ancient fan deposits supplied much of the coarse sediment later consolidated into the Mallos.

• ScreeCompared with: Its water-laid, often sorted deposits differ from gravity-fed scree.

• Turan DepressionBroader topic: Rivers descending from surrounding uplands deposit sediment along the depression’s margins.

• Ziz GorgesRelated: Such deposits form where tributaries emerge from mountain valleys into the Ziz corridor.