Marshes, swamps, and bogs are all types of wetlands—lands saturated by water long enough to support aquatic plants and hydric soils. They differ by **water source, vegetation, and chemistry**.
| Type | Water Source | Dominant Vegetation | Soil / Chemistry | Key Function |
|---|---|---|---|---|
| Marsh | Surface water (river, lake, tide); mineral-rich | **Emergent herbaceous**: cattails, bulrushes, sedges, reeds, wild rice | Mineral soil (hydric); neutral to alkaline | Flood buffer, water filtration, waterfowl nursery, carbon sequestration |
| Swamp | Surface + groundwater; often riverine/floodplain | **Woody**: trees (cypress, tupelo, mangrove, cedar) + shrubs | Mineral/organic; nutrient-rich | Flood storage, timber, wildlife corridor, nutrient cycling |
| Bog | **Precipitation only** (ombrotrophic); isolated from groundwater | **Sphagnum moss** + ericaceous shrubs (cranberry, blueberry), stunted conifers | **Peat** (accumulated Sphagnum); **acidic (pH 3–4), nutrient-poor** | Carbon sink (millennia), paleoclimate archive, unique endemics |
**87% of wetlands lost since 1700** (Ramsar). **35% since 1970.** Main drivers: drainage for agriculture, urbanization, pollution, climate change.
Marsh, swamp, bog, fen — **all wetlands, all essential, all vanishing.** Knowing the difference is the first step to saving them.