A River-Channel Field Transect: Linking Sediment to Flow
A river transect is a structured way to observe how channel form and sediment change from one bank to the other. It links visible landforms with the m
A river transect is a structured way to observe how channel form and sediment change from one bank to the other. It links visible landforms with the m
Rivers transport sediment of many sizes, from dissolved ions and fine clay to sand, gravel and large boulders. The material carried at a location depe
Permafrost is ground that remains at or below freezing for at least two consecutive years. It occurs in high-latitude and high-elevation regions, wher
Weathering breaks down or alters rock in place, whereas erosion removes and transports material. The processes often operate together, but separating
Coastlines are dynamic boundaries shaped by waves, tides, currents, sediment supply and sea-level change. Erosion occurs when material is removed fast
Soil develops where climate, organisms, topography, parent material and time interact. Its horizons preserve evidence of weathering, organic activity,
Learn how aquifers store and transmit groundwater through pores, fractures and connected geological formations.