Chapter 14 Flashcards
4 factors that change the nature and rapidity of shorelines
- Material of which the shoreline is made
- Weather, wind, climate, and climate change
- Tidal range
- Tectonic activity
submergent shorelines
when the land sinks or sea level rises, the shoreline appears to be drowned, with irregular coastline, prominent bays, and abundant islands, marshes, and lagoons
emergent shorelines
risen from sea by tectonic uplift or a drop in sea level \
Straight and bounded by steep cliffs; where tectonic uplift has occurred
wave base
depth of wave action limited to half of the wavelength
longshore drift
longshore currents move sand and silt parallel to the shoreline
wave-cut bench
as waves drive loose sediment across shorelines underlain by bedrock, the sediment abrades a flat surface
wave-cut notch
where costal cliffs made of unconsolidated sediment, the waves eat into the cliff and use the sediment as added abrasives
sea arch
zones of weak bedrock eroded quickily isolating stronger material and starting to cut into it as well
sea stack
when further erosion removes the support for the arch, it will colapse and form this
Beaches
most common depositional features and consist of sand and coarser sediment, coreal shelves and shell fragmeents
spits
elongate sand bars attached at one end to the mainland
Some are straight but others are curved shaped called hooks
Barrier islands
elongate sand bars that lie offshore and are not connected to the mainland
Salt/ tidal marshes
area between a barrier island and the shoreline
typically marshy wetland formed by sediment derived from mainland