For the Instructor
These student materials complement the Coastal Processes, Hazards and Society Instructor Materials. If you would like your students to have access to the student materials, we suggest you either point them at the Student Version which omits the framing pages with information designed for faculty (and this box). Or you can download these pages in several formats that you can include in your course website or local Learning Managment System. Learn more about using, modifying, and sharing InTeGrate teaching materials.Estuary Formation
Different ways that estuaries can form include:
- Ria Estuaries: rising sea level fills an existing river valley such as what happened to create a special case of Ria known as the Coastal Plain Chesapeake Bay Estuary of the eastern U.S.A. (Figure 3.35).
- Tectonic Estuaries: tectonic deformation of the earth's crust, such as faulting, creates a localized depression that fills in with marine waters such as San Francisco Bay (Figure 3.36). Water depths in tectonic estuaries can be highly variable.
- Bar Built Estuaries: migrating barrier islands or spits extend across the mouth of a bay and restrict the amount of marine water entering the bay to create an estuary (Figure 3.36). They tend to be relatively shallow and typically less than 10m of water.
- Fjord Estuaries: glacially carved, U-shaped valleys that filled with marine water since the end of the last ice age (Figure 3.37, Figure 3.38). They can extend long distances 10s to 100s of kilometers and as deep as several hundred meters.
Credit: NASA
Credit: https://commons.wikimedia.org/wiki/File:BayareaUSGS.jpg courtesy of the U.S. Geological Survey
Credit: Christchurch,_New_Zealand,_NASA_2.jpg (author) derivative work: Schwede66. Public domain via Wikimedia Commons
Credit: By en:User:Worldtraveller, (en:Image:Sognefjord, Norway.jpg) GFDL or CC-BY-SA-3.0