Your Watershed-It Matters!

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Shorelines & Estuaries Vital Parts of the Watershed Estuaries are bodies of water partly surrounded by land where fresh water from rivers and streams runs into and mixes with salt water from the ocean. Estuary is another name for bay, sound, inlet, harbor, lagoon - anywhere there is the mixing of fresh and salt water. There are 102 estuaries in the U.S. according to the EPA. Of these, 28 have been designated by their states and the federal government to be of national importance. Estuaries have many different types of habitats including shellfish beds, sea grass meadows, salt and fresh marshes, forested wetlands, beaches, river deltas, and rocky shores. Among the most productive natural systems on earth due to the mixing of nutrients from land and sea, estuaries provide more food per acre than the richest Midwestern farmland. Estuaries and coastal waters provide essential habitat for over 75% of the commercial fish catch and 80-90% of the recreational catch of fish. As more and more people move to our coastlines and estuaries, it is important to understand the role these areas play in healthy watersheds. To lessen our harmful impacts, it is important to minimize bulkheads, docks, and shoreline structures. When possible consider soft erosion control methods which use natural materials such as gravel, sand, logs, and root masses to absorb wave energy.

PHOTO CREDIT: “Rocks on Cannon Beach” from http://www.flickr.com/photos/paraflyer/2210170066/ by paraflyer, “Tobias”. Accessed June 2011. Reproduced under Creative Commons Attribution-NonCommercial-NoDerivs 2.0 Generic (CC BY-NC-ND 2.0)





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Carbon - Another Natural Cycle All organic life is based on the chemical element carbon Carbon forms compounds with other elements and is present in a diversity of states including gases (carbon dioxide), solid minerals (limestone), and soft tissues (all plant and animal parts). The carbon cycle is the movement of carbon through living organisms, oceans, the atmosphere and the crust of the planet. The earth maintains a natural carbon balance, slowly working to remove carbon from the atmosphere. Natural carbon removal doesn’t keep up the pace of the rapid rate in which humans are moving carbon into the atmosphere by burning fossil fuels, so carbon in the atmosphere is increasing faster than nature can process it. Carbon continually exchanges within a closed system consisting of the atmosphere, oceans, biosphere, and landmass. There are short- and longterm cycles at work.

Short-Term Carbon Cycles: Carbon is exchanged rapidly between plants and animals through respiration and photosynthesis, and through gas exchange between the oceans and the atmosphere. Long-Term

Carbon Cycle:

Over millions of years, carbon in the air is combined with water to form weak acids that very slowly dissolve rocks. This carbon is carried to the oceans where some forms coral reefs and shells. These sediments may be moved deep into the earth by drifting continents and eventually released into the atmosphere by volcanoes.










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