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Last modified
1/26/2010 10:08:02 AM
Creation date
10/5/2006 4:05:15 AM
Metadata
Fields
Template:
Floodplain Documents
County
Statewide
Basin
Statewide
Title
Protecting Floodplain Resources
Date
6/1/1996
Prepared For
US
Prepared By
FEMA
Floodplain - Doc Type
Floodplain Report/Masterplan
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<br />r <br /> <br /> <br />[ <br /> <br />.~ <br /> <br />_1;~ _"':.-.~ ~t. JJ. ::;l~:!t~.:;' <br /> <br />. " <br /> <br />i- <br /> <br />I <br />r <br /> <br />~ - <br />~"""' <br /> <br />-" <br /> <br />.- <br /> <br />~ <br /> <br />',- --"-'~ <br />~~~,"-~" <br />. ,~.,- <br /> <br />.....- <br /> <br /> <br />.~ <br /> <br />- <br /> <br />J_ . <br /> <br />- <br />~- <br /> <br />II Understanding Floodplain Resources <br /> <br />What Are Floodplain Natural Resources? <br /> <br />The term "natural resources" often brings to mind products, such as timber or fossil <br />fuels that may be extracted from their natural environments and sold as commodities <br />for profit. But the natural values of floodplains are different; their value lies not in their <br />removal and sale, but in the functions that they perform within the floodplain environ- <br />ment. Floodplain natural resources include the soils, nutrients. water quality and quan- <br />tity, and diverse species of plants and animals that exist in the areas between the \vater's <br />edge and the higher ground adjoining flood-prone areas. These can be considered as <br />natural "infrastructure." But what is it about these resources that make a naturally <br />functioning floodplain so valuable? \Ve will begin the discussion with some basic <br />information about hO\v l100dplains are formed. <br /> <br /> <br />Rivers Slzape tlze Landscape. The formation of a !loodplain is intimately tied to the <br />adjacent river or stream, \vhich over long periods of time carves out the surface geology <br />of the landscape and deposits sand, silt. and other material (these deposits are referred to <br />as alluvium) that form rich soils. A typical river corridor has several features that result <br />from the geological and hydrological processes that form these landscapes (Figure 4). <br />The river channel meanders through the landscape, carving through the terrain and <br />depositing sediment as it goes. Sediment deposits and depressions around the water's <br />edge may result in the formation of wetlands, areas that are always or periodically <br />inundated with water. <br /> <br />The level areas bordering river channels are known as floodplains. These portions of <br />river valleys are frequently defined in terms of the likelihood of flooding in a given <br />year. Hence, the" I OO-year" flood is the flood having a 1 % chance of occurring during <br />any given year. (Similar definitions can be made for the 25- or 50-year !loods.) As the <br />river cuts downward it may leave terraces. formed from a time \vhen the river flowed <br />at higher elevations. These landforms are a part of the larger river corridor. and are <br />extremely important to the functioning of the floodplain ecosystem. <br /> <br />ll'ater.5heds - \Vhile the floodplain and its resources are the ccntcrpiece of discussion <br />for this guidebook, watersheds are central to the understanding and management of <br />resources in floodplains. A watershed includes the area of land that is drained by a <br />river and its tributaries. Different watersheds are separated from each other by ridges <br /> <br />- <br />
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