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<br />38 <br /> <br />............,.,... <br />,...._......-..,.... <br />-." <br />-...,- <br />_.._,...,_..... <br />-......- <br />-.....".... <br />..-....'_...1 <br />.......-...... <br />"..,........- <br />"'0'''''''' <br />~.......... <br />-......,-,... <br />.....t. ._......... <br />.."....-."..... <br />(.0'........... <br />......,. <br /> <br />-.......... "Sola"'--r-TOOz.no-- <br />Zcno Zono <br /> <br />_T.r,ace Zone <br /> <br /> <br />-.-..,.... <br />~._'.. ....," <br />;:::.:~.::.~'...I <br />.......-..,.....'."." <br />..".._..'0..'0.""......... <br />::::::'::.:~...I;:;;;:':':;,.." <br />....ft.,..""'....-_n'"....... <br /> <br />-~~-.-i- <br /> <br />... -"- ; <br />--.... 1- <br />-----~~-~. <br /> <br />Figure ft. Str.....nlt zone.. <br /> <br />,rolll L. D. Logan. 1979. MaUve Ve~etj1tlon t'or ~t,..~alllb~nk Control, pagf'9 IS_lA, <br />In. Riparian .nd ~ethnd Habf.tats of the Great Plnlns. ProceedlnlZs of the 31st <br />Annual Meeting. Great Plains 4ricultural CouncIl. Rod:y Mountain Forest ;t(ld <br />Range Expert_nt: Station. Fort Col11(18. PB8Q-16Q005. <br /> <br />Channel Pattet'ns <br /> <br />Stream6 are characterized by different alignments and geometries which <br />make each O/le unique (Figure 7). Reaches of a stream ]Day be relatively <br />straight, hllve many interlaced chanrlels or be sinuous 1.ith rather tight <br />bends. Theile three deacripti,ons of stream I~attern are uaed to c1usify <br />streams as'lltra1ght, braided, or meandering.. <br /> <br />;-- <br /> <br />:::::::;:~~:/ <br /> <br />Straight <br /> <br />Sinuous <br /> <br />~ <br /> <br />~~~v <br /> <br />In-.sular <br /> <br />Irregular meender <br /> <br />~ <br />~ <br /> <br />~ <br /> <br />Reguhr Oleander <br /> <br />l'ortuous lIIeande r <br /> <br />_,_I <br /> <br />Filute 7. StRall chanMl ...ndering. <br /> <br />Straight Pattern <br /> <br />Straight channels sre often considered transitional to llIeandering. <br />Individual .tream reaches may have bends followed by straight reaches, but <br />