- ^?o - 



c . Hydroioqy .'Uii.i, .t . 



nraina'-ie 1j:i i;i: Newport River 



Hydro locj i c: :;, ; t • i: Mesic 



llydrologic Pib.y !'.i:i: Mesic to dry-mesic 



Water clicm i s t ry : Fresh 



W.itnr ruqitr.. : Permanently exposed 



d. Suriima ry-Tuj )'.>'[ rcii-'liy ,ii;d P!v/.: i (■,' i ,_i ■!:■,. 



Topographic :.i'> '\'\-i'- ci,,! t h ■ • ; i i i,-.; 



Laii 1 forr.: Slope and narrow fringe of adjacent upland . 



SiKjltor: Sheltered 



A.succt' Most slope a'-ea" fare easterly or westerly, 



Slofji- a.-iqJ' : Nearly level (0-2) to gently sloping (2-6); 



rarely sloping (6-10) 

 l^rofiio: Convex, concave, and constant 



L^arfaco [..iM' ii; ; Mostly smooth 



PosiLion: Entire slope and fringe of adjacent upland 



Physiogr a[)ii i c .,ii'; • yp'^ <"ir U'lui.n .H' .i: 



Walker's Mill Pond Natural Area 



Physiographic slLu l.yijc ol ..■( ...liuim i i \- cnvM" ; ■ ■ or 



community type-: Slopes and adjacent upland fringes within 



Walker's Mill Pond Natural Area 

 (ieoloyic format ion: Planner Beach Formation (Mixon and Pilkey 

 Geologic formation agu: pleistocene ^'^''^^ 



Roferences: Mixon, R. and 0. Pilkey. 1976. Reconnaissance Geo- 

 logy of the Submerged and Emerged Coastal Plain Province, Cape 

 Lookout Area, North Carolina. US Geol. Survey Prof. Paper 859 

 US Govt. Print. Office, Washington. 



