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Soils of the - Agriculture and Agri-Food Canada

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E<br />

F<br />

FG<br />

I<br />

Definition 2<br />

Colluvial : Materials that have reached<br />

<strong>the</strong>ir present position by direct, gravity -<br />

induced movement.<br />

Eolian : Materials transported an d<br />

deposited by wind action .<br />

Fluvial : Materials transported an d<br />

deposited by rivers <strong>and</strong> streams .<br />

Fluvioglacial : Fluvial materials that have<br />

been deposited ei<strong>the</strong>r directly in front <strong>of</strong> ,<br />

or in contact with, glacier ice .<br />

Ice : Areas <strong>of</strong> snow <strong>and</strong> ice where<br />

evidence <strong>of</strong> active movement is present .<br />

Lacustrine : Sediments that have settle d<br />

from suspension in st<strong>and</strong>ing fresh wate r<br />

or have accumulated in <strong>the</strong> margins<br />

through wave action .<br />

Morainal : Materials transported<br />

beneath, beside, on, within or in front o f<br />

a glacier <strong>and</strong> deposited directly fro m<br />

<strong>the</strong> glacier.<br />

0 Organic : Materials resulting from<br />

vegetative growth, decay an d<br />

accumulation ; rate <strong>of</strong> accumulatio n<br />

exceeds that <strong>of</strong> decay.<br />

R Bedrock : Outcrop, <strong>and</strong> rock covered b y<br />

a thin mantle (less than 10 cm thick) <strong>of</strong><br />

unconsolidated mineral <strong>and</strong>/or organi c<br />

materials .<br />

W<br />

W e<br />

Marine : Sediments that have settle d<br />

from suspension in salt or brackis h<br />

water bodies or that have accumulate d<br />

at <strong>the</strong>ir margins through shorelin e<br />

processes .<br />

Glaciomarine : Sediments <strong>of</strong> glacia l<br />

origin, laid down in a marin e<br />

environment in close proximity to glacier<br />

ice .<br />

SURFACE EXPRESSIO N<br />

Definitio n<br />

Blanket : A mantle <strong>of</strong> unconsolidate d<br />

materials thicker than 1 m .<br />

Fan : A fan-shaped form possessing a<br />

perceptible gradient from apex to toe .<br />

Level : A flat or gently sloping surfac e<br />

not broken by marked elevations o r<br />

depressions .<br />

Veneer: Unconsolidated material s<br />

between 10 cm <strong>and</strong> 1 m thick ; if n o<br />

information about <strong>the</strong> underlyin g<br />

stratigraphic unit is supplied, it i s<br />

assumed <strong>the</strong> veneer overlies bedrock .<br />

COMPOSITE UNITS<br />

Composite units are employed when <strong>the</strong> individual<br />

terrain units in a map polygon cannot be delimite d<br />

individually at <strong>the</strong> scale <strong>of</strong> mapping . The components<br />

are indicated in decreasing order <strong>of</strong> abundance . Th e<br />

symbolization is as follows :<br />

/ <strong>the</strong> component in front <strong>of</strong> <strong>the</strong> symbol is mor e<br />

abundant than <strong>the</strong> one that follows .<br />

// <strong>the</strong> component in front <strong>of</strong> <strong>the</strong> symbol i s<br />

considerably more abundant than th e<br />

component that follows .<br />

' Classification modified from Environment <strong>and</strong> L<strong>and</strong> Use Committee Secretariat, 1976 .<br />

2 The deposits are more adequately described in <strong>the</strong> pages under Surficial Geologic Deposits .<br />

_<br />

aL<br />

\ ~, l<br />

CJ<br />

n ~'<br />

~~<br />

~ J~<br />

:-<br />

~ttOrr~~ll7leYR~i~1IenUalh G<br />

(i'<br />

y<br />

v<br />

~<br />

JfTJ<br />

hEir,<br />

~<br />

~l'err<br />

-1~<br />

~ rz a q I w~0qi.~~ ~~m 11 Îa-.~ l' v'~'"`~ ~~~ ~~~~~~~ ~ ~.~E ~ ~ xiuYwxn~-~<br />

~. a• ' . I ~i~a~'~q, ~ ( ni`jr .~n ~ ;~ .,.<br />

~i-`]~~LJt~~, a_,~L~seu Sr: U► r~~~ ."r; - - I pp ~~~~~~ ~r,~~ . ,'F„ ~~, I'~'i ~~` ~,a ~~,,; ~~` -r-~,<br />

~,~~( , ~<br />

-.CbyscdalcJi,l ,~ ~~I .ANGL~~~ f$IL IC~~~ _ ; ~ w . . rf ~tZ ~L ,/=1_ GI I e ~ ~w7 "L ~<br />

~~0 l ~ d~i~ „prf +.-~.,~~.~ - ~.I;r - -r i .. cad •~. ~ H i ~ç-~~<br />

I<br />

~~9eU<br />

aàn l+uxiav 'v7~ 1<br />

~ -_ I ~~~`F1dS[@Y~ elq~ ~ ~, 0-/<br />

- ^~r-~ .~r ly '<br />

~` -<br />

.--<br />

J~~ ~<br />

~: ~<br />

~(~ ~r~~t~~~~~, ~ =~I ~~' , ~~ . 1C - ~ . ~, •~ . . . r ~_~. I F; '~ ~,~ r ~~ , ~<br />

J_,J_lL~~~q~ I t ~~ l'1~L,,~ . .5'v ~r~~~ ~l ~ Créar6r6ôk~ ~° ~~ r~t,~fôt âsi„ôe- C 7 . eooEa~4~ ~~`'<br />

~ :~~~ 1 q bL~~F~.~ NU~~~ IPlyLITYCp~depo~~ ~ ~~_r:ék~1. ~~I~ /'t JÉ/ ~~ rK .~~ 2W II<br />

/ i<br />

7 \ .h 1~ .R.'--`J,J'l ~'JV . \ / I ~-tr-~r-<br />

/~r T - rl E M~J~ EÎG.y<br />

i ~~<br />

°' Gnctia (rG~l [•~,~ Ì ? ~. f ,1~ I UrvIC~PALTV -„ i ~ ~<br />

9f-^(~ é~ 3n I .\ ~~=_ C~•'O.~Ll,._ ilt~ ._:_~IIL~ I' lj7 t -,.<br />

o~ ~<br />

i a,i ' I ~ ~ s II :j~'O~-dnr, I~1iSJ r-~,r o ~°<br />

^/ _ , ~~s ~ _ ` A<br />

rt-~-r ~<br />

`-iI a^^~i ~ ~l( Îun ~~ lûl .,h<br />

li . r ~~~<br />

Dou^l m~ ~r:2 ~-InIIr -I<br />

~~ ~~Ü. _~~ .~ Il~u~~il ~n . ~<br />

~-~~.~ ~,<br />

r ~~<br />

Figure 2 . Generalized surficial deposits map <strong>of</strong> <strong>the</strong> Coast Mountains <strong>and</strong> Sunshine Coast portion <strong>of</strong> <strong>the</strong> Langley-Vancouver map area .

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