Soils of the - Agriculture and Agri-Food Canada
Soils of the - Agriculture and Agri-Food Canada
Soils of the - Agriculture and Agri-Food Canada
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MISCELLANEOUS LAND TYPE S<br />
Miscellaneous l<strong>and</strong> types consist <strong>of</strong> naturally occuring or man-made components <strong>of</strong> <strong>the</strong> l<strong>and</strong>scape but ar e<br />
considered not to be "soil" as defined in this report . They, however, are mappable <strong>and</strong> seven different l<strong>and</strong> types<br />
are classified in <strong>the</strong> map area .<br />
Anthropogenic (A) : The Anthropogenic l<strong>and</strong> type consists <strong>of</strong> areas which are man-made or so severel y<br />
man-modified that <strong>the</strong> original characteristics <strong>of</strong> <strong>the</strong> soil have been destroyed . About 310 ha are classified<br />
as Anthropogenic l<strong>and</strong> type, located mainly in <strong>the</strong> vicinity <strong>of</strong> Vancouver. In <strong>the</strong> map area, this l<strong>and</strong> typ e<br />
consists mainly <strong>of</strong> l<strong>and</strong> fill materials including hog fuel, gravel, <strong>and</strong> s<strong>and</strong> dredgings . An anthropogenic soi l<br />
variant employed in some map units is similar to this Anthropogenic l<strong>and</strong> type except that l<strong>and</strong> disturbance<br />
is usually less severe <strong>and</strong> some characteristics <strong>of</strong> <strong>the</strong> original soil are still identifiable .<br />
Gravel Pit (GP) : The Gravel Pit l<strong>and</strong> type consists <strong>of</strong> both active <strong>and</strong> inactive areas <strong>of</strong> gravel or san d<br />
extraction sufficiently large to be mapped at <strong>the</strong> time <strong>of</strong> <strong>the</strong> survey . About 550 ha are classified as Grave l<br />
Pit l<strong>and</strong> type .<br />
Ice (I) : The Ice l<strong>and</strong> type consists <strong>of</strong> glaciers <strong>and</strong> permanent snow fields that occupy a small part <strong>of</strong> <strong>the</strong> ma p<br />
area. About 85 ha are classified as Ice l<strong>and</strong> type in <strong>the</strong> vicinity <strong>of</strong> Mt . Robie Reid .<br />
Recent Alluvium (RA) : The Recent Alluvium l<strong>and</strong> type is composed <strong>of</strong> gravel <strong>and</strong> s<strong>and</strong> bars, spits an d<br />
o<strong>the</strong>r similar deposits in or adjacent to rivers <strong>and</strong> streams . They are usually inundated except during low<br />
water <strong>and</strong> are generally unvegetated. Their shape, size <strong>and</strong> location may be altered from year to year b y<br />
erosion <strong>and</strong> subsequent redeposition . About 1050 ha are classified as Recent Alluvium l<strong>and</strong> type, mainl y<br />
in or adjacent to <strong>the</strong> Fraser River.<br />
Rock Outcrop (RO) : The Rock Outcrop l<strong>and</strong> type is common in <strong>the</strong> map area, particularly at <strong>the</strong> highe r<br />
elevations in <strong>the</strong> mountains . It consists <strong>of</strong> areas <strong>of</strong> exposed bedrock or bedrock areas with less than 10 c m<br />
<strong>of</strong> mineral or organic soil on <strong>the</strong> rock surface . Topographically, Rock Outcrops areas are usually very t o<br />
extremely sloping or hilly to very hilly ; slope gradients are mostly greater than 30 percent. About 440 ha <strong>of</strong><br />
Rock Outcrop l<strong>and</strong> type are classified as well as 23 040 ha <strong>of</strong> complexes dominated by Rock Outcrop . Th e<br />
complexes are with a variety <strong>of</strong> soils <strong>and</strong> Talus l<strong>and</strong> type .<br />
Talus (TA) : The Talus l<strong>and</strong> type consists <strong>of</strong> actively accumulating, colluvial depositions <strong>of</strong> mostly gravel ,<br />
stones <strong>and</strong> boulders at <strong>the</strong> base <strong>of</strong> rock cliffs <strong>and</strong> o<strong>the</strong>r steep rock faces . They are usually unvegetated<br />
<strong>and</strong> occur mainly at <strong>the</strong> higher elevations in association with Rock Outcrops . About 3290 ha are classified<br />
as Talus l<strong>and</strong> type with an additional 430 ha mapped as complexes dominated by Talus l<strong>and</strong> type . Th e<br />
complexes are mostly with Rock Outcrop l<strong>and</strong> type <strong>and</strong> Paton <strong>and</strong> Lions soils .<br />
Tidal Flat (TF) : The Tidal Flat l<strong>and</strong> type consists <strong>of</strong> areas lying outside <strong>the</strong> dykes that are periodicall y<br />
covered by tidal waters . The main areas are along Boundary <strong>and</strong> Mud Bays, along Roberts Bank <strong>and</strong> nea r<br />
<strong>the</strong> mouth <strong>of</strong> <strong>the</strong> Fraser River . The deposits are mainly fine s<strong>and</strong>y to silty in texture, are strongly saline <strong>and</strong><br />
very poorly drained . About 3940 ha are classified as Tidal Flat l<strong>and</strong> type .<br />
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