National Ecological Framework (15 of 23)
Surficial Geology
These data are presented as a set of components within each polygon. The following attributes are included:
Name | Description |
---|---|
UNIT | Surficial Geology |
The extent and nature of the surficial materials in this
database are derived from the Surficial Materials Map of Canada
(Fulton, 1996). The map identifies twenty-four types of
materials.
UNIT | Description |
---|---|
I | Glaciers: Ice and minor morainal debris. |
A | Alluvial Deposits: stratified silt, sand, clay, and gravel; floodplain, delta, and fan deposits; in places overlies and includes glaciofluvial deposits. |
Marine Deposits: sediments deposited in marine waters under nonglacial conditions and remaining at or below present lake level. | |
mM | Marine Mud: Fluid silty clay and clayey silt: deposited as quiet water sediments. |
sM | Marine Sand: Sand and locally gravel; deposited as sheet sands, lags, and beaches. |
Lacustrine Deposits: sediments deposited in lakes under nonglacial conditions and remaining at or below present lake level. | |
mL | Lacustrine Mud:Fluid silty clay and clayey silt: deposited as quiet water sediments. |
sL | Lacustrine Sand: Sand and locally gravel; deposited as sheet sands, lags, and beaches. |
E | Eolian Deposits: sand and minor silt: dunes, blowouts, and undulating plains: In most places overlies deltaic sediments, coarse lacustrine sediments, or glaciofluvial deposits. |
O | Organic deposits: peat, muck and minor inorganic sediments; large bog, fen, and swamp areas where organic fill masks underlying surficial materials; generally >2 m thick. |
Colluvial Deposits: colluvial and residual materials deposited as veneers and blankets of debris through downslope movement and in place disintegration of bedrock; includes areas of rock outcrop. | |
bC | Colluvial Blocks: Blocks, and rubble with sand and silt; derived from crystalline bedrock, medium grade metamorphic substrate, and cemented sandstone. |
rC | Colluvial Rubble: Rubble and silt; derived from carbonate and consolidated fine classic sedimentary rock substrate. |
fC | Colluvial Fines: Silt, clay, and fine sand: derived from substrate weakly consolidated shale and siltstone substrate. |
sC | Colluvial Sand: Sand and gravel; derived from poorly lithified sandstone and conglomerate substrate. |
Glaciolacustrine and Lacustrine deposits: sediments deposited in a glacial lake during deglaciation and subsequent lake drainage. | |
fM | Fine Grained: Fine grained silt and clay, locally containing stones: deposited as quiet water sediments. |
cL | Coarse Grained: sand, silt, and gravel: deposited as deltas, sheet sands and lag deposits. |
Glaciomarine and Marine Deposits: sediments deposited from meltwater and floating ice, in marine waters, during deglaciation and subsequent regression. | |
fM | Fine Grained: Dominantly silt and clay, locally containing stones; deposited as a quiet water sediment. |
cM | Coarse Grained: Sand and gravel: deposited as sheet sands, deltas, and extensive flights of beaches. |
Mv | Lag: Sand, gravel, and pockets of fine sediment; thin to discontinued sediment veneer and residual lag developed during marine submergence; includes areas of washed till and rock. |
Glaciofluvial Deposits: gravel and sand, deposited by meltwater streams. | |
Gp | Plain: Sand and Gravel: deposited as outwash sheets, valley trains, and terrace deposits. |
Gx | Complex: Sand and gravel and locally diamicton: undifferentiated ice contact stratified drift, and outwash; locally includes till and rock. |
Glacial Deposits: silty, sandy, and clayey diamicton; formed by the direct action of glacier ice. | |
Tb | Till Blanket: Thick and continuous till. |
Tv | Till Veneer: Thin and discontinuous till: may include areas of rock outcrop. |
V | Quarternary Volcanics: consolidated lava, breccia and tephra: dominantly basaltic and andesitic in composition; includes flows, volcanic piles and cinder cones. |
Rock: areas of abundant ( > 75%) rock outcrop. | |
Ra | Alpine Complexes: rock, colluvium, and till: rock and Quarternary deposits complex in an area, characterized by alpine and glacial landforms. |
R | Undivided: rock with minor Quaternary deposits. |
This database does not capture the linear features identified on the "Surficial Materials of Canada". The original source map identifies the former Wisconsin and maximum glaciation ice-limits; general ice flow direction based on drumlins, fluting, etc.; areas of hummocky topography; end and interlobate moraines; and eskers. All are important characterizing features that contribute to the delineation of the ecological units in the national framework.
A table on the back of the "Surficial Materialsof Canada" map lists the sources of surficial materials maps in Canada through 1993.
Source:
Fulton, R. J. (Compiler), 1996. Surficial Materials of Canada, Geological Survey of Canada, Natural Resources Canada. Ottawa. Map 1880A, Scale 1:5 000 000