It is assumed that a terrain map will be presented on a topographic base map.
The function of the surface expression terms is to augment and highlight
the information provided by the topographic base map. They may describe
features that are not evident from the contours of the map or highlight
the topographic information where necessary. It is recommended that data
provided by the topographic contours (e.g., slope angle and configuration)
be included on a terrain map that is presented on a planimetric base map and if
a terrain map is stored in a computer database.
The surface expression of surficial materials is classified according to
slope, geometric shape and spatial pattern. The surface expression terms
have no genetic implication.
SURFACE EXPRESSION TERMS AND SYMBOLS
Surface Expression
| Surface Expression Name | Map Symbol |
|---|---|
| moderate slope | a |
| blanket | b |
| cone(s) | c |
| depression(s) | d |
| fan(s) | f |
| hummock(s) | h |
| gentle slope | j |
| moderately steep slope | k |
| rolling | m |
| plain | p |
| ridge(s) | r |
| steep slope | s |
| terrace(s) | t |
| undulating | u |
| veneer | v |
| mantle of variable thickness* | w |
| thin veneer* | x |
2a. Thickness of the surficial material is relatively uniform over bedrock or surficial material (3)1b. There is no apparent relation between the topography of the surficial material and that of underlying bedrock or older surficial material; depositional or erosional landforms are present (4)
3a. Thickness of the surface material is less than about 1 m. See VENEER (v) and THIN VENEER (x)2b. Thickness of surface material is variable, ranging from 0 to a few metres; surface material fills or partly fills depressions in an irregular substrate that may be either bedrock or surficial material. See MANTLE OF VARIABLE THICKNESS (w)3b. Thickness of surface material is greater than 1 m. See BLANKET (b)
4a. Simple, constructional or erosional landforms are present, consisting primarily of planar surfaces (5)
5a. Slopes are between 0 and 3° (0-5%). See PLAIN (p)4b. More complex depositional or erosional landforms are present, consisting mainly of multi-directional, non-planar surfaces (6)5b. Slopes are between 4 and 15° (6-26%). See GENTLE SLOPE (j)
5c. Slopes are between 16 and 26° (27-49%). See MODERATE SLOPE (a)
5d. Slopes are between 27 and 35° (50-70%). See MODERATELY STEEP SLOPE (k)
5e. Slopes are steeper than 35° (70%). See STEEP SLOPE (s)
6a. Non-linear rises and hollows with slopes generally less than 15° (26%) See UNDULATING TOPOGRAPHY (u)6b. Elongate rises and hollows with slopes generally less than 15° (26%). See ROLLING TOPOGRAPHY (m)
6c. Non-linear rises and hollows with many slopes steeper than 15° (26%). See HUMMOCKS (h)
6d. Elongate rises with many slopes steeper than 15° (26%). See RIDGES (r)
6e. Hollows, separated from an adjacent gentler surface by a marked break of slope. See DEPRESSIONS (d)
6f. A fan shaped landform that is a sector of a cone: longitudinal gradient less than 15° (26%). See FAN (f)
6g. A fan shaped landform that is a sector of a cone; longitudinal gradient more than 15° (26%). See CONE (c)
6h. Level areas and scarps adjacent downslope. See TERRACES (t)
| Blanket | Hummock(s) | Rolling | Undulating |
| Cone(s) | Gentle Slope | Ridge(s) | Veneer |
| Depression(s) | Moderately Steep Slope | Steep Slope | Mantle of Variable Thickness |
| Fan(s) | Plain | Terrace(s) | Thin Veneer |
| Moderate Slope | Map Symbol: a |
- Does not include the surface expression cone (see CONE below).
- Applied to constructional and erosional slopes in unconsolidated materials, such as the foreset slope of deltas, erosional slopes in weak materials, and some constructional slopes in till and colluvium.
Examples: foreset slope of a delta sgFGa erosional slope in glaciomarine sediments zWGa
| Example: | rock slope with alternating steeper and gentler sections | Ras |
| Example: | colluvial veneer overlying moderately sloping smooth bedrock |
|
| Blanket | Map Symbol: b |
Definition of Surface Expression Terms
A layer of unconsolidated material thick enough to mask minor irregularities of the surface of the underlying unit, but still conforms to the general underlying topography. A blanket is greater than 1 metre thick and possesses no constructional forms typical of the materials' genesis; outcrops of the underlying unit are rare.

Figure 13. Schematic cross-sections that illustrate and distinguish the surface expression terms blanket, veneer, and mantle of variable thickness.
- The surface expression of the blanket is expressed by either the surface expression of the underlying unit, or by the contour lines of the topographic map (Figures 13 and 14).
- If the underlying unit is unconsolidated material, its presence is indicated in a stratigraphic symbol (see Stratigraphic Symbols).
Example: till blanket overlying hummocky
glaciofluvial gravels
- If the underlying unit is bedrock, no stratigraphic information need be supplied, except where the contours of the topographic map do not adequately depict the land surface.
Examples: till blanket overlying bedrock with
surface shape shown by contours
(bedrock-controlled topography)Mb till blanket overlying bedrock with
surface shape not shown by contours
(bedrock-controlled topography)
Figure 14. Schematic cross-sections to illustrate the use of stratigraphic symbols with the surface expression terms blanket, veneer, and mantle of variable thickness. In (d), "Mb" is used alone because contours indicate the long, convex hillside.
| Cone(s) | Map Symbol: c |
Definition of Surface Expression Terms
A cone or segment of a cone with a relatively smooth slope gradient from apex to toe greater than 15° (26%), and a longitudinal profile that is either straight, concave or convex.
Application and Examples:
- A cone is distinguished from a fan on the basis of slope gradient (Figure 15). Refer to FAN.
- Typically applied to talus cones, avalanche cones, coalescing cones where individual cones can be distinguished and volcanic cones of pyroclastic materials.
Examples: talus cones rCc avalanche cones arCc-A cinder cone rVc
- Small volcanic cones may be indicated by on-site symbols (see Other Landforms and Features).

| Depression(s) | Map Symbol: d |
Circular or irregular area of lower elevation (hollow) than the surrounding terrain and marked by an abrupt break in slope; side slopes within the depression are steeper than the surrounding terrain; depressions are two or more metres in depth.
Application and Examples:
- Typically used when mapping deposits containing kettle holes, karst depressions, or depressions caused by piping.
- If map scale permits, the term depression may be applied to a single enclosed depression.
Example: a large kettle in ice-contact materials gsFGd
- The origin of the depression, when known, should be indicated by the use of a "Geomorphological Process" symbol (see Geomorphological Process Terms and Symbols).
Examples: a kettle hole gsFGd-H pitted outwash plain sgFGpd-H glaciolacustrine terrace with depressions caused by piping mLGtd-P
- On-site symbols for kettles, piping depressions, and karst depressions should be used instead of "d" where occurrence is of limited extent in relation to the whole map unit.
| Fan(s) | Map Symbol: f |
Definition of Surface Expression Terms
A fan is a relatively smooth sector of a cone with a slope gradient from apex to toe, up to, and including 15° (26%), and a longitudinal profile that is either straight, concave or convex.
Application and Examples:
- A fan is distinguished from a cone on the basis of slope gradient (Figure 16). Refer to CONE.
- Typically applied to fluvial (alluvial) fans, colluvial fans, or glaciofluvial fans.
Examples: active colluvial fan rCf "relict" fluvial fan sgFf
- Applied to coalescing fans where individual fans are distinguishable.
| Hummock(s) | Map Symbol: h |
Definition of Surface Expression Terms
Steep sided hillock(s) and hollow(s) with multidirectional slopes dominantly between 15 and 35° (26 to 70%) if composed of unconsolidated materials; bedrock slopes may be steeper. Local relief is greater than 1 metre. In plan, an assemblage of non-linear, generally chaotic forms that are rounded or irregular in cross-profile.
Application and Examples:
- Hummocky unconsolidated materials are sufficiently thick to mask the surface irregularities of the underlying unit (Figure 17).
- Hummocky topography is distinguished from undulating topography on the basis of the predominant slope angles. Refer to UNDULATING TOPOGRAPHY.
- Commonly applied to knob-and-kettle topography, some landslide deposits, and hummocky bedrock.
Examples: kame-and-kettle glaciofluvial sediments gsFGh-H landslide debris mdCh till mantle of variable thickness overlying
hummocky bedrock (till is thin on crests
and thicker in depressions)
| Gentle Slope | Map Symbol: j |
An unidirectional (planar) surface with a slope gradient greater than 3° , to and including 15° (5 to 26%), and a smooth, longitudinal profile that is either straight, concave or convex; local surface irregularities generally have a relief of less than 1 metre.
Application and Examples:
- Does not include the surface expression fan. Refer to FAN.
- Applied to constructional slopes underlain by till or glaciofluvial materials, gently sloping beaches, and the floodplains of steep creeks.
Examples: floodplain of a steep creek bgFAj thick till with gentle slopes and minor surface irregularities dmMj
- Not applied to till or colluvium, or other material on bedrock-controlled slopes.
Example: till 2-3 m thick covering gently
sloping bedrock
Figure 16. Examples of the surface expression terms rolling, ridged, undulation and hummocky. (a) Rolling till plain made up of low, gently sloping drumlinoid features on the Nahlin Plateau in the northwest corner of British Columbia (map symbol: Mm). (b) Drumlinized till plain on the McGregor Plateau; the drumlins are linear features characterized by steep slopes (map symbol: Mr). (c) Undulating glaciomarine deposit in the Fraser Valley characterized by gentle slopes and irregularly distributed swales (map symbol: WGu). (d) Till hummocks with steep slopes in the Interior of British Columbia (map symbol: Mh).
| Moderately Steep Slope | Map Symbol: k |
Definition of Surface Expression Terms
An unidirectional (planar) surface with a slope gradient greater than 26° , to and including 35° (50 to 70%), and a smooth, longitudinal profile that is either straight, concave or convex; local surface irregularities generally have a relief of less than 1 metre.
Application and Examples:
- Does not include the surface expression cone. Refer to CONE.
- Applied to constructional and erosional slopes in unconsolidated materials, such as scarps resulting from stream erosion, gully side-scarps, ice-contact slopes and talus slopes.
Examples: scarp of glaciofluvial terrace gFGk side-slopes of gully eroded into till Mk
- Applied to erosional slopes in bedrock, and to rock where rock controlled slopes are covered by till, colluvium or other materials.
Examples: moderately steep sloping bedrock Rk colluvial veneer overlying moderately
steep, smooth bedrock
| Rolling Topography | Map Symbol: m |
Definition of Surface Expression Terms
Elongate hillock(s) with slopes dominantly between 3 and 15° (5 to 26%) with local relief greater than 1 metre. In plan, an assemblage of parallel or sub-parallel linear forms with subdued relief.
Application and Examples:
- Rolling topography is distinguished from ridged topography on the basis of predominatly gentler slopes (Figure 17). Refer to RIDGE(S).
- Rolling unconsolidated materials are sufficiently thick to mask the surface irregularities of the underlying material.
- Commonly applied to fluted till plains, swell-and-swale topography, and subdued, beach and bedrock ridges.
Examples: "washboard" moraine Mm beach strandlines Wm
- Where rolling topography is the result of glaciation and reflects former ice-flow direction, the appropriate on-site symbols should be applied to the terrain map (e.g., drumlins, flutings, and roches moutonnées. See Glacial Features).
Example: grooved till plain Mm
(with appropriate
on-site symbol)
| Plain | Map Symbol: p |
Definition of Surface Expression Terms
A level or very gently sloping, unidirectional (planar) surface with gradients up to, and including 3° (5%); local surface irregularities generally have a relief of less than 1 metre.
Application and Examples:
- Commonly applied to floodplains, deep organic deposits, lacustrine and marine plains, and the level portions of terraces and deltas (Figure 18).
Examples: active floodplain sgFAp thick organic deposit Op silty lacustrine plain zLp
Figure 17. Level to very gently sloping (<3°) active delta deposit (map symbol: sgFAp) (location of photo: Port Hardy, Vancouver Island).
| Ridge(s) | Map Symbol: r |
Definition of Surface Expression Terms
Elongate hillock(s) with slopes dominantly between 15 and 35° (26 to 70%) if composed of unconsolidated materials; bedrock slopes may be steeper. Local relief is greater than 1 metre. In plan, an assemblage of parallel or sub-parallel linear forms.
Application and Examples:
- Ridged unconsolidated materials are sufficiently thick to mask the irregularities of the underlying material surface.
- Ridged topography is distinguished from rolling topography on the basis of predominatly steeper slopes (Figure 17). Refer to ROLLING.
- Commonly applied to drumlinized till plains, eskers, morainal ridges, crevasse fillings and ridged bedrock.
Examples: sandy gravel esker sgFGr till mantle of variable thickness
overlying bedrock ridges
- Where ridged topography is the result of glaciation and reflects former ice-flow direction, the appropriate on-site symbols should be applied to the terrain map (e.g., drumlins, flutings, and roche moutonnées. See Glacial Features).
Example: drumlinized till plain Mr (with appropriate
on-site symbol)
| Steep Slope | Map Symbol: s |
Definition of Surface Expression Terms
An unidirectional (planar) surface with gradients greater than 35° (70%), and a smooth longitudinal profile that is either straight, concave or convex; local surface irregularities generally have a relief of less than 1 metre; bedrock slopes may be more irregular.
Application and Examples:
- Most commonly applied to steep erosional slopes of unconsolidated materials, such as terrace scarps, river banks and lake shore bluffs, steep bedrock slopes such as cliffs and steep slopes overlain with colluvium.
Examples: cirque headwall Rs lakeshore bluff LGs escarpment of a river terrace Fs steep-sided gully in thick till (gully
comprises entire polygonMs-V
- Where the map scale does not permit the delineation of a scarp, an on-site symbol should be applied to indicate the scarp location and extent (see Other Landforms and Features).
Example: multiple fluvial terraces with
narrow scarpsFt (with scarp symbols)
| Terrace(s) | Map Symbol: t |
Definition of Surface Expression Terms
A single or assemblage of step-like forms where each step-like form consists of a scarp face and a horizontal or gently inclined surface (tread) above it.
Application and Examples:
- Terrace is applied to both the scarp and the flat tread, that is, to the whole feature in the landscape; includes river and lake terraces, kame terraces and structurally-controlled, stepped topography (Figure 18).
Examples: river terrace gsFt stepped bedrock topography Rt
- In units comprising more than one terrace, individual terrace scarps can be designated by a scarp on-site symbol (see Other Landforms and Features).
Figure 18. Terraces made up of thick Quaternary sediments (map symbol: FGt) (location of photo: Churn Creek near the Gang Ranch).
| Undulating Topography | Map Symbol: u |
Definition of Surface Expression Terms
Gently sloping hillock(s) and hollow(s) with multidirectional slopes generally up to 15° (26%); local relief is greater than 1 metre. In plan, an assemblage of non-linear, generally chaotic forms that are rounded or irregular in cross-profile.
Application and Examples:
- Undulating topography made up of unconsolidated materials sufficiently thick to mask the surface irregularities of the underlying material.
- Undulating topography is distinguished from hummocky topography on the basis of the predominantly gentler slopes (Figure 17). Refer to HUMMOCK(S).
- Commonly applied to undulating till plains, some landslide and dune deposits, and some ice-contact deposits.
Examples: undulating till plain Mu dunes on river terrace discrete areas of kame hummocks and undulations FGhu
| Veneer | Map Symbol: v |
Definition of Surface Expression Terms
A mantle of unconsolidated materials too thin to mask the minor irregularities of the surface of the underlying material. It is between about 10 cm to 1 metre in thickness and possesses no constructional form typical of the material genesis.
Application and Examples:
- The surface topography of the veneer is indicated by either the surface expression of the underlying unit, or as expressed by the contour lines of the topographic map (Figures 13 and 14).
- When the underlying unit is unconsolidated material, its presence must be indicated by stratigraphic information, (see Stratigraphic Units).
Example: sandy eolian veneer overlying
river terrace gravels
- If the underlying unit is bedrock, no stratigraphic information need be supplied, except where the contours of the topographic map do not adequately depict the land surface.
Examples: colluvial veneer overlying bedrock
with surface shape shown by contoursCv colluvial veneer overlying bedrock
with surface shape not shown by contours
- If veneer (v) and thin veneer (x) are used together, e.g., Cvx, then v indicates material 20 cm to 1 m thick, and x indicates material thinner than 20 cm.
| Mantle of Variable Thickness* | Map Symbol: w |
Definition of Surface Expression Terms
A layer or discontinuous layer of surficial material of variable thickness (typically 0 to 3 m) that fills or partly fills depressions in an irregular substrate. It is generally too thin to mask prominent irregularities in the underlying material (see figure 14c).
Application and Examples:
*Note: This is a new term (1997).
- Similar to blanket and veneer.
- Mantle of variable thickness is draped over the underlying material and has no constructional form of its own.
Examples: mantle of variable thickness over
hummocky rock (Figure 13c)mantle of glaciolacustrine sediments
over hummocky till (Figure 14b)
| Thin Veneer* | Map Symbol: x |
Definition of Surface Expression Terms
A very thin layer of unconsolidated material about 2-20 cm in thickness.
Application and Examples:
*Note: This is a new term (1997).
- Similar to veneer. Intended primarily for bioterrain mapping that is to be used as the basis for ecosystem mapping.
- If veneer (v) and thin veneer (x) are used together, e.g., Cvx, then v indicates material 20 cm to 1 m thick, and x indicates material thinner than 20 cm.
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