NCEES FS·Section 2 · Mapping Processes and Methods

Digital Terrain Models

Machine control, TINs, digital surface models, digital elevation models — the surface representations modern surveying produces.

The hook

A DTM (Digital Terrain Model) is the surface itself — not a map of it. Civil software grades, computes volumes, and renders 3D from a DTM. Two dominant representations: TIN (Triangulated Irregular Network — the surface as triangular facets) and grid DEM (a regular array of elevations). Each has trade-offs the exam will test.

TINirregular triangles, dense where neededGrid DEM949698100989694929092949694929088868890929088868482848688868482807880828482807876747678807876747270727476747270686668707270686664uniform cells, each holds elevation
Same surface, two representations. TIN preserves breaklines and varies triangle density with terrain. Grid DEM samples uniformly — easy to process but smooths out features.
Memorize these

Concepts that show up on the exam

TIN (Triangulated Irregular Network)
A surface model built by Delaunay-triangulating the survey points. Each triangle has its own slope; breaklines are honored as edges. Memory-efficient for variable terrain density.
Grid DEM (Digital Elevation Model)
A raster where each cell holds an elevation. Easy to process (uniform indexing), simple math (slope = (Δz/Δx) cell-by-cell). Can be huge for large areas.
DTM vs. DEM vs. DSM
DTM = bare-earth terrain. DEM is generic — could be either. DSM (Digital SURFACE Model) includes vegetation + buildings. Lidar produces a DSM first; "ground filtering" extracts the DTM.
Breakline
A line in the surface where slope changes sharply (curb edge, ridgeline, top of bank). TINs honor these as triangle edges; DEMs only honor them if you raster-burn them in.
Contour from DTM
Civil software interpolates contour lines from the DTM at the requested interval. Quality of contours = quality of the underlying DTM.
Cut/fill from DTM
Compute the volume difference between two DTMs (existing vs. proposed). Foundational to earthwork estimation, mass diagrams, grading design.
TINGrid DEM
StorageVertices + edges (compact for variable terrain)Every cell stored (huge for large areas)
BreaklinesNative — triangle edges follow featuresMust be burned into the raster
Slope analysisPer-triangle (variable size)Per-cell (uniform; faster)
Edit-friendlinessMust re-triangulate after editsEdit one cell value, re-derive products
Common usesCivil 3D, site grading, ALTA topoLidar, regional terrain, SRTM
Don't fall for these

What trips people up

TIN extrapolation outside the data
A TIN only knows about the area enclosed by its outermost triangles. Pulling contours just past the edge invents elevations from nothing. Always restrict the analysis area to the surveyed extent.
Grid DEM at the wrong resolution
A 30 m DEM is great for a watershed; useless for a parking lot. The cell size IS the spatial resolution. Don\'t infer cm-level features from m-level cells.
Mixing DSM and DTM
If you compute a building footprint elevation by sampling a DSM, you get the roof, not the slab. Always confirm whether you\'re working with bare-earth or surface data.
Test yourself

How well did it stick?

A quick 5-question check on Digital Terrain Models. See where you stand and what to review.

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