2.2 The visual analysis: reading the site and the face
The visual analysis is the half of soil classification everyone believes they are already doing. In practice "I looked at it" means looking at the face. Appendix A (d)(1) asks for seven specific observations, only two of which are about the face — the rest are about the site, the spoil, the layers, the water and the traffic going past. This chapter is that list, and how to run it in about five minutes.
1 What the visual analysis is for
Appendix A (d)(1) states the purpose: visual analysis is conducted to determine qualitative information about the excavation site in general, the soil adjacent to the excavation, the soil forming the sides of the open excavation, and the soil taken as samples from excavated material.
Four subjects, then: the site, the ground next to the hole, the walls, and the spoil. And (d)(3) sets the standard of care — the visual and manual analyses "shall be designed and conducted to provide sufficient quantitative and qualitative information as may be necessary to identify properly the properties, factors, and conditions affecting the classification."
2 The seven observations
| ¶ | What you observe | What it tells you |
|---|---|---|
| (i) | Samples of excavated soil and the soil in the sides: estimate the range of particle sizes and their relative amounts | Primarily fine-grained material = cohesive. Primarily coarse sand or gravel = granular, therefore Type C |
| (ii) | Soil as it is excavated: does it stay in clumps? | Stays in clumps = cohesive. Breaks up easily and does not stay in clumps = granular |
| (iii) | The opened side and the surface next to it: crack-like openings, tension cracks, chunks spalling off a vertical side, small spalls | Fissured material; small spalls are evidence of moving ground and indications of potentially hazardous situations |
| (iv) | Evidence of existing utilities and other underground structures, and previously disturbed soil | Previously disturbed soil cannot be Type A; utilities change the dig entirely |
| (v) | The opened side, to identify layered systems — and whether the layers slope toward the excavation; estimate the degree of slope | Layers dipping into the cut at 4H:1V or steeper make the material Type C |
| (vi) | Surface water, water seeping from the sides, the level of the water table | Submerged or freely seeping soil is Type C; water is also its own hazard under 651(h) |
| (vii) | Sources of vibration that may affect the stability of the face | Vibration disqualifies Type A; heavy traffic and pile driving are named in the standard |
Three of the seven — (iv), (v) and (vii) — cannot be answered by looking at the wall at all. Previously disturbed soil is a records-and-history question. Layer dip is geometry read across the whole face. Vibration is a question about the street, the plant next door and your own compactor.
3 Previously disturbed soil: the invisible disqualifier
Appendix A gives no definition of "previously disturbed," and it does not need one: any ground that has been excavated and put back is disturbed. Backfill is not the same material it was, however long ago it went in and however well it was compacted.
Where to look for it, in rough order of how often it catches crews:
- The old utility trench you are paralleling or crossing. Utility corridors are layers of other people's backfill.
- Any dig inside a graded subdivision, a parking lot subgrade or an engineered fill.
- The second pass. The moment you re-open your own trench, the soil in it is disturbed.
- Trees, stumps and old foundations removed and the void filled.
- Anything near a structure: the excavation for the footing was backfilled against the wall.
The visual clue is a change in color, texture or particle mix that runs vertically rather than horizontally — a seam of different material where an old trench wall used to be. If you can see the outline of somebody else's excavation in your face, that side is disturbed.
4 Reading layers and their dip
Appendix A (d)(1)(v) asks you to identify a layered system and estimate whether the layers slope toward the excavation, and how steeply. That matters because the dip angle changes the class outright: layers dipping into the cut at 4H:1V or steeper put the material in Type C; less steeply than 4H:1V, and Type B (vi) may apply if the material would otherwise be Type B.
4H:1V is a shallow angle — 14 degrees, one unit down for four along. It looks nearly flat on a trench face. Interpreting it needs the whole face, not a patch: sight along the seam from one end of the open cut to the other and see whether it rises or falls toward you.
5 A five-minute route around the excavation
- 1Start at the spoil: particle sizes, does it clump, is there a seam of different material in the pile?
- 2Walk the full length of each open face: cracks, spalling, ravelling, seams and their dip, any change in color or texture.
- 3Look at the ground surface 10 to 15 feet back from each edge: tension cracks parallel to the trench, subsidence, old pavement patches marking a buried trench.
- 4Look for water: standing water, damp bands on the face, seepage at a seam, the bottom going soft.
- 5Stand still and feel the ground: traffic on the street, a compactor, a pile driver, your own excavator tracking past.
- 6Write down the class and the two analyses that support it, on the daily inspection record, with your name.
The last step is the one that turns an opinion into a classification. The standard does not prescribe a form, and OSHA does not require a specific record here — but a class with no name attached is not a decision anybody can inherit at shift change.
6 What the visual analysis cannot tell you
It cannot give you strength. Type A and Type B are separated by unconfined compressive strength — 1.5 tsf — and no amount of looking produces that number. That is why (c)(2) requires a manual analysis as well, and why "we looked at it and it's good clay" is half a classification at best.
It also cannot tell you what is behind the face. The failure surface of a cave-in develops in the soil behind the wall you are looking at, which is why the signs in Appendix B — subsidence at the edge, tension cracks back from the lip — matter as much as the face itself. Chapter 2.3 puts hands on the soil.
- Appendix A (d)(1) lists seven observations covering the site, the adjacent ground, the faces and the spoil — not just the wall.
- Soil that stays in clumps when excavated is cohesive; soil that breaks apart is granular, and granular is Type C.
- Small spalls and ravelling are evidence of moving ground, not cosmetic damage.
- Previously disturbed soil cannot be Type A, and backfill stays disturbed no matter how old or well compacted.
- Layers dipping into the excavation at 4H:1V or steeper make the material Type C; a layered system otherwise takes its weakest layer.
- The visual analysis cannot produce a strength figure, which is why at least one manual analysis is also required.
Free educational content — not OSHA-authorized training, no certificate or card issued. Follow your employer's program and the standards cited.