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PE Geotechnical Slope Stability: 5 Problem Types You'll See on Exam Day

Five slope-stability problem types on the PE Geotechnical exam — infinite slope, wedge, Ordinary, Bishop's, seismic — with worked NCEES examples.

PEwise Team
April 29, 2026

You can solve a bearing-capacity problem in two minutes and find a settlement under a footing in your sleep. Then a slope-stability question lands in front of you, the slip surface is already drawn, the water table is shown, and you stall — because the question is asking you to pick between an Ordinary-Method-of-Slices answer and a Bishop's-Simplified answer, and the difference between the two is roughly the difference between passing and not.

Slope stability is one of the highest-weighted topics on the PE Geotechnical exam, and it shows up in two distinct sub-topics: static analysis under Topic 5 (Earth Structures) and seismic analysis under Topic 4 (Earthquake Engineering and Dynamic Loads). It also rewards engineers who treat it as a calculation discipline rather than a theory chapter. Most online prep posts on this topic walk you through the concepts and stop. This one walks you through the five problem types NCEES can build a question around — with worked numerical examples and the formulas you'll actually punch into your calculator on exam day.

You'll learn how to recognize each problem type from the prompt within ten seconds, which equation to reach for, where the trap is in the wording, and how to navigate the on-screen reference library — the NCEES PE Civil Reference Handbook plus the full searchable PDFs of USACE EM 1110-2-1902, FHWA NHI-06-088/089, and FHWA-NHI-11-032 — without losing time.

Why slope stability dominates the PE Geotechnical exam

Per the NCEES April 2024 PE Civil Geotechnical specification — the current spec (last revised April 2024; the next revision is April 2027) — Topic 5, Earth Structures, Ground Improvement, and Pavement, carries 9–14 questions. Sub-topic 5C, "Slope stability evaluation and slope stabilization," is one of three calculation-heavy areas inside that block. Topic 4, Earthquake Engineering and Dynamic Loads, adds another 5–8 questions, and sub-topic 4B explicitly calls out "Seismic analyses and design (e.g., liquefaction, pseudo static, earthquake loads)" — pseudo-static is a slope-stability question dressed in seismic language.

Combined, that's a realistic 4–7 questions on the 80-question exam where slope stability is the underlying skill. Miss those and your safety margin against a fail evaporates. Land them and you've banked roughly 5–9% of the exam from a single chapter of mechanics.

The exam is closed-book with electronic references. Alongside the PE Civil Reference Handbook, NCEES supplies full searchable PDFs of USACE EM 1110-2-1902 (Slope Stability), FHWA NHI-06-088/089 (Soils and Foundations Reference Manual, Volumes I and II), and FHWA-NHI-11-032 / GEC No. 3 (LRFD Seismic Analysis and Design of Transportation Geotechnical Features) — the last of which is the seismic slope-stability standard. The handbook itself excerpts only the cohesionless infinite-slope formula, the Ordinary Method slice decomposition, and a guideline table that tells you to use Bishop's. Bishop's full derivation lives in EM 1110-2-1902; pseudo-static slope analysis lives in NHI-11-032. Standards open one chapter at a time, so retrieval speed is the skill — knowing which document and which chapter to open before you click is what separates candidates who finish on time from those who don't.

The core concepts you must master

Effective stress and the Mohr-Coulomb envelope

Every slope-stability calculation reduces to a single question: is the available shear strength along the failure surface greater than the driving shear stress? Available shear strength comes from Mohr-Coulomb:

τf = c′ + σ′ tan φ

where c′ is effective cohesion, σ′ is effective normal stress on the failure plane, and φ′ is the effective friction angle. Effective stress is total stress minus pore pressure: σ′ = σu. Skip this step and you'll overestimate strength by exactly the pore-pressure term, which is usually how candidates accidentally turn an unstable slope into a stable one on paper.

Drained versus undrained shear strength

For long-term, slow-loading conditions in granular or stiff fine-grained soils, use drained strength (c′, φ′). For short-term loading on saturated clays — end-of-construction embankments, rapid drawdown — use undrained strength (su, total-stress φ = 0). The PE exam will tell you which condition applies; circle the keyword "long-term," "end-of-construction," or "rapid drawdown" before you set up any equation.

Pore-water pressure and seepage

A water table at the surface with seepage parallel to the slope is the single most common pore-pressure scenario on the exam. It can cut a granular slope's factor of safety by roughly 50% versus the same slope dry. The NCEES handbook (§3.6.4) parameterizes pore pressure with the coefficient:

ru = u / (γ h)

where h is the depth to the slip surface. For steady seepage parallel to the slope at full saturation, ru = (γw / γsat) cos2β — at typical exam slope angles (β = 15°–25°) that's roughly 0.45–0.50.

Limit equilibrium and factor of safety

Limit-equilibrium methods assume a failure surface, sum the resisting and driving forces (or moments), and compute:

F = (resisting shear strength) / (driving shear stress)

Standard targets per USACE EM 1110-2-1902: F ≥ 1.5 for long-term static, ≥ 1.3 for temporary or end-of-construction, and ≥ 1.0–1.1 for seismic pseudo-static. NCEES will sometimes ask you to identify which threshold applies — the answer depends on loading duration, not on the slope's geometry.

The 5 problem types you'll see on exam day

1. Infinite slope analysis

Recognize it from a long, planar slope with a shallow failure plane parallel to the surface — typically a thin layer of weathered material over rock, or a clean sand fill on a uniform grade.

The NCEES handbook §3.6.4 gives the cohesionless infinite-slope FoS in two forms. No pore water pressure (ru = 0):

F = tan φ′ / tan β

With pore water pressure:

F = (tan φ′ / tan β) × [1 − ru(1 + tan2β)]

For the common exam case — water table at the surface, steady seepage parallel — substituting ru = (γw / γsat) cos2β reduces the second form to the textbook short form:

F = (γ′ / γsat)(tan φ′ / tan β)

Either form gives the same FoS; use whichever is faster given how the prompt states pore pressure.

The handbook does not provide a c′-φ′ infinite-slope form. For cohesive infinite slopes with seepage, the standard extension — derived in FHWA NHI-06-088 Chapter 6 (Eq. 6-9) and worth committing to memory — is:

F = c′ / (γsat h cos2β tan β) + (γ′ / γsat)(tan φ′ / tan β)

Worked example. A 6-m-thick sand layer rests on impermeable bedrock at a uniform 20° slope. Soil properties: φ′ = 32°, c′ = 0, γsat = 19.0 kN/m3. The water table sits at the ground surface and steady seepage runs parallel to the slope. Compute the factor of safety against shallow translational failure using the NCEES handbook formula.

Step 1 — Pore-pressure coefficient. For seepage parallel at full saturation:

ru = (γw / γsat) cos2β = (9.81 / 19.0)(cos2 20°) = 0.516 × 0.883 = 0.456

Step 2 — Apply the handbook formula:

F = (tan φ′ / tan β)[1 − ru(1 + tan2β)]

Step 3 — Plug in:

F = (0.6249 / 0.3640) × [1 − 0.456(1.133)] = 1.717 × 0.484 = 0.83

Answer: F ≈ 0.83 — the slope is unstable under steady seepage. Dry, the same slope would give F = tan 32° / tan 20° = 1.72, which illustrates how punishing pore pressure is on cohesionless slopes.

2. Planar / wedge failure analysis

Recognize it from a single rigid block sliding on one inclined plane — rock cuts, a weak seam in stratified ground, geotechnical reinforcement problems with one critical interface. Geometry is given; you sum forces along and normal to the slip plane.

Driving force = W sin α
Resisting force = cL + (W cos αU) tan φ
F = Resisting / Driving

where W is the weight of the wedge per unit length, α is the inclination of the slip plane, L is the length of the slip plane, and U is the resultant water uplift along that plane.

The exam trap here is forgetting U, the uplift due to a tension crack or a daylighting water table behind the wedge. Always check whether the prompt mentions a piezometric surface — if it does, U is non-zero.

3. Method of slices: Ordinary (Fellenius) method

Recognize it from a circular slip surface drawn through layered soil, with a table of slice geometry (W, α, b or l, sometimes u). The Ordinary Method ignores inter-slice forces, which makes it conservative for circular failures with high pore pressure but easy to compute by hand. The NCEES handbook §3.6.5 gives the slice decomposition for effective-stress analysis as W′ = Wub and N′ = (Wub) cos α, where b is the horizontal width of the slice. The FoS itself is not written out in the handbook — you compute it as:

F = Σ [cl + (Wub) cos α · tan φ′] / Σ (W sin α)

where l is the length of the slip-plane base of each slice. The summation runs over every slice. Each slice contributes a resisting term (top of the fraction) and a driving term (bottom). Be careful with sign conventions on α — slices on the passive side of the slip circle have negative α and contribute negative driving force.

4. Method of slices: Bishop's simplified method

Recognize it from the same circular slip surface, but the question gives you enough information to iterate, or it explicitly references "Bishop's simplified" in the prompt. Bishop accounts for normal inter-slice forces (but not shear) and is more accurate than Ordinary — typically 5–20% higher for the same slip surface.

The NCEES handbook §3.6.6 explicitly directs you to use Bishop's Method for granular soils and most cohesive analyses — but the equation itself is not in the handbook. The full derivation is in USACE EM 1110-2-1902 Appendix C-3 (and FHWA NHI-06-088 §6.4), both searchable on exam day, but you don't want to be looking it up cold. Have the form ready:

F = (1 / Σ W sin α) × Σ {[cb + (Wub) tan φ′] / mα}
mα = cos α + (sin α tan φ′) / F

Bishop's is implicit — F appears on both sides, so you iterate. Start with the Ordinary FoS as the seed value, recompute mα for each slice, recompute F, and stop when successive values agree to within ~0.01. Two iterations is usually enough on the exam.

Worked example. A trial circular slip surface through a homogeneous c′-φ′ soil is divided into three slices with the geometry below. Soil: c′ = 10 kPa, φ′ = 25°. Pore pressure is zero along the slip surface. Compute the FoS by the Ordinary Method of Slices.

SliceW (kN/m)α (°)l (m)
1120503.0
2200252.5
390−102.2

Step 1 — Driving sum Σ W sin α:

120 sin 50° + 200 sin 25° + 90 sin(−10°) = 91.93 + 84.52 − 15.63 = 160.82 kN/m

Step 2 — Resisting term per slice (cl + W cos α tan φ′, with u = 0):

Slice 1: 10(3.0) + 120 cos 50° tan 25° = 30 + 35.97 = 65.97
Slice 2: 10(2.5) + 200 cos 25° tan 25° = 25 + 84.52 = 109.52
Slice 3: 10(2.2) + 90 cos(−10°) tan 25° = 22 + 41.32 = 63.32
Σ resisting = 238.81 kN/m

Step 3 — FoS:

F = 238.81 / 160.82 = 1.48

Answer: F ≈ 1.48 by the Ordinary Method — just below the long-term static target of 1.5. Recomputing by Bishop's Simplified would raise this by roughly 5–10% to ~1.55–1.62, which would clear the threshold. NCEES often pairs the two methods to test whether you know that the Ordinary Method is conservative.

5. Seismic / pseudo-static slope stability

Recognize it from any mention of an earthquake coefficient kh or kv, design ground motion, or seismic FoS. The pseudo-static method replaces dynamic loading with an equivalent static horizontal force khW (and sometimes a vertical force kvW) acting through the slope's center of mass.

The NCEES handbook §3.1.5 covers Mononobe-Okabe pseudo-static analysis for retaining walls only — pseudo-static slope analysis lives in FHWA-NHI-11-032 / GEC No. 3, §6.2.2 (Limit Equilibrium Pseudo Static Stability Analysis), the seismic geotechnical standard NCEES supplies as a searchable PDF. One subtlety worth knowing: EM 1110-2-1902 App. C-3 explicitly cautions that the Simplified Bishop Method is questionable for pseudo-static analysis because it doesn't satisfy horizontal equilibrium — the recommended seismic methods are Modified Swedish, Simplified Janbu, or Spencer's. For a dry cohesionless infinite slope:

Fseismic = [(cos βkh sin β) tan φ′] / (sin β + kh cos β)

For circular failure, the same modification flows through every slice: the driving term becomes W(sin α + kh cos α) and the effective-normal-stress term becomes W(cos αkh sin α). The acceptable seismic FoS is typically 1.0–1.1, not 1.5 — because the design earthquake load is itself rare.

Choosing kh is itself an exam question. Common rules of thumb cited in USACE EM 1110-2-1902 and FHWA-NHI-11-032 are kh = ½ × peak ground acceleration (PGA) for dams and embankments, and kh = ⅔ × PGA for permanent slopes where some displacement is acceptable.

A multi-concept worked problem

Step 1: Read the prompt and pick the method

A 5-m-thick saturated silty sand layer sits on impermeable rock at a uniform 18° slope. φ′ = 30°, c′ = 5 kPa, γsat = 18.5 kN/m3. The water table is at the ground surface with seepage parallel to the slope. Design ground motion gives PGA = 0.30g; the agency uses kh = ½ PGA. Compute the static and seismic factors of safety against shallow translational failure and report whether the slope meets long-term static and seismic targets.

The shallow failure surface and uniform geometry make this an infinite-slope problem. We need the c′-φ′ form because c′ ≠ 0.

Step 2: Static FoS with seepage

γ′ = 18.5 − 9.81 = 8.69 kN/m3. With h = 5 m, β = 18°:

Fstatic = c′ / (γsat h cos2β tan β) + (γ′ / γsat)(tan φ′ / tan β)
= 5 / (18.5 × 5 × 0.9045 × 0.3249) + (8.69 / 18.5)(0.5774 / 0.3249)
= 0.184 + 0.835 = 1.02

Step 3: Seismic FoS

kh = 0.5 × 0.30 = 0.15. cos 18° = 0.951, sin 18° = 0.309. The seismic driving denominator is (sin β + kh cos β) = 0.309 + 0.15(0.951) = 0.452. The seismic force khW acts on the total weight, so γ′/γsat multiplies only the cos β term in the friction numerator:

Friction term = [(γ′/γsat) cos βkh sin β] tan φ′ / (sin β + kh cos β)
= [(8.69/18.5)(0.951) − (0.15)(0.309)] × 0.5774 / 0.452
= [0.447 − 0.046] × 0.5774 / 0.452
= 0.231 / 0.452 = 0.511

Cohesion term = c′ / [γsat h cos β (sin β + kh cos β)]
= 5 / (18.5 × 5 × 0.951 × 0.452) = 5 / 39.78 = 0.126

Fseismic ≈ 0.126 + 0.511 = 0.64

Step 4: Interpret

Fstatic ≈ 1.02 fails the 1.5 target — the slope is marginal even before the earthquake. Fseismic ≈ 0.64 fails the 1.0 floor — the slope is predicted to fail under the design earthquake. Stabilization is required: drainage to lower the water table, flattening the slope, or a structural toe buttress. NCEES will often ask the follow-up: which intervention raises FoS most efficiently? The answer is almost always drainage, because pore-pressure removal lifts both the static and seismic FoS at once.

See Slope Stability Come to Life

PEwise's PE Geotechnical course uses animated videos to visualize slip-surface geometry, pore-pressure distributions, and pseudo-static force diagrams. When you can SEE how the friction term shrinks under earthquake loading, the equations stop being abstract.

Common errors that cost points

Mixing total and effective stress

If you have c′ and φ′, you must use σ′ = σu. Plugging total normal stress into a Mohr-Coulomb equation that calls for effective normal stress is the single most common slip in this topic.

Forgetting uplift on wedge problems

A piezometric surface daylighting on the slip plane creates an uplift U that subtracts from the normal force. Candidates routinely set U = 0 because the prompt didn't draw a separate water-pressure diagram.

Wrong factor-of-safety threshold

A 1.3 FoS on a permanent embankment is a fail; a 1.3 FoS on a temporary excavation is acceptable. Read the loading description before you read the FoS.

Bishop's iteration without seeding

Starting Bishop's Simplified with F = 1.0 wastes iterations. Seed with the Ordinary Method result — Bishop's typically converges in two iterations from a good seed.

Sign errors on α in slices

Slices on the passive (toe) side of the slip circle have negative α. If you square them or take absolute values, your driving moment will be wrong by 10–20%.

Using kh that doesn't match the agency standard

"PGA" and "kh" are not the same number. Most agencies use kh between ½ and ⅔ of PGA. The prompt will tell you which — read it before you set up the equation.

How to study slope stability effectively

Phase 1 — Build the conceptual scaffold (Week 1)

Read NCEES PE Civil Reference Handbook §3.6 (Slope Stability) end-to-end so you know what the handbook itself contains. Then read FHWA NHI-06-088 Chapter 6 (static slope stability — Eq. 6-9 is the c′-φ′ infinite-slope form, §6.4 covers the slice methods), USACE EM 1110-2-1902 Chapter 3 (Table 3-1 FoS criteria) and Appendix C-3 (Bishop's derivation), and FHWA-NHI-11-032 §6.2 (seismic slope stability, including the pseudo-static method in §6.2.2). Every one of these is searchable on exam day — Phase 1 is about indexing them in your head so you know which document and which section to open in the on-screen reference.

Phase 2 — Drill the five problem types (Weeks 2–3)

Work three problems of each type from a question bank. Time yourself: six minutes per problem is the exam pace. PEwise's complete PE Geotechnical exam prep course covers each of the five problem types with animated worked examples in Module 7.

Phase 3 — Integrate seismic and static (Week 4)

Solve five mixed problems where you must compute both static and seismic FoS for the same slope and compare against thresholds. This is the integration the exam tests.

Phase 4 — Reference-library practice (Week 5)

Solve every remaining slope problem with only the on-screen library open — handbook for the cohesionless infinite slope and OMS slice geometry, EM 1110-2-1902 for Bishop's, NHI-11-032 for pseudo-static. You're not training calculation — you're training retrieval speed: which document, which chapter, which figure, in under thirty seconds.

Quick reference: slope stability formulas and typical FoS values

ItemExpression / ValueNotes
Mohr-Coulomb (effective)τf = c′ + σ′ tan φσ′ = σu
Pore-pressure coefficientru = u / (γ h)NCEES handbook §3.6.4
Infinite slope, no pore pressureF = tan φ′ / tan βHandbook §3.6.4 (ru = 0)
Infinite slope, with pore pressureF = (tan φ′ / tan β)[1 − ru(1 + tan2β)]Handbook §3.6.4
Infinite slope c′-φ′, seepage parallelF = c′ / (γsat h cos2β tan β) + (γ′ / γsat)(tan φ′ / tan β)FHWA NHI-06-088 Eq. 6-9 (§6.3.2)
Ordinary Method of SlicesF = Σ [cl + (Wub) cos α · tan φ′] / Σ W sin αSlice form per handbook §3.6.5; FHWA NHI-06-088 §6.4
Bishop's SimplifiedF = (1 / Σ W sin α) × Σ {[cb + (Wub) tan φ′] / mα}mα = cos α + sin α tan φ′ / F; iterate. EM 1110-2-1902 App. C-3
Pseudo-static (infinite, dry, c′ = 0)F = (cos βkh sin β) tan φ′ / (sin β + kh cos β)kh ≈ ½–⅔ PGA. FHWA-NHI-11-032 §6.2.2
Long-term static targetF ≥ 1.5USACE EM 1110-2-1902
Temporary / end-of-constructionF ≥ 1.3USACE EM 1110-2-1902
Pseudo-static seismicF ≥ 1.0–1.1Agency-dependent

Connecting this to your overall PE exam strategy

Slope stability sits at the intersection of effective-stress mechanics, shear-strength selection, and limit-equilibrium accounting. The same three skills carry through bearing capacity, retaining-wall stability, and seepage problems — which is why getting slope stability right tends to pull the rest of Topic 5 along with it. If you're still struggling to recognize when a question demands drained versus undrained strength, start with our geotechnical PE exam study guide, then come back to this post and rework the five problem types.

If you've been failing diagnostic exams in this section specifically, the issue is usually pattern recognition rather than mechanics — every NCEES slope-stability question is one of the five problem types above. Diagnose which type you keep mis-classifying using why you keep failing the PE Geotechnical exam, then drill that one type until you can identify it within ten seconds of reading the prompt. For the conceptual half of Topic 5 — when the exam asks you to choose a stabilization strategy rather than compute an FoS — see PE Geotechnical exam conceptual questions.

Final thoughts

The five problem types above account for essentially every slope-stability question NCEES has asked since the April 2024 spec took effect. As you build toward exam day, treat each type as a small drillable skill: see it, name it, reach for the formula, plug in cleanly, check the FoS threshold. The candidates who lose points on this topic aren't the ones who don't know the theory — they're the ones who can't decide between the Ordinary Method and Bishop's in the first thirty seconds. Make that decision automatic and the points come with it.

Master Slope Stability with PEwise

PEwise's PE Geotechnical course breaks slope stability into clear, visual explanations across all five problem types — infinite slope, planar wedge, Ordinary Method of Slices, Bishop's Simplified, and pseudo-static seismic — with worked examples and animated diagrams of each failure mechanism. Course author Mahdi Bahrampouri, Ph.D., is a Geotechnical Earthquake Engineer whose research specialty is exactly seismic slope stability.