Free online GSI calculator based on Hoek 1995. Click your rock mass structure and surface condition on the chart — or enter RMR89 directly. Get instant GSI, Hoek-Brown parameters (mb, s, a), radar chart, and rock mass strength estimates.
Rows = how blocky is the rock mass. Columns = quality of discontinuity surfaces. Click the cell that best describes your site — the intersection gives your GSI range and midpoint.
GSI ≈ RMR89 − 5 (valid only when RMR89 > 23). For RMR89 ≤ 23, switch to Visual Chart — the formula loses accuracy for very poor rock.
D = 0 for undisturbed rock (TBM, careful blasting). D = 1.0 for heavily blasted slopes. Affects Hoek-Brown mb and s — does not change GSI itself.
Select rock type to auto-fill mi, or enter directly. Required to calculate mb = mi × exp((GSI−100)/(28−14D)).
Hoek 1995 — five rock mass quality classes and engineering significance.
| GSI Range | Rock Mass Quality | Description | Engineering Significance |
|---|---|---|---|
| 75–100 | Very Good to Intact | Fresh massive or blocky rock, rough discontinuities | High strength. Tunnels self-supporting. Em > 30 GPa. |
| 55–75 | Good | Blocky, interlocked, good surface condition | Moderate support. Systematic bolting + shotcrete sufficient. |
| 40–55 | Fair | Very blocky to disturbed, fair surface condition | Significant support. Squeezing possible at depth. |
| 25–40 | Poor | Disturbed, heavily jointed, poor surface condition | Heavy support. Deformation monitoring essential. |
| 10–25 | Very Poor | Disintegrated or sheared zones | Very heavy support. Face support often required. |
3 simple steps — takes about 2 minutes with basic field observations.
Everything engineers and students need to know about Geological Strength Index — Hoek 1995.
GSI (Geological Strength Index) was developed by Evert Hoek in 1995. Unlike RMR or Q-System, it was designed specifically as geomechanical input for the Hoek-Brown failure criterion — to estimate rock mass strength from two field observations: degree of blockiness and quality of discontinuity surfaces.
Rock mass UCS: σcm = σci × sa (σci = intact UCS)
For RMR89 > 23: GSI = RMR89 − 5. Convenient but loses accuracy for very poor rock. For RMR89 ≤ 23, estimate GSI directly from the chart — it was specifically calibrated for weak and sheared rock masses where RMR gives unreliable results.
D reduces mb and s only — does NOT change GSI itself.
Hoek-Brown mi values for common rock types — Hoek and Brown 1997.
| Rock Type | Category | mi Value | Typical UCS (MPa) |
|---|---|---|---|
| Granite | Igneous | 28–33 | 100–250 |
| Granodiorite / Diorite | Igneous | 25–29 | 80–200 |
| Gabbro / Diabase | Igneous | 25–27 | 100–300 |
| Basalt | Igneous | 16–25 | 50–250 |
| Sandstone (coarse) | Sedimentary | 17–19 | 20–170 |
| Limestone | Sedimentary | 9–12 | 30–250 |
| Dolostone | Sedimentary | 9–11 | 30–250 |
| Siltstone / Mudstone | Sedimentary | 7–9 | 5–100 |
| Shale | Sedimentary | 6–8 | 5–100 |
| Quartzite | Metamorphic | 20–23 | 150–300 |
| Marble | Metamorphic | 9–25 | 50–200 |
| Gneiss | Metamorphic | 25–30 | 100–250 |
| Schist / Phyllite | Metamorphic | 7–12 | 10–100 |
| Slate | Metamorphic | 7–9 | 25–180 |
Common questions from engineers and students about the GSI system.
Rock classification systems used alongside GSI in geotechnical engineering.
Bieniawski 1989. Most widely used system. Calculate RMR89 first, then GSI = RMR89 − 5 for Hoek-Brown analysis.
Bieniawski 2014 with EQA. More accurate for TBM tunnels. Use base RMR before EQA for GSI correlation.
Barton 1974. Correlates as RMR ≈ 9 ln(Q) + 44. Use alongside GSI to cross-check rock mass quality.
Romana 1985. Extends RMR89 for slope stability with joint-slope orientation corrections.
| GSI Value | — |
| Rock Mass Quality | — |
| RMR89 estimate | — |
| Disturbance D | — |
| mi (intact rock) | — |
| mb (rock mass) | — |
| s | — |
| a | — |
| σcm / σci | — |