Geotechnical characteristics of glacial tills (after McGown and Derbyshire (1977))
| Till | Class | Fabric | OCR | Relative comparison of geotechnical propertiesa | |||
|---|---|---|---|---|---|---|---|
| Density | Compressibility | Permeability | Anisotropy | ||||
| Deformation | G | Deformed basal sediments or bedrock | 1 | 5 | 3 | 5–8 | |
| W | |||||||
| Mg | |||||||
| Mc | |||||||
| Lodgement | G | Interlaying of glaciofluvial, joints, fissures, contortions; preferred clast orientation | 2–5 | 4–7 | 1 | 5–6 | 7 |
| W | 5–8 | 2 | 2–3 | ||||
| Mg | 6–8 | 2 | 4–5 | ||||
| Mc | 6–8 | 3 | 2 | ||||
| Melt-out | G | Occasional interlaying with glaciofluvial; clast oriented with englacial state | 1–2 | 2–4 | 2–4 | 7–9 | 3–5 |
| W | 2–6 | 3–5 | 4–5 | ||||
| Mg | 2–6 | 3–6 | 5–8 | ||||
| Mc | 2–7 | 4–7 | 3–4 | ||||
| Till | Class | Fabric | OCR | Relative comparison of geotechnical properties | |||
|---|---|---|---|---|---|---|---|
| Density | Compressibility | Permeability | Anisotropy | ||||
| Deformation | G | Deformed basal sediments or bedrock | 1 | 5 | 3 | 5–8 | |
| W | |||||||
| Mg | |||||||
| Mc | |||||||
| Lodgement | G | Interlaying of glaciofluvial, joints, fissures, contortions; preferred clast orientation | 2–5 | 4–7 | 1 | 5–6 | 7 |
| W | 5–8 | 2 | 2–3 | ||||
| Mg | 6–8 | 2 | 4–5 | ||||
| Mc | 6–8 | 3 | 2 | ||||
| Melt-out | G | Occasional interlaying with glaciofluvial; clast oriented with englacial state | 1–2 | 2–4 | 2–4 | 7–9 | 3–5 |
| W | 2–6 | 3–5 | 4–5 | ||||
| Mg | 2–6 | 3–6 | 5–8 | ||||
| Mc | 2–7 | 4–7 | 3–4 | ||||
1 is low; 9 is high
G, granular till; Mc, matrix till (cohesive); Mg, matrix till (granular); W, well-graded till
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