Figures and tables

Figures

(Figure 1) Aspects of the Quaternary geology and geomorphology of Wales and the Welsh borderland (after Bowen 1977a, 1982b)

(Figure 2) Some proposed ice limits on Gower (from Bowen 1970a; Bowen 1981a, 1981b; Campbell 1984; Bowen et al. 1985)

(Figure 3) Quaternary sequence at Hunts Bay (after Bowen and Henry 1984)

(Figure 4) Pleistocene sequence at Bacon Hole Cave (from Currant et al. 1984)

(Figure 5) Pleistocene sequence at Minchin Hole (from Sutcliffe and Currant 1984)

(Figure 6) Quaternary sequence at Eastern Slade and Western Slade (after Bowen and Henry 1984)

(Figure 7) Quaternary sequence at Horton (after Bowen and Henry 1984)

(Figure 8) Quaternary sequence at Rhosili Bay (after Campbell 1984)

(Figure 9) Quaternary sequence at Broughton Bay (after Campbell et al. 1982)

(Figure 10) Quaternary deposits at Ynyslas and Borth Bog (after Godwin 1943)

(Figure 11) Quaternary sequence at Clarach (from Heyworth et al. 1985)

(Figure 12) Pleistocene sequence at Morfa-bychan (after Watson and Watson 1967)

(Figure 13) Drift provinces of South Wales (from Bowen 1970a)

(Figure 14) Some suggested Late Devensian ice limits in South Wales (from Bowen and Henry 1984; Campbell 1984)

(Figure 15) The Gwaun–Jordanston meltwater channel system (from Bowen and Henry 1984)

(Figure 16) The Maesyprior meltwater channel system (after Bowen 1970a)

(Figure 17) The Cledlyn Valley pingos (after Watson 1971; Watson and Watson 1972)

(Figure 18) Mynydd Du: principal landforms (after Ellis-Gruffydd 1972; Statham 1976)

(Figure 19) Traeth Mawr: a summary of pollen, lithological and radiocarbon evidence (from Walker 1984)

(Figure 20) Craig Cerrig-gleisiad: a summary of pollen, lithological and radiocarbon evidence (from Walker 1984)

(Figure 21) Quaternary sequence at Cwm Nash (after Evans et al. 1978)

(Figure 22) Cadair Idris: principal landforms (after Watson 1977a)

(Figure 23) Cwm Ystwyth: principal landforms (after Watson 1966; Watson and Watson 1977)

(Figure 24) Llyn Gwernan: a summary of pollen, lithological and radiocarbon evidence (from Lowe et al. 1988)

(Figure 25) Elan Valley Bog: Devensian late-glacial and Holocene sequence (from Moore and Chater 1969a)

(Figure 26) Tregaron Bog: a summary of pollen, lithological and radiocarbon evidence (from Hibbert and Switsur 1976)

(Figure 27) Late Devensian and Late Devensian readvance ice limits (from Bowen 1974, 1977b)

(Figure 28) Quaternary sequence at Dinas Dinlle (from Whittow and Ball 1970)

(Figure 29) Pleistocene sequence at Gwydir Bay (from Saunders 1968d)

(Figure 30) Pleistocene sequence at Porth Oer (from Saunders 1968d)

(Figure 31) Quaternary sequence at Porth Neigwl (from Saunders 1968d)

(Figure 32) Quaternary sequence at Porth Ceiriad (from Whittow and Ball 1970)

(Figure 33) Quaternary sequence at Glanllynnau (after Whittow and Ball 1970; Boulton 1977a)

(Figure 34) Quatemary sequence at Morannedd (from Whittow and Ball 1970)

(Figure 35) Quaternary sequence at Pontnewydd (after Green et al. 1981)

(Figure 36) Snowdon (Yr Wyddfa): principal landforms

(Figure 37) Y Glyderau: principal landforms (after Campbell 1985b)

(Figure 38) Y Carneddau: principal landforms

(Figure 39) Devensian late-glacial and Holocene sequence at Cors Geuallt (after Crabtree 1972)

Tables

(Table 1) Geochronology (age) of Oxygen Isotope Stage boundaries is from Martinson et al. (1987) [back to stage 7], and Imbrie et al. (1984). Specific events are radiocarbon dated at 10, 11, 12, 13, 14 and 17,000 years BP (details in text). The Pennard and Minchin Hole D/L Stages are from Bowen et al. (1985). For chronostratigraphic correlations see Bowen and Sykes (1988), Behre (1989) and Bowen et al. (1989). Sites outside Wales are correlated with Oxygen Isotope Stages as follows — Upton Warren, St Germain II and Odderade (Sub-stage 5a), Chelford, BrOrup and St Germain I (Sub-stage 5c) and Stanton Harcourt and Aveley (Stage 7).

(Table 2) Gower chronology (T N George 1932)

(Table 3) Uranium-series age determinations on stalagmite samples from Bacon Hole.

References