Authors:
VANWEERT FHA
VANGIJSSEL K
LEIJNSE A
BOULTON GS
Citation: Fha. Vanweert et al., THE EFFECTS OF PLEISTOCENE GLACIATIONS ON THE GEOHYDROLOGICAL SYSTEM OF NORTHWEST EUROPE, Journal of hydrology, 195(1-4), 1997, pp. 137-159
Authors:
BOULTON GS
CABAN PE
VANGIJSSEL K
LEIJNSE A
PUNKARI M
VANWEERT FHA
Citation: Gs. Boulton et al., THE IMPACT OF GLACIATION ON THE GROUNDWATER REGIME OF NORTHWEST EUROPE, Global and planetary change, 12(1-4), 1996, pp. 397-413
Authors:
BOULTON GS
VANDERMEER JJM
HART J
BEETS D
RUEGG GHJ
VANDERWATEREN FM
JARVIS J
Citation: Gs. Boulton et al., TILL AND MORAINE EMPLACEMENT IN A DEFORMING BED SURGE - AN EXAMPLE FROM A MARINE-ENVIRONMENT, Quaternary science reviews, 15(10), 1996, pp. 961-987
Citation: Gs. Boulton, THEORY OF GLACIAL EROSION, TRANSPORT AND DEPOSITION AS A CONSEQUENCE OF SUBGLACIAL SEDIMENT DEFORMATION, Journal of Glaciology, 42(140), 1996, pp. 43-62
Citation: Gs. Boulton et P. Caban, GROUNDWATER-FLOW BENEATH ICE SHEETS .2. ITS IMPACT ON GLACIERTECTONICSTRUCTURES AND MORAINE FORMATION, Quaternary science reviews, 14(6), 1995, pp. 563-587
Citation: Mr. Bennett et Gs. Boulton, DEGLACIATION OF THE GLENFINNAN AREA, WESTERN SCOTLAND, FOLLOWING THE LOCH-LOMOND STADIAL - A REPLY, JQS. Journal of quaternary science, 9(4), 1994, pp. 382-383
Authors:
BOULTON GS
SLOT T
BLESSING K
GLASBERGEN P
LEIJNSE T
VANGIJSSEL K
Citation: Gs. Boulton et al., DEEP CIRCULATION OF GROUNDWATER IN OVERPRESSURED SUBGLACIAL AQUIFERS AND ITS GEOLOGICAL CONSEQUENCES, Quaternary science reviews, 12(9), 1993, pp. 739-745
Citation: Mr. Bennett et Gs. Boulton, DEGLACIATION OF THE YOUNGER DRYAS OR LOCH-LOMOND STADIAL ICE-FIELD INTHE NORTHERN HIGHLANDS, SCOTLAND, JQS. Journal of quaternary science, 8(2), 1993, pp. 133-145
Citation: Gs. Boulton et Ke. Dobbie, CONSOLIDATION OF SEDIMENTS BY GLACIERS - RELATIONS BETWEEN SEDIMENT GEOTECHNICS, SOFT-BED GLACIER DYNAMICS AND SUBGLACIAL GROUNDWATER-FLOW, Journal of Glaciology, 39(131), 1993, pp. 26-44
Citation: Mr. Bennett et Gs. Boulton, A REINTERPRETATION OF SCOTTISH HUMMOCKY MORAINE AND ITS SIGNIFICANCE FOR THE DEGLACIATION OF THE SCOTTISH HIGHLANDS DURING THE YOUNGER DRYAS OR LOCH-LOMOND STADIAL, Geological Magazine, 130(3), 1993, pp. 301-318