Fig. 10.6 The Vergennes soil
series is a Glossaquic Hapludalfs
derived from calcareous estuarine
and glaciolacustrine clays in the
eastern Lake Ontario basin. The
exposure is from a road cut of the
upper 25 cm.The photo is from
the soil survey of Essex County,
NY (Smith 2010)
Fig. 10.7 Schematic landscape cross-section showing the relationship of soils on the Iroquois Plain between the Niagara Escarpment and Lake
Ontario. Source The Soils of the Regional Municipality of Niagara, ON, Vol. 1 (Kingston and Presant 1989)
10.2 Soils by Natural Resource Segment
133
series is a Glossaquic Hapludalfs
derived from calcareous estuarine
and glaciolacustrine clays in the
eastern Lake Ontario basin. The
exposure is from a road cut of the
upper 25 cm.The photo is from
the soil survey of Essex County,
NY (Smith 2010)
Fig. 10.7 Schematic landscape cross-section showing the relationship of soils on the Iroquois Plain between the Niagara Escarpment and Lake
Ontario. Source The Soils of the Regional Municipality of Niagara, ON, Vol. 1 (Kingston and Presant 1989)
10.2 Soils by Natural Resource Segment
133
