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along with the Mersey estuary are the two largest iceways discerned in this region. Further iceways were identified underlying the lower
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is a linear channel eroded through bedrock by the passage of glacial ice. The term was coined by
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Ronald Kay
Gresswell in a paper in 1964 in relation to the origins of the
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R K Gresswell, 1964 Origins of the Dee and Mersey
Estuaries
52:. The Dee estuary and its landward continuation south of
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68:. Each of these have also been referred to as
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64:valley and the Alt-Ditton depression east of
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32:on the boundary of northwest
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56:as far as
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22:geographer
66:Liverpool
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44:through
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54:Chester
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62:Gowy
28:and
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