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The flow of time in the Connecticut valley

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The Flow of Time in the Connecticut Valley
The Flow of Time in the Connecticut Valley
Illustration from The flow of time in the Connecticut valley: geological imprints

Pl. 1. The Connecticut Valley as it is seen from Mount Sugarloaf.

The western highland shows through the pine boughs at the extreme right. The eastern highland balances it on the far left. The Holyoke Range hems the basin on the south except at the gap where the river escapes to the Springfield area.

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