| Page |
| [Introduction] | 9 |
| [Regional relations] | 11 |
| [Rocky River] | 15 |
| [Description of the river and its valley] | 15 |
| [Relation of the valley to geologic structure] | 16 |
| [Junction of Rocky and Housatonic Rivers] | 18 |
| [Abnormal profile] | 18 |
| [Preglacial course] | 20 |
| [The buried channel] | 23 |
| [Effect of glaciation] | 25 |
| | |
| [The Neversink-Danbury valley] | 27 |
| | |
| [Still River] | 30 |
| [Statement of the problem] | 30 |
| [Evidence to be expected if Still River has been reversed] | 31 |
| [A valley wide throughout or broadening toward the south] | 32 |
| [Tributary valleys pointing upstream] | 34 |
| [The regional slope not in accord with the course of the Still] | 35 |
| [Evidence of glacial filling and degrading of the river bed] | 36 |
| [Glacial scouring] | 36 |
| [The Still-Saugatuck divide] | 38 |
| [Features of the Umpog valley] | 38 |
| [The preglacial divide] | 42 |
| [The Still-Croton divide] | 43 |
| [Introduction] | 43 |
| [Features of Still River valley west of Danbury] | 43 |
| [The Still-Croton valley] | 44 |
| [Glacial Lake Kanosha] | 45 |
| [Divides in the highlands south of Danbury] | 46 |
| [The ancient Still River] | 47 |
| [Departures of Still River from its preglacial channel] | 48 |
| | |
| [Suggested courses of Housatonic River] | 50 |
| | |
| [Glacial deposits] | 53 |
| [Beaver Brook Swamp] | 53 |
| [Deposits northeast of Danbury] | 54 |
| [Deposits between Beaver Brook Mountain and mouth of Still River] | 54 |
| [Lakes] | 55 |
| [History of the glacial deposits] | 56 |