The earth shattering dam break that created the land form of the Esopus Shoals also formed the Glenerie Breaks and the lower Esopus gorge. The breaks consist of a series of three bedrock shelves of different geological strata that step down in twenty foot drops from the level savanna the Esopus Creek meanders through at the two hundred foot elevation. The flow at the breaks is in an easterly direction diverting the Esopus northward flow in a zig-zag through the breaks to regain the northward flow again deep in the gorge.
The nature of the breaks was scientifically described in detail in an 1835 article for a publication called the Zodiac. What is called a “transit” is run from the base of the Catskill escarpment in a line to the Hudson River going straight through the breaks. It's analysis of the stresses on the rock that forms the cataract steps and the walls that form the break and gorge speculate for the first time on the glaceral lake it calls Lake Albany.
There had been an early saw mill near the top of the breaks but the cascades further in and steep walls made the falls further down nearly inaccessible. Col. Edward Clark managed to overcome the challenge and set up his lead mill inside the gorge in 1831. The person doing the scientific study writes in his article about Clark, his Great Falls Manufacturing Company and the atmosphere of a hermitage he had create at what was called Glen Eirie, or eagles nest.
Col. Clark was a respected civil engineer with many inventions for such things as dry docks and canal locks. His early reputation began during the war of 1812 and his testimony is frequently found in the congressional record. He arrived in Saugerties in a wave of technically oriented people seeking the common ground Henry Barclay had cultivated there.
Edward Clark found Charles Ripley there and they decided to build a processing facility for making lead pigment and grinding it into oils in an oil refinery's empty mill building below Barclay's dam, John Eldridge, Robert L. Livingston's agent, had sitting idle.
This was in the earliest of the shake-down period for applying the water to generating power to the iron and paper mills and the water was being rationed so Clark decided he wanted to experiment with his own water works and began purchasing flood rights for a dam just where the Esopus comes out of the gorge into Barclay's Pond at the second fall. This made bad blood between him and Henry Barclay .
Meanwhile Charles Ripley had attracted the interest of the Jewetts; established lead dealers in New York; for financing the enlargement of the old refinery, creating a rivalry between Ripley and Jewett's lead works and Clark's.
Clark had found that the natural dam at the lowest fall at the breaks had the drop and flow for the power he needed and could be made operational on the same schedule as his rival's expansion.
Recent information shows how quickly this took place. A surveyor's field book details a town road being laid out on both sides of the gorge between the Glasco Turnpike bridge and Clark's home and lead mill. This survey is done in April, 1833 and Clark has a house for himself built on the west side and the mill fully built on the east side of the Esopus Gorge.
When the naturalist stays with Edward Clark while writing the study published in 1835 he marvels at the refinements Clark has made in his solitary Glenerie including an iron cable suspension bridge that spanned the entire gorge.