Letchworth State Park

Letchworth State Park is located in western New York. It is here that the North-flowing Genesee Grand Canyon of the EastRiver has been carving it's way through these layers of rock since the end of the last ice advance. Rapid erosion rates make for steep canyon walls and spectacular scenery. The Geometry of the river valley takes on a winding course and is essentially an incised meander, or a deeply etched sinusoidal pattern, where at the level of the high cliff-tops the water once flowed in semi-circular loops.The wide canyon here was a large glacial lake when the Wisconsin (most recent) ice sheet occupied the region twenty-two thousand years ago.


The layers of rock you see here were all deposited in shallow seas that advanced and retreated several times during the Paleozoic era, about up until the Late Devonian period when continental collisions on the eastern side of New York raised the land and drained the water away. This location is at a higher elevation than Niagara Falls and buries the Lockport Dolostone formation, though further downstream the dolomite is exposed. Primary rock types are Sandstone, and Shale. An interesting notion about these layers is that they dip 35-50 feet every mile you travel to the south; a product, no doubt, of the countless mountain building episodes on the Eastern Flank of New York since the of the Devonian Period.


Upper Falls Lower Falls

Three waterfalls are located within a two mile stretch. As the Wisconsin Ice Sheet melted away, it would create lakes within the gorge. As the ice got further and further from one waterfall, a new one would develope. In this manner the first waterfall to develope was the upper falls (left). When the lake level dropped, the Middle Falls developed, and so-on as the lower falls (right) began to erode. The waterfalls similarly share a common trait: that each of them spill over erosion-resistent sandstone layers.


Breaking all the rules, Baby!!

Observe shear nonconformity. Shale, flaking away as it weathers in this formation contrasts with the more resilient sandstone.


Of all the places in New York I remember being to, I have not seen a more tranquil place to just walk around and observe. The scenery here can not be fully appreciated in this web page, you have to go see it yourself. The scene makes for an ideal romantic getaway, a good hike among several trails, great biking, clear air, several historic NY sites--including a canal and train bridge, varieties of plant/animal life, and just down-right awesome nature.