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Leave a Reply Cancel reply. Central Park is an urban park in New York City located between the Upper West and Upper East Sides of Manhattan.It is the fifth-largest park in the city by area, covering 843 acres (341 ha). During the last ice age, glaciers dragged rocks across the surface of Manhattan's bedrock, leaving behind the groves and striations that can be seen in Central Park … Stop 10. The northward-flowing Genesee River was partially formed and rerouted by the glacial mass as the ice advanced and retreated across New York all those millions of years ago. Reply. The one I posted earlier came via iPhone, and iPhone cameras are rather low in resolution, especially after pocket-lint accumulates on the unprotected lens. Glacial flows reached down through the state, and as they receded they carved out our Finger Lakes, scenic gorges, and many of our rivers and waterfalls. Type: Park (Public). It is the most visited urban park in the United States with an estimated 38 million visitors annually, and is the most filmed location in the world. lockwooddewitt says: 6 March 2010 at 14:22 If you accept that ice is technically a mineral (and it is), that would make glaciers enormous rocks, and the above a form of slickensides. Glaciers can pick up chunks of rocks and transport them over long distances. Stop 10.Glacial trough and striations on Umpire Rock Photo by Andrew Orgonik. Group sitting around glacial grooves on Umpire Rock listening to Charles Merguerian explain the geology of Manhattan and Central Park Photo by Gil Hanson. D. contains glacial erratics that can be seen in Central Park. Stop 10 Close up of galcial striations and trough. Features: Cambrian Manhattan Formation; metamorphic rock and glacial features; Hartland Formation. Such rocks can be found throughout the park, including the famous "Glacial Boulder" near Inspiration Point in the park. Better shot of glacial striations in Central Park . C. was buried by an ice sheet 250 meters thick during Pleistocene times. The glacial striations are orientated from North to South which show the direction to where the glaciers retreated. Glacial striations, southern Central Park Comments. Photo by Andrew Orgonik. Horenstein explained that during the last ice age glaciers scraped over Manhattan's bedrock, leaving grooves and striations on the otherwise smooth surfaces in Central Park. Such evidence includes: glacial striations, glacial erosion, erratics, roche moutonee. At Umpire Rock in Central Park, overlooking baseball fields, the geologist noted places where glacial ice and rubble had carved massive grooves, wider than a … Posted by Callan Bentley. B. has glacially polished bedrock in Central Park. Central Park consists of many different geologic features with noticeable evidence of glacial history. Glacial erratics dot a field in Yellowstone National Park. 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