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Quarry Lake is a manmade lake in the Pikesville area of Baltimore County, Maryland.Originally a marble quarry, it is now one of the deepest lakes in the state. The lake is surrounded by Quarry Lake at Greenspring, a mixed residential development and commercial development that includes single-family homes, condominiums, shops, and office buildings.
Google Earth is a web and computer program that renders a 3D representation of Earth based primarily on satellite imagery.The program maps the Earth by superimposing satellite images, aerial photography, and GIS data onto a 3D globe, allowing users to see cities and landscapes from various angles.
Liberty Reservoir is a reservoir west of Baltimore, Maryland; about a mile north of Patapsco Valley State Park's McKeldin area. It is owned by the City of Baltimore Department of Public Works, but is located outside the city, and it divides Baltimore and Carroll Counties.
Google Maps' satellite view is a "top-down" or bird's-eye view; most of the high-resolution imagery of cities is aerial photography taken from aircraft flying at 800 to 1,500 feet (240 to 460 m), while most other imagery is from satellites. [5]
There are seven mainline sections of MD 144: MD 144 in Allegany County runs 17.55 miles (28.24 km) from MD 807 in Cumberland east to US 40 Scenic east of Flintstone. The state highway generally parallels I-68 and crosses over the freeway multiple times as both highways pass through mountainous creek valleys and over Martin Mountain and Polish Mountain.
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The lake is contained within the bounds of Lake Roland Park, which was established in the 1920s and supervised by the newly organized Baltimore City Department of Parks and Recreation. [ 8 ] [ 9 ] The lake is an artificial impoundment created by a dam on the Jones Falls and two smaller streams, Towson Run and Roland Run.
The Cockeysville Marble is a Precambrian, Cambrian, or Ordovician marble formation in Baltimore, Carroll, Harford and Howard Counties, Maryland. It is described as a predominantly metadolomite, calc-schist, and calcite marble, with calc-gneiss and calc-silicate marble being widespread but minor.