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A Quaker school, Sandy Spring Friends School, was established in 1961. In 1967 a Quaker retirement community, Friends House, was founded next to the school. The Sandy Spring Library opened behind the Sandy Spring Store in 1842. [1] The Farmer's Club of Sandy Spring was established in 1844 to discuss preferable methods of farming. [1]
Sandy Spring Friends Meetinghouse: Sandy Spring Friends Meetinghouse: September 22, 1972 : 17715 Meeting House Road: Sandy Spring: Large, Flemish bond brick, Federal-style Quaker Meeting House built in 1817. 64
Ashton-Sandy Spring is a census-designated place (CDP) in Montgomery County, Maryland, United States. The CDP is designated to include the two unincorporated communities of Ashton and Sandy Spring, as well as the smaller community of Brinklow. It had a population of 5,746 as of the 2020 census. [3]
Hart-Miller Island State Park: Baltimore: 244 acres 99 ha 1977: Back River Chesapeake Bay: Accessible only by boat; 3,000-foot (910 m) sandy beach Herrington Manor State Park: Garrett: 365 acres 148 ha 1964: Herrington Creek: Swimming, non-motorized boating, picnicking, hiking, tennis, volleyball, cabins Janes Island State Park: Somerset: 3,160 ...
The Sandy Spring Friends Meetinghouse is a historic building located at Sandy Spring, Montgomery County, Maryland. It is a large, Flemish bond brick, Federal-style Quaker Meeting House built in 1817. The meetinghouse is on two acres deeded by James Brooke in the 1750s, for the use of the Quaker Meeting. Nearby is the cemetery where he and many ...
Sandy Spring Museum's exhibits include a replica of a 19th-century classroom, a replica of a blacksmith's shop, a replica of a general store, and a tractor made from a Model T Ford. [8] [6] The museum has archived more than 15,000 artifacts and photographs from the area around Sandy Spring. [6] Some of its collection dates back to 1650. [6]
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The Northwest Branch underneath the Green and Yellow Lines of the Washington Metro near the West Hyattsville station The Northwest Branch at the Fall Line. Northwest Branch crosses the geological fall line between the Piedmont and Atlantic coastal plain regions, which forms a small waterfall on the stream 0.5 miles (0.80 km) south of the Burnt Mills Dam parks. [7]