Matches in DBpedia 2016-04 for { ?s ?p "The Geology of Washington, D.C. is broadly divisible into two regions. The northwestern quadrant of the city lies mainly in the Appalachian Piedmont region, marked by moderate to steep hills underlain by metamorphic rocks of Ordovician through Devonian age, similar to the adjacent Piedmont regions of Montgomery County, Maryland."@en }
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- Geology_of_Washington,_D.C. comment "The Geology of Washington, D.C. is broadly divisible into two regions. The northwestern quadrant of the city lies mainly in the Appalachian Piedmont region, marked by moderate to steep hills underlain by metamorphic rocks of Ordovician through Devonian age, similar to the adjacent Piedmont regions of Montgomery County, Maryland.".
- Q5535410 comment "The Geology of Washington, D.C. is broadly divisible into two regions. The northwestern quadrant of the city lies mainly in the Appalachian Piedmont region, marked by moderate to steep hills underlain by metamorphic rocks of Ordovician through Devonian age, similar to the adjacent Piedmont regions of Montgomery County, Maryland.".