Nonstop flight route between New York City, New York, United States and College Park, Maryland, United States:
Departure Airport:

Arrival Airport:

Distance from JRA to CGS:
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- About this route
- JRA Airport Information
- CGS Airport Information
- Facts about JRA
- Facts about CGS
- Map of Nearest Airports to JRA
- List of Nearest Airports to JRA
- Map of Furthest Airports from JRA
- List of Furthest Airports from JRA
- Map of Nearest Airports to CGS
- List of Nearest Airports to CGS
- Map of Furthest Airports from CGS
- List of Furthest Airports from CGS
About this route:
A direct, nonstop flight between West 30th Street Heliport (JRA), New York City, New York, United States and College Park Airport (CGS), College Park, Maryland, United States would travel a Great Circle distance of 197 miles (or 317 kilometers).
A Great Circle is the shortest distance between 2 points on a sphere. Because most world maps are flat (but the Earth is round), the route of the shortest distance between 2 points on the Earth will often appear curved when viewed on a flat map, especially for long distances. If you were to simply draw a straight line on a flat map and measure a very long distance, it would likely be much further than if you were to lay a string between those two points on a globe. Because of the relatively short distance between West 30th Street Heliport and College Park Airport, the route shown on this map most likely still appears to be a straight line.
Departure Airport Information:
IATA / ICAO Codes: | JRA / KJRA |
Airport Name: | West 30th Street Heliport |
Location: | New York City, New York, United States |
GPS Coordinates: | 40°45'16"N by 74°0'24"W |
Area Served: | New York City |
Operator/Owner: | Hudson River Park Trust |
Airport Type: | Public |
Elevation: | 7 feet (2 meters) |
View all routes: | Routes from JRA |
More Information: | JRA Maps & Info |
Arrival Airport Information:
IATA / ICAO Codes: | CGS / KCGS |
Airport Name: | College Park Airport |
Location: | College Park, Maryland, United States |
GPS Coordinates: | 38°58'50"N by 76°55'20"W |
Operator/Owner: | Maryland-National Capital Park & Planning Commission |
Airport Type: | Public |
Elevation: | 48 feet (15 meters) |
# of Runways: | 1 |
View all routes: | Routes from CGS |
More Information: | CGS Maps & Info |
Facts about West 30th Street Heliport (JRA):
- The furthest airport from West 30th Street Heliport (JRA) is Margaret River Airport (MGV), which is located 11,750 miles (18,910 kilometers) away in Margaret River, Western Australia, Australia.
- The closest airport to West 30th Street Heliport (JRA) is East 34th Street Heliport (TSS), which is located only 2 miles (3 kilometers) ESE of JRA.
- Because of West 30th Street Heliport's relatively low elevation of 7 feet, planes can take off or land at West 30th Street Heliport at a lower air speed than at airports located at a higher elevation. This is because the air density is higher closer to sea level than it would otherwise be at higher elevations.
- Since this is a heliport and not an airport, there are no Instrument Procedures.
Facts about College Park Airport (CGS):
- In 1920, Emile and Henry Berliner brought their theories of vertical flight to the field and in 1924 made the first controlled helicopter flight.
- The furthest airport from College Park Airport (CGS) is Margaret River Airport (MGV), which is located 11,684 miles (18,803 kilometers) away in Margaret River, Western Australia, Australia.
- The closest airport to College Park Airport (CGS) is Bolling Air Force Base (BOF), which is located only 11 miles (17 kilometers) SSW of CGS.
- College Park Airport (CGS) currently has only 1 runway.
- The road to the airport is named in honor of Corporal Frank S.
- In April 1910, the Aero Club of America chapters from Washington and Baltimore chose the College Park Airport for the next James Gordon Bennett Race.
- Because of College Park Airport's relatively low elevation of 48 feet, planes can take off or land at College Park Airport at a lower air speed than at airports located at a higher elevation. This is because the air density is higher closer to sea level than it would otherwise be at higher elevations.