Nonstop flight route between College Park, Maryland, United States and Funafuti, Tuvalu:

About this route:

A direct, nonstop flight between College Park Airport (CGS), College Park, Maryland, United States and Funafuti International Airport (FUN), Funafuti, Tuvalu would travel a Great Circle distance of 7,332 miles (or 11,800 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 large distance between College Park Airport and Funafuti International Airport, the route shown on this map most likely appears curved because of this reason.

Try it at home! Get a globe and tightly lay a string between College Park Airport and Funafuti International Airport. You'll see that it will travel the same route of the red line on this map!

Departure Airport Information:

Arrival Airport Information:

Facts about College Park Airport (CGS):

• The museum offers changing exhibits, special events, lectures, workshops and programs for the public, schools and groups.
• Since the 9/11 attacks, and owing to the airport's proximity to the national capital, the operations of the airport have been severely restricted by the Transportation Security Administration in the interest of national security, but civilian pilots are still free to use the airport after going through a one-time background check procedure.
• College Park Airport (CGS) currently has only 1 runway.
• 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.
• 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.
• College Park Airport was established in August 1909 by the United States Army Signal Corps to serve as a training location for Wilbur Wright to instruct two military officers to fly in the government's first aeroplane.
• 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.
• George Brinckerhoff took over management of the Airfield and ran it from 1927 until 1959, hosting numerous airshows and teaching hundreds of pilots to fly during his tenure.
• 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.

Facts about Funafuti International Airport (FUN):

• The closest airport to Funafuti International Airport (FUN) is Arorae Island Airport (AIS), which is located 440 miles (708 kilometers) NNW of FUN.
• Funafuti Airport was built by United States Navy Seabee construction battalions in 1943 during World War II.
• The furthest airport from Funafuti International Airport (FUN) is Tamale Airport (TML), which is nearly antipodal to Funafuti International Airport (meaning Funafuti International Airport is almost on the exact opposite side of the Earth from Tamale Airport), and is located 12,365 miles (19,900 kilometers) away in Tamale, Northern Region, Ghana.
• Funafuti International Airport (FUN) currently has only 1 runway.
• Because of Funafuti International Airport's relatively low elevation of 9 feet, planes can take off or land at Funafuti International 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.
• The deterioration of the runway's sub-base is a consequence of its low elevation and the hydrologic dynamics in the sub-surface of the atoll.