Compare Terrain (2006) - Terrain (2004)

Compare Terrain (2006) with Terrain (2004)

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	Terrain (2006)	Terrain (2004)
Arctic Ocean	central surface covered by a perennial drifting polar icepack that, on average, is about 3 meters thick, although pressure ridges may be three times that thickness; clockwise drift pattern in the Beaufort Gyral Stream, but nearly straight-line movement from the New Siberian Islands (Russia) to Denmark Strait (between Greenland and Iceland); the icepack is surrounded by open seas during the summer, but more than doubles in size during the winter and extends to the encircling landmasses; the ocean floor is about 50% continental shelf (highest percentage of any ocean) with the remainder a central basin interrupted by three submarine ridges (Alpha Cordillera, Nansen Cordillera, and Lomonosov Ridge)	central surface covered by a perennial drifting polar icepack that averages about 3 meters in thickness, although pressure ridges may be three times that size; clockwise drift pattern in the Beaufort Gyral Stream, but nearly straight-line movement from the New Siberian Islands (Russia) to Denmark Strait (between Greenland and Iceland); the icepack is surrounded by open seas during the summer, but more than doubles in size during the winter and extends to the encircling landmasses; the ocean floor is about 50% continental shelf (highest percentage of any ocean) with the remainder a central basin interrupted by three submarine ridges (Alpha Cordillera, Nansen Cordillera, and Lomonosov Ridge)
British Indian Ocean Territory	flat and low (most areas do not exceed two meters in elevation)	flat and low (most areas do not exceed four meters in elevation)
Guatemala	mostly mountains with narrow coastal plains and rolling limestone plateau	mostly mountains with narrow coastal plains and rolling limestone plateau (Peten)
Holy See (Vatican City)	urban; low hill	low hill
Iles Eparses	Bassas da India: atoll, awash at high tide; shallow (15 m) lagoon Europa Island, Glorioso Islands, Juan de Nova Island: low, flat, and sandy Tromelin Island: low, flat, sandy; likely volcanic seamount	-
Montenegro	highly indented coastline with narrow coastal plain backed by rugged high limestone mountains and plateaus	-
Nepal	Tarai or flat river plain of the Ganges in south, central hill region, rugged Himalayas in north	Terai or flat river plain of the Ganges in south, central hill region, rugged Himalayas in north
Saint Helena	the islands of this group result from volcanic activity associated with the Atlantic Mid-Ocean Ridge Saint Helena: rugged, volcanic; small scattered plateaus and plains Ascension: surface covered by lava flows and cinder cones of 44 dormant volcanoes; ground rises to the east Tristan da Cunha: sheer cliffs line the coastline of the nearly circular island; the flanks of the central volcanic peak are deeply dissected; narrow coastal plain lies between The Peak and the coastal cliffs	Saint Helena - rugged, volcanic; small scattered plateaus and plains note: the other islands of the group have a volcanic origin
Serbia	extremely varied; to the north, rich fertile plains; to the east, limestone ranges and basins; to the southeast, ancient mountains and hills	-
Serbia and Montenegro	-	extremely varied; to the north, rich fertile plains; to the east, limestone ranges and basins; to the southeast, ancient mountains and hills; to the southwest, extremely high shoreline with no islands off the coast
United States Pacific Island Wildlife Refuges	low and nearly level sandy coral islands with narrow fringing reefs that have developed at the top of submerged volcanic mountains, which in most cases rise steeply from the ocean floor	-
Wake Island	atoll of three low coral islands, Peale, Wake, and Wilkes, built up on an underwater volcano; central lagoon is former crater, islands are part of the rim	atoll of three coral islands built up on an underwater volcano; central lagoon is former crater, islands are part of the rim

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