Iceland is an island country at the confluence of the North Atlantic and Arctic oceans, east of Greenland and immediately south of the Arctic Circle, atop the constructive boundary of the northern Mid-Atlantic Ridge. The island country is the world's 18th largest in area and one of the most sparsely populated. It is the westernmost European country when not including Greenland and has more land covered by glaciers than continental Europe. Its total size is 103,125 km2 (39,817 sq mi) and possesses an exclusive economic zone of 751,345 km2 (290,096 sq mi).
A waterfall is any point in a river or stream where water flows over a vertical drop or a series of steep drops. Waterfalls also occur where meltwater drops over the edge of a tabular iceberg or ice shelf.
Multnomah Falls is a waterfall located on Multnomah Creek in the Columbia River Gorge, east of Troutdale, between Corbett and Dodson, Oregon, United States. The waterfall is accessible from the Historic Columbia River Highway and Interstate 84. Spanning two tiers on basalt cliffs, it is the tallest waterfall in the state of Oregon at 620 ft (189 m) in height. The Multnomah Creek Bridge, built in 1914, crosses below the falls, and is listed on the National Register of Historic Places.
Goðafoss is a waterfall in northern Iceland. It is located along the country's main ring road at the junction with the Sprengisandur highland road, about 45 minutes from Akureyri. The water of the river Skjálfandafljót falls from a height of 12 metres over a width of 30 metres. A 1.8-mile hiking trail loops around the waterfall area.
Dettifoss is a waterfall in Vatnajökull National Park in Northeast Iceland, and is reputed to be the second most powerful waterfall in Europe after the Rhine Falls. Dettifoss is situated on the Jökulsá á Fjöllum river, which flows from the Vatnajökull glacier and collects water from a large area in Northeast Iceland. The sediment-rich runoff colours the water a greyish white.
Eyjafjallajökull, sometimes referred to by the numeronym E15, is one of the smaller ice caps of Iceland, north of Skógar and west of Mýrdalsjökull. The ice cap covers the caldera of a volcano with a summit elevation of 1,651 metres (5,417 ft). The volcano has erupted relatively frequently since the Last Glacial Period, most recently in 2010, when, although relatively small for a volcanic eruption, it caused enormous disruption to air travel across northern and western Europe for a week.
Snæfellsjökull is a 700,000-year-old glacier-capped stratovolcano in western Iceland. It is situated on the westernmost part of the Snæfellsnes peninsula. Sometimes it may be seen from the city of Reykjavík over Faxa Bay, at a distance of 120 km (75 mi).
Skógafoss is a waterfall on the Skógá River in the south of Iceland at the cliff marking the former coastline. After the coastline had receded, the former sea cliffs remained, parallel to the coast over hundreds of kilometres, creating together with some mountains a clear border between the coastal lowlands and the Highlands of Iceland.
Glymur is a waterfall in Hvalfjarðarsveit, Vesturland, Iceland. It is the second-tallest in the country with a cascade of 198 metres (650 ft). Glymur was long regarded as the tallest until being surpassed by Morsárfoss, a newly measured waterfall near Morsárjökull in 2011.
The Skjálfandafljót River is situated in the north of Iceland. Skjálfandafljót is 178 kilometres (111 mi) long, and is the fourth longest river of Iceland.
Kirkjubæjarklaustur is a village in the south of Iceland on the hringvegur between Vík í Mýrdal and Höfn. It is part of the municipality of Skaftárhreppur and has about 500 inhabitants. It is surrounded by hills and plateaus to the north. Kirkjubæjarklaustur is roughly 190 kilometres (120 mi) east of the capital Reykjavik.
Route 1 or the Ring Road is a national road in Iceland that circles the entire country. As a major trunk route, it is considered to be the most important piece of transport infrastructure in Iceland as it connects the majority of towns together in the most densely populated areas of the country. Economically, it carries a large proportion of goods traffic as well as tourist traffic. The total length of the road is 1,322 kilometres (821 mi).
Delaware Water Gap National Recreation Area is a 70,000-acre (28,000 ha) national recreation area administered by the National Park Service in northwest New Jersey and northeast Pennsylvania. It is centered around a 40-mile (64 km) stretch of the Delaware River designated the Middle Delaware National Scenic River. At the area's southern end lays the Delaware Water Gap, a dramatic mountain pass where the river cuts between Blue Mountain and Kittatinny Mountain.
Skaftafell is a preservation area in Öræfi, southeast Iceland. It was once a major farm, later being named a national park. Originally known as Skaftafell National Park, it was subsequently joined together with other nearby regions to form the larger Vatnajökull National Park.
Selfoss is a waterfall on the river Jökulsá á Fjöllum in the north of Iceland. The river drops over a number of waterfalls over about 30 km before flowing into Öxarfjörður, a bay of the Arctic Sea. The river originates as melt water from the glacier Vatnajökull and therefore the water flow varies depending on the season, the weather and volcanic activity.
The following outline is provided as an overview of and topical guide to Iceland:
Vatnajökull National Park is one of three national parks in Iceland. It encompasses all of Vatnajökull glacier and extensive surrounding areas. These include the national parks previously existing at Skaftafell in the southwest and Jökulsárgljúfur in the north.
The Diamond Circle is a popular tourist route around Húsavík and Lake Mývatn in North Iceland. The route is fully paved and easily accessible during the summer. The southern section of the route follows Route 1 from Akureyri, before turning north along Route 862, the new road to Dettifoss. Then it joins Route 85 at Ásbyrgi Canyon and follows the coast through Húsavík and eventually re-joining Route 1.
The Skaftá is a river in South Iceland. It is primarily glacial in origin and has had its course modified by volcanic activity; as a result of both, it often floods because of glacial melting.
