Þingvellir (Thingvellir) is a historic site and national park in Iceland, east of Reykjavík. It's known for the Alþing (Althing), the site of Iceland's parliament from the 10th to 18th centuries. On the site are the Þingvellir Church and the ruins of old stone shelters. The park sits in a rift valley caused by the separation of 2 tectonic plates, with rocky cliffs and fissures like the huge Almannagjá fault.

Gullfoss is two separate waterfalls; the upper one has a drop of 11 meters and the lower one 21 meters. The rock of the river bed was formed during an interglacial period. Water flows over Gullfoss at an average rate of 109 cubic meters per second. The heaviest floods have recorded a flow of 2000 cubic meters per second. During the summer, the flow is 130 cubic meters per second, which would take only 3 seconds to fill this building. People were eager to exploit the power potential of Gullfoss, and many plans for hydroelectric developments on the river Hvítá have been proposed. (Driving time is included in the time, usual stop at Gullfoss is 30-60 minutes)

Geysir, sometimes known as The Great Geysir, is a geyser in southwestern Iceland. It was the first geyser described in a printed source and the first known to modern Europeans. The English word geyser derives from Geysir. The name Geysir itself is derived from the Icelandic verb geysa.

Langjökull is the second largest ice cap in Iceland, after Vatnajökull. It is situated in the west of the Icelandic interior or Highlands of Iceland and can be seen clearly from Haukadalur. Its volume is 195 km³ and the ice is up to 580 m thick. The highest point of the ice cap is about 1,450 m above sea level.

Drop off at your hotel. (Driving time is included in time)