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The peninsula has a volcanic origin having the Snæfellsnes volcanic belt down its centre, and the Snæfellsjökull volcano, regarded as one of the symbols of Iceland, at its western tip. With its height of 1,446 m (4,744 ft), it is the highest mountain on the peninsula and has a glacier at its peak ( jökull means "glacier" in Icelandic ).
This is an area of renewed intra-plate volcanism in the North American Plate, [17] with rocks no older locally than 800,000 years, [1] that overlay an extinct rift zone that produced the more than 5 million years old crustal basement tholeiitic flood basalts of the Snæfellsnes peninsula.
Stykkishólmur (Icelandic pronunciation: [ˈstɪhcɪsˌhoulmʏr̥] ⓘ) is a town and municipality situated in the western part of Iceland, in the northern part of the Snæfellsnes peninsula. It is a center of services and commerce for the area.
Djúpalónssandur Lifting stones in Djúpalónsandur in Iceland, weighing from top to bottom 23, 54, 100, and 154 kg.. Djúpalónssandur (Icelandic pronunciation: [ˈtjuːpaˌlounsˌsantʏr̥]) is a sandy beach and bay on foot of Snæfellsjökull in Iceland.
Helgrindur (Icelandic pronunciation: [ˈhɛlˌkrɪntʏr̥], also known as Lýsuskarð, Lysuhóll or Lysukard) [2] [3] is a volcanic mountain range or massif in the middle of the Snæfellsnes peninsula that provides a backdrop to the port of Grundarfjörður.
Hellnar (Icelandic pronunciation: [ˈhɛtlnar̥]) is an ancient fishing village, a cluster of old houses and buildings situated close to Arnarstapi on the westernmost part of the Snæfellsnes peninsula, Iceland.
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It contains cinder cones and is the only system on the peninsula that has erupted in recorded history, in 960 CE ± 10. [2] This produced from a single crater a 13 km 2 (5.0 sq mi) lava flow called Rauðhálsahraun [ˈrœyðˌhaulsaˌr̥œyːn] , and a tephra scoria layer that covered about 50 km 2 (19 sq mi). [ 1 ]