After most visitors to Iceland arrive at Keflavik international airport, they quickly grab their bags and set their sights on traveling to downtown Reykjavík. Unfortunately, the don't give any thought to visiting the rest of the Reykjanes Peninsula.







 Little do they know that a beautiful, less crowded and completely underrated place waits just outside of the airport. I was delighted when I found out that this peninsula had been designated a UNESCO Global Geopark in 2015.



I have been fortunate to travel to this area on several occasions. When there, I am always pleasantly surprised by how amazing and diverse the landscape is. While I don’t want this peninsula to become overcrowded with visitors, I do think it is a shame that more people do not explore this place. It is literally brimming  with geothermal activity, mud pools and lava fields. It is also home to so many hiking trails and fascinating Icelandic history.



Most notably, it is one of the best places to see the separation of the Eurasian and North American tectonic plates.   After learning more about this place, I decided it was worth it to dedicate this episode to the Reykjanes Peninsula.



The Unique Geology of the Reykjanes Peninsula



During one of my visits to the area I found the geology to be quite interesting. After looking up how the area was formed, I found the following quote from Visit Reykjanes brochure. Just a heads up, there is some science lingo in the quote but I still think it is worth sharing,



“Reykjanes Peninsula is an important region from a geological standpoint. It is a geologically young section of Iceland and is a land born and highly volcanic counterpart of the North Atlantic Ridge where the tectonic plates diverge at an average rate of 2.5 cm/ yr. The peninsula contains late Quaternary volcanic palagonite tuff and pillow lava formations as fells and mountains from the last glacial periods. Widespread basaltic lava flows and volcanic structures from interglacial periods, especially from the last 11,500 years (the Holocene Era) characterise the area. Four elongated volcanic systems and fissure swarms line the peninsula from SW to NE. They contain open fissures, normal faults, high temperature geothermal fields and numerous volcanic fissures that are lined with monogenetic craters.”



Whether you care about the science behind how this area was formed or not, the beauty and the uniqueness of the landscape can’t be denied.



Where is the Reykjanes Peninsula & How to Get There



Before jumping into what to see and do in this part of south Iceland, I think it is important to go over where it is and how to get there. As I mentioned in the beginning, this peninsula is in the south of the country, specifically the south-west.



The towns and villages that make up the Reykjanes Peninsula include Suðurnesjabær, Grindavík, Vogar, and Reykjanesbær. If it is relatively clear when you are flying into Iceland, you can get a glimpse of the stark black sand beaches along the coastline and the jagged lava rock that dominates this part of the country.



By car, it is very easy to drive around the peninsula. Whether you rent a car on your own or take a tour. However, the real fun begins when you get out of the car and explore on foot.



Different Towns on Reykjanes Peninsula



Each of the towns of the peninsula that I mentioned above have unique features that attract visitors. For instance, Reykjanesbær, which is the municipality that is home to Keflavik international airport is made up of three districts: Keflavík, Hafnir and Njarvík. With a population of a little over 15,000 people, it is the largest town on the peninsula. There you will find different types of accommodations, stores, bars and museums.



Suðurnesjabær



Suðurnesjabær



Suðurnesjabær is a fairly new municipality in Iceland. In 2018, it was created by merging Garður and Sandgerði and it has a population of about 3,000 people.