The Blue Lagoon

Inlet created because of a subsidence.

Important for birdlife and marine biology.

Location: Near small village Hafnir - short walk from road 44

Earthquake fissures in a shield that built up in several eruptions.

In a narrow fissure system. Can find there small caves.

It is most common to walk to Skálafell from parking at Gunnuhver.

Kalfatjörn is a former farm, parsonage and church site in the Vatnsleysa County. It was a parsonage until 1907, when the parish was united with the Gardar parish of the Kjalarnes deanery. During catholic times, the church was dedecated to St Peter. The present church was built in 1892-93 and consecrated June 11th 1893. It was built of wood and covered with corrugated iron on stone foundations. It seats 150 persons. It now belongs to the Tjorn Parish. The altarpiece, a replica of the one in the Reykjavik Cathedral, painted by Sigurdur Guðmundsson, is equally old as the church.

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Brimketill is a small pool carved naturally by marine erosion. It lies at the lava shore edge west of the town of Grindavík and is one of the most popular natural attractions of Reykjanes. According to folklore it was regularly occupied by a giantess named Oddný, hence its old name Oddnýjarlaug

Gianta in the mountain moved to Reykjanesbær during the family and cultural festival the Night of Lights in 2008 and is now located in Black Cave at the marina in Gróf. There Gianta has been settling in her nice cave with its superb view over the bay of Keflavík and Faxaflói.

Gianta is originally the creation of author Herdís Egilsdóttir who has written 16 stories about the little girl Sigga and her friend Gianta in the mountain. The last one describes her migration to Reykjanesbær. Gianta is in full size and sits sleeping in a rocking chair in the kitchen.

Open every day from 10:00 -17:00. Free Admission

An ancient fishing outfit and a trading post just south of Stafnes.

It was one of the harbours of the Danish Trade Monopoly posts comprising Hafnir, Stafnes and Midnes. During the night of January 9th 1799 a catastrophic tidal flood devastated Batsendar. It swept most of the houses away and some of the people barely escaped. Only one old woman drowned. This was the most devastating, tidal flood in the history of the country.

How to get there: Road from Sandgerði to Stafnesi. There is a parking and walk from there until you see ruins of the place and old wall made from rocks.

Háleyjarbunga is a small, flat lava shield with a large, 20 to 25 meter deep crater.

The shield is at least 9,000 years old. It was formed during a highly effusive lava eruption. The basalt-type is a primitive deep-mantle derived picrite that contains much of the green mineral olivine.

Location: The Háleyjarbunga is close to Reykjanes lighthouse on the tip of Reykjanes. A hikingpath is marked form Gunnuhver over the lavafield to Háleyjarbunga.

Háleyjarbunga is a geosite within Reykjanes Unesco Global Geopark.

Seaweed-coverd rocks which are part of the Þráinsskjöldur Lava Flow.

They were formed about 10,000 years ago.

Due to the pourous roks that form the foundation of this part of Iceland fresh water seeps from the ground in many places.

Located near town Vogar.

A eroded subglacial volcano.

A section of a small hyaloclastite hill is exposed in the costal cliffs. A dyke named Festi(ladder), evidently the feeder for Festarfjall, passes up through the basement and the Festarfjall sequence, branching towards the base of the lavas. The story say that Festi is a neckless of a woman-troll.

The story also say that it is impossible to walk on the beach downbelow without getting wet! Try and see if you can!

Location: Near highway 427

Ásbrú - Keflavík

Name of the facility: Andrews theater

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Place of execution according to an old folk story.

Cliffs, two of which are quite high, with an inlet several fathoms deep between them. A tree between was laied between the two cliffs and men hanged from it a punishment for serious crimes.

Location: About 1 km from Básendar, short walk from road 45

Company: Hljómahöll

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Here are two very attractive and interesting exhibitions:

The Saltfish Museum:The exhibition Saltfisksetrið brings to light our seafaring history. The exhibition is very intriguing for foreign tourists, and it is interesting for local students, who can study the most important
profession of the country, and enjoyable for every Icelander passing through on a weekend trip.

The people of Grindavík have long been among the most prolific in the production of dried salted cod. The exhibition about Iceland's history in the processing and sales of dried salted cod and it's significance to Iceland's economy is therefore well placed in Grindavík.

The Saltfisksetrið exhibition opened in the year 2002. The exhibition offers large pictures, a text detailing the history of dried salted cod processing along with some historical objects from characteristic harbor towns of old.

The self-guided walking tour has a marked beginning and end, and is therefore outlined in chronological order. The floor is made of gravel, and there are stage sets of buildings from different periods on show throughout the exhibit.

Great care was taken to recreate the history of dried salted cod processing, and the exhibit has attracted much attention.

The Township of Grindavík was a leading force in the construction of this site, in collaboration with its founders and other donors from GrEarth Energy:
In Iceland there are unique possibilities to see and investigate most of earth's dynamic processes, such as volcanism and geothermal heat, which is the result of the young age of the island. It might be said that Iceland is a window into the past as well as into the future. By reading the history of the different
geological strata it is possible to forecast geological events that are likely to happen again.

The larges glaciers and the mightiest glacial rivers in Europe are here in Iceland and here are to be found the largest high- and low-temperature geothermal areas, unusually high volcanic and tectonic activity and magnificent and rough nature.

EARTH ENERGY has 18 boxes showing:

1 Ísland - a land in the shaping
2 The battle between sea and fire
3 The birth of Iceland
4 The earth can be compared to an egg
5 The boundaries of the plates on earth's crust
6 A Seismic model
7 The active volcanic belt
8 Earthquakes in Iceland
9 Volcanic eruptions are frequent on the
Reykjanes peninsula
10 Fissure eruptions are common in Iceland
11 The age of the earth
12 A glacier covers Scandinavia
13 Iceland was a subtropical paradise
14 Research and science
15 Energy from the bowles of the earth
16 Drilling for hot water
17 The power plant at Svartsengi
18 The Blue Lagoon

EARTH ENERGY - In cooperation with HS Orka
indavík.

A free standing, hyaloclastite mountain north of Grindavik.

It offers great panoramic view over most of the Reykjanes Peninsula on fine days. The northeastern part of the mountain depicts thermal activity an to its north and northeast is an extensive high temperature area. It is split by a fissure called "The Thieves´ Gap" (Thjofagja), occupied by 15 thieves according to the legend. They were eventually overwhelmed and killed by trickery.

Vogastapi was named "The Heifer Cove Cliff", later "The Cove Cliff" and sometimes just "The Cliff" by the inhabitants of the area. It is an 80 m. high, dolerite hillock between Coves Vogavik and Njardvik. It is precipitous towards the sea, but has a gradual gradient inland. It is mostly sparsely vegetated and somewhat barren in places. The main road to the western communities crosses it. The view from its highest point, Grimsholl, is excellent and a view dial explains the topographical names of the surroundings. Up to this date the Vogastapi Area is haunted by a ghost, which has mislead people off the brink of the cliff. During the motorized age, some of the passers by have noticed a being carrying its head under its arm and sometimes drivers travelling alone spotted it in their rear view mirrors sitting in the back seats.

Company: Hljómahöll

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Protected coastline because of birdlife, marine biology and rifts.

Location is west of Grindavik by road 425.

A lava flow formed in an eruption in the year 1151 AD.

In that year a 25 km long fissure opened obliquely acorss the Reykjanes peninsula. The lava field is located in south of ridge Nupshlidarhals(Vesturhals) and craters in the northern part are part of crater row in the north of Ridge Nupshlidarhals. Ogmundur is a male name in Iceland.

Junkaragerdi was a farm just north of the Hafnarberg Cliffs. Its name was probably derived from 12-18 foreigner, who lived there, and were called "Junkers". They were said to be heavy drinkers, strong men, and womanizers. The neighbours wanted to get rid of them, and one night they damaged the rowlocks of their boats. The Junkers went fishing in the early morning and during the day they encountered bad weather and the rowlocks broke. The Junkers then supported the oars with their knees and got back home. The next time their oars were sawn half through and the saw marks were hidden. The Junkers went fishing and never came back.

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Company: Hljomaholl

Name of the facility: Felagsbio

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Lava pile between Grindavík and Krýsuvík.

A good place to ,,read" the history of the peninsula.

Location: Short walk from road 427

Annually, The Blue Lagoon and the town of Grindavík sponsor a Midsummer night hike on the mountain Þorbjörn. On the top of the mountain there is entertainment which includes singing and camp fire. The walk ends at the Blue Lagoon which is open past midnight that evening. This is an entertaining recreation for the whole family. For information about the forthcoming Midsummer day hike visit the official website of Grindavík www.grindavik.is or www.bluelagoon.com.

Company: Ráin

Name of the facility: Brúin

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During the 19th century ships started frequenting this harbour again. The merchants of Keflavik often unloaded salt, timber and heavy merchandize there and loaded fish from the farmers of Midnes and Hafnir. In the beginning of the 20th century the arrivals of ships diminished, because of the opening of the Sandgerdi harbour and a new trading post there.

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Ruins of farm partly covered by lava flow.

The Húshólmi area is a so called "clearing" over which the lava Ögmundarhraun didn´t flow during an eruption in the year 1151. The lava came flowing from vulcanic craters on the east side of Núpshlíðarháls hill down to the shore. According to archaeologists, in the western part of the "clearing" are ruins of the ancient Krýsuvík farm, dated back since before the year 900. Among the ruins are presumably parts of a home, a church and a semetary.

Húshólmi is a popular outdoor area and a interesting site worth visiting.

Each summer in August a Family Day is held in Vogar in Vatnsleysuströnd. At this time the family is in the forefront and everyone is welcome. The program is mostly arranged by the locals and made to fit all ages of family members. Among other things for amusement are soap-soccer, fishing in the harbour, home-made car race and many other interesting and amusing things.
Also look for other events and more information about the festival on www.vogar.is

A well known locality for xenolithes.

Xenolithesa are gabbroic crystal aggregates related to the host magma. The source of the lava is not known nor is its age.

Location: Near Grindavik, walk from road 427

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Company: Hotel Keflavík

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The mud pools and steam vents on the south-west part of Reykjanes.

The area is close to Reykjanes lighthouse and is collectively named Gunnuhver after a female ghost that was laid there. She had caused great disturbance until a priest set a trap for her and she fell into the spring. This happened about 400 years ago.

The mud pools take form where steam from boiling geothermal reservoir water emanates and condenses and mixes with surface water. Accompanying gases such as carbon dioxide and hydrogen sulphide make the water acid. This causes alteration of the fresh lava rock to clay.

Steaming of the ground at Reykjanes increased markedly as a consequence of a pressure drawdown in the geothermal reservoir upon the start of production from the reservoir in 2006.

Iceland´s largest mud pool at present prominent, highest up in the Gunnuhver group. It is 20 meters wide across a rim of mud, boiling vigorously.

Two ramps are located at the Gunnuhver group, on close to Gunnuhver itself where you can look down to the spring and hear the vigorous noise, see the boiling water and feel the power bursting from the ground and the steam on your face. The other ramp is located on Kísilhól a silica hill. From there you have a good view over Gunnuhver group and surroundings.

Gunnuhver stands in the heart of the Reykjanes UNESCO Global Geopark where the North Atlantic ridge rises from the ocean, you find 100 different craters and lava fields, bird cliffs, high geothermal areas, black sand beaches, The Bridge Between Continents, geothermal power plants, lighthouses, and exhibitions.

Kalmanstjorn is an abandoned farm, a former mansion to the south of Lake Kalmanstjorn, where there are still some ruins reminding of the habitation, where the mansion of Kirkjuhofn stood. According to a legend the house had 50 doors. The farm Kalmanstjorn is said to have been an outlying farm from the mansion Kirkjuhofn. It was a church site and some people claim to be able to see some traces of the cemetery there. A short distance further south is Sandhofn and still further Sandhofn, which was abandoned in 1828. Those farms were all abandoned because of earthquakes and sandstorms.

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A rock with three holes, shape like bowls.

Most wanted stop for travellers that had to go to either to Grindavik or Krýsuvík. It is located were these two old roads meet.

The story says that one is for a dog, one for a man and the third for a horse. The water is holy and people could always trust that there would be water to drink.

Location: Short walk from road 427.

The normal fault and tension fracture, Hrafnagjá, is the longest of its kind at the Reykjanes peninsula. It is 12 km long and up to 30 m high. The set of fractures east of Vogar village forms a typical rift valley.

Location: Hrafnagjá is visible from Reykjanesbraut (road nr. 41) to Keflavík International Airport. A hikingtrail leads to the location from the parking place by the intersection of the town Vogar.

Hrafnagjá is a geosite in the Reykjanes Unesco Global Geopark.

The spit on which you are standing is named Hópsnes on the west side and Þórkötlustaðanes on the east side. The spit is 2 km long and 1 km wide and was formed 2,800 years ago when lava flowed into the sea.

Hópsnes/Þórkötlustaðanes was formed during an eruption from a row of craters named Sundhnúkur located just north of the village of Grindavík. Port conditions in Grindavík are excellent due to this lava flow and the lagoon (Hópið) that formed beside the spit when the sea began to erode the lava and move loose materials. If the spit were not there, the village of Grindavík would probably never have been built. The fact is that it is one of six communities on the Reykjanes peninsula that owes its existence to an eruptive fissure in a volcanic system that is still active. Eruptions could occur in this area at any time.

From its earliest days, Grindavík has been one of the main fishing centres in Iceland. Sundhnúkur, from where the lava that formed the spit flowed, has navigation signals showing the route through the gap into the harbour. Travelling around the spit, one can see a number of shipwrecks that have run aground here and in the neighbourhood in the course of the 20^th century. There are information signs by some of the wrecks.

Both the village and fishing-vessel operations flourished in the early 20^th century. Numerous rowing boats and later motor boats were operated from Þórkötlustaðanes. There are a good number of remains of the settlement that is no more, such as entrance cairns, fish-storage huts, ice storages, fish-processing houses, liver-processing and salt huts. The fishing operation moved to the location that is now Grindavík harbour in 1939, when a group of energetic Grindavík residents took it upon themselves to dig a channel through the reef that had hitherto prevented boats from entering the Hópið lagoon. The Hópsnes lighthouse was built in 1928.

Today the area is a popular recreational area with a hiking and biking trail.

Ásbrú - Keflavík

Name of the facility: Andrews Banquet

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Company: Hljómahöll

Name of the facility: Merkines

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The southwest corner of the Reykjanes peninsula.

There the Mid-Atlantic Ridge comes ashore. At this location it is literally possible to see the Mid-Atlantic Ridge rise out of the sea.

Reykjanes is a part of Suðurnes which is the largest urban in Iceland. Almost all travelers go around the area entering or leaving from Iceland.

The nature is magnificent. Various volcanic formations are found on Reykjanes Peninsula, such as mountains and hills chiefly made of volcanic tuff, large and small lava flows plus different types of volcanoes and volcanic edifices.

Marine birds are common on the Reykjanes Peninsula. A number of high sea cliffs attract many individuals of different species during the breeding season. In addition, gulls and Arctic terns are common sight.

Agriculture and fishing were the main activites on the peninsula for more than a millennium. Today, cultivation revolves around gardening, reforestation and reclamation of soils and vegetation. Land for outdoor activities and tourist service is considered to be a valuable resource.

THE REYKJANES VOLCANIC SYSTEM

The Reykjanes peninsula volcanic zone is a direct continuance of the North Atlantic Ridge that surfaces from the ocean at Reykjanes. The peninsula has four volcanic systems that become active in eruptive series, approximately every 1,000 years. Each series lasts for around 200 to 350 years.

The western-most system is the Reykjanes system. This system extends from the west side of Reykjanes to Grindavík in the south and thence to the north-east over the peninsula along Vogar to Kúagerði. Approximately 35 km of the system is on land (40-45 km if the undersea part is included), and is 5-15 km in width, broadest in the south. The system is believed to extend 5-10 km under water to the south-west.

The most recent eruptions in the system were the Reykjaneseldar (Reykjanes Fires), which were in 1210 to 1240. The preceding eruptive series occurred 1,500 to 1,800 years ago.

There are between 40 and 50 volcanic outlets in the system from several drift and eruptive series, as well as 14 shield volcanos or shield volcano tops. Signposted hiking trails lie to Háleyjabunga and Skálafell shield volcanos. Picrite, a rare, primitive basalt variant akin to that which forms in Earth's mantle can be seen near Háleyjabunga mountain.

The surface within the system is rather fissured. The system contains numerous faults, including the large rift valley near Valahnúkur and another that lies alongside the Reykjanesbraut highway near Vogastapar.

The most active part of the system is here, in the south-west, where volcanic rock quickly piles up and where the geothermal area is liveliest.

"Darkness in the middle of the day"

The Sturlunga Saga and several other compilations mention the winter of 1226-1227 as being the "Sand Winter" and a significant "Winter of Famine". There was an undersea eruption off the coast of Reykjanes, and the ash-fall was so great that in some places, it was pitch dark in the middle of the day. Numerous farm animals in Iceland were killed, and it was said that Snorri Sturluson lost 100 cattle that he owned in Svignaskarð in Borgarfjörður. Karlinn (the Man), a 51 m sea pillar just off the coast of Reykjanes, was formed in this eruption.

Stadur is a former parsonage and a church site a short distance to the west of the town Grindavik. It was a parsonage until in the beginning of the 20th century. The catholic churches there were dedicated to the Holy Mother, St John the Apostle, St Stephan, St King Olaf, St Bishop Blasius, St Bishop Thorlakur, and St Holy Virgin Cathrine. The Stadur Church was moved to the District of Jarngerdarstadir in 1909 and named the Church of Grindavik. The semetary of Grindavík is there. A statue of the beloved reverand Oddur V. Gíslason is in the semetary who served the parish in 19th century.

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Kirkjuvogur (Church Cove) was a mansion in Hafnir, an annexed church site of the Grindavik parish, which was long served by the reverends of Utskalar. Still earlier, Kirkjuvogur was served from Hvalsnes. The catholic churches were dedicated to the Holy Mother. During the flood storm of 1799 the church was severely damaged.

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A popular recreational area.

Pounds, rich of vegetation and important resting place for migration birds.

Next to the pounds is Háibjalli, a 10 m high fault.

Location: Road 43 near Seltjörn and Sólbrekkuskógur.

Keflavík

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One of the five major high temperature areas of the Reykjanes Peninsula.

It supplies all of the communities of the Reykjanes Area with hot water for house heating and other purpose. The famous Blue Lagoon comes from the discharge from the power station. Area of green patches north of the hill Svartsengisfell north of the town Grindavík. On summertime the people of Grindavík celebrate there.

Cliffs known as Gallows Cliffs or Hanging Rocks.

The cliffs were used to execute thieves captured in Þorbjarnarfell according to an old folk story.

Location: From road 43 there is a short walk.

A crater row formed in eruption 2.350 years ago.

It created natural harbour condtions in the town Grindavík. Sundahnúkur was used as a landmark for the Grindavík harbour in former times.

Mt Fagradalsfjall, the westernmost part of the mountain ridge of the Reykjanes Peninsula, is really a small plateau. Some hyalocaslite ridges protrude, especially in the western part. Its highest elevation is 385 m. above sea level.

Frank M. Andrews, the commander in chief of the American forces in the North-Atlantic area during World War II, with several other high ranking officers, was killed there in a crash. They were arriving from USA and preparing for landing on Keflavík Airport. Only one man survived the crash. He had to wait more than 24 hours for rescue. There can still been found items from the plane.

Location: In the center of Reykjanes Peninsula, north-east of Grindavík.

Frank Maxwell Andrews

The Zoological Viking Home is in operation next door to the Vikingworld. These are some calves, lambs and goats as well as chickens and rabbits in a fun environment. All the animals have in common to be of the same kind as the domestic animals brought over the Atlantic Ocean with the first permanent settlers in Iceland over 1100 years ago.

Arnarsetur is a short monogenetic volcanic fissure with scoria and spatter craters, formed in an eruption that was an integral part of the Reykjanes Fires, a volcano-tectonic episode from 1210 to 1240. The fissure is two kilometers in length and the lava formations that originate from it cover 20 square kilometers. They are rugged and contain lava tubes and remains of human activity. The name Arnarsetur means Eagle's nest and derives from a pair of eagles that lived in the area before.

Arnarsetur is located east of the road to town Grindavík (43). The exit is about half way from Reykjanesbraut (41) to Grindavík.

This is a deep southern inlet of the big Faxi Bay between spit Keilisnes in the east and the Stakkur Peak of the Holmur Cliff in the west. The Stakkur Peak is crowned with a lighthouse. The bay was named after a freestanding rock in the sea off Cliff Holmsberg.

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Patterson Airport was built in 1942 by the usa navy.

The airport was mainly used to maintain the aircrafts. Next to the airport can be found Subfossils shells, since 20.000-22.000 years ago. They lived shorly before the Late Glacial Maximum at about 18.000 years age. The sea level at that time was about 5-10 m. The airport was closed 1945.

Location: Road 44 at fence on Patterson. Walk north from old ammunition supplier

A family and port festival is held annually in Grindavík in the beginning
of june. Held on the seamens´day week end, it is an entertaining
festivity which honors earlier times which influenced the local
community since it's establishment seamanship and seagoing has
been the main source of occupation and income for the inhabitants
of Grindavík. For more information visit Grindavík's official homepage
www.grindavik.is.

Shelters made of rock, ancient paths and stacked walls.

They have been discoverd near Eldvörp, a row of scoria and spatter cones formed in the Reykjanes Fires 1210-1240 AD.

Location: Close to Eldvörp, walk from road 425.

Company: Keilir

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A pond with good walking paths, picnic facilities and a barbecue.

Next to Seltjörn is Sólbrekkuskógur, a small forest, but sheltered and lovely as it is situated hugging small slopes, with interesting rock formations in a few places.