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Laugardælir is a small hamlet near the town of Selfoss. Laugardælir was one of Iceland's busiest ferry sites until a bridge was built across Ölfusá in Selfoss in 1891. The church at Laugardælir was built in 1965 using mainly concrete and it is 300 m2 in total. In the church cemetery is the burial site of former World Chess Champion Bobby Fischer (1943-2008).

Selfoss Church was built from 1952 to 1956 and consecrated on Palm Sunday, 25 March 1956. It was designed by the headmaster of the Technical College in Selfoss, Bjarni Pálsson (1912-1987). The building was expanded between 1978 and 1984; a tower, porch and congregation hall with a kitchen and facilities, which now serve the purpose of a convention center, was added to the structure.

A beautiful sports and outdoor recreational area on the banks of Hvítá River. The area is owned by the Youth Association Baldur.

Kerið, is a 55 m deep volcanic crater, about 3000 years old. It is a part of a group of volcanic hills called Tjarnarhólar, and is now filled with water, creating a lake whose steep circular slopes resemble an ancient amphitheatre.

Apavatn is a lake in southwest Iceland. With a surface area of around 13 km².

Apavatn is renowned for its good fishing, especially trout. This lake is historically important as can be read in one of the country's Sagas (Sturlunga). It is said that one of Iceland's ancient poets, Sighvatur Þórðarson, who lived in the 11th century, received his gift of poetry from eating a strange fish he caught in Apavatn.

Situated in the lower part of the Biskupstungur valley between the rivers Hvítá and Brúará, Skálholt is one of Iceland's places of special historical interest. For seven centuries it was the scene of the most dramatic events which shaped the political, spiritual and cultural life in Iceland. Its early history is traced back to the 11th century when religious disputes were at their sharpest in Iceland. Within two centuries of the settlement of Iceland, the first bishopric was founded at Skálholt in 1056 for South Iceland, and soon a second at Hólar in 1109 for North Iceland.

The man who chose Skálholt as the site of the first Episcopal see in Iceland was Ísleifur (1006 - 1080), son of Gissur the White. Skálholt had earlier been his patrimonial estate and his grandfather, Teitur Ketilbjarnarson, was the first settler there. According to an old account, Skálholt was at that time "the largest town in Iceland". Ísleifur's father, who was a wealthy aristocrat and a redoubtable political figure as well, played a decisive role in the Christianization of Iceland and the future status of the church. He built the first church in Iceland at Skálholt around the year 1000.

In the 12th century bishop Klængur Þorsteinsson built a great cathedral at Skálholt. It was a sumptuous edifice made of timber shipped from Norway. For centuries Skálholt was the centre of learning and culture in Iceland, a status which lasted up to the Reformation in 1550.

In 1954, a team of archaeologists, while digging up the foundations of the old cathedral, came upon a sarcophagus which was believed to contain the skeleton of Páll Jónsson, one of the most powerful bishops of Skálholt. His sarcophagus, together with a few relics found at the scene, is now on display in an underground vault beneath the new memorial church built during 1956-1963 on the site of the old cathedral. All churches in Scandinavia contributed financially to its construction.

The last Catholic bishop of Iceland, Jón Arason, was executed at Skálholt in 1550, along with his two sons. He had opposed the Reformation imposed upon Iceland by King Christian III of Denmark. Today, a memorial stands at the site of the execution. Arason's Episcopal robes are on display at the National Museum of Iceland in Reykjavík.

Today, Skálholt is visited for the new cathedral, the tomb of bishops, the museum, and the collection of ancient books in the tower.

A suspension bridge over Ölfusá River was first built in 1891 and became the largest bridge in Iceland at the time. In September 1944, when the bridge had been in use for 53 years, the eastern bearing cables broke due to the weight of two trucks. A new suspension bridge was built in 1945 which only took five and a half months but while it was being constructed the old bridge had been fixed for temporary use. The bridge is 84 meters long and is in the town Selfoss.

Hellisskógur is a small forest just outside of the town Selfoss. In Hellisskógur are roads and walking paths around the area and benches so visitors can relax and enjoy the area.

The cave in Hellisskógur forest was formed at a latter glacial period by sea erosion. Sea levels have been higher than now several times and signs of sea erosion can be seen on more cliffs in the area which are made of around 0, 7 - 3, 1 million year old basalt. The cave was previously used to store hay in the back and as a sheepcote in the front. It was once believed that the cave was haunted by a ghost wearing a blue scarf. The story tells of a young man who was broken hearted and hung himself in the cave using a long blue scarf.

Here is a map of Hellisskógur

Ingólfsfjall mountain in Ölfus is 551m. Ingólfsfjall is fenced with cliffs in three ways and very steep. When the sea level was highest at the end of the ice age, it was a steep head that the waves broke down and created the steep slopes. It is connected to Grafningsfjöll with Grafningsháls. Ingólfsfjall is mainly made of palagonite with lava layers in between. Ingólfsfjall was formed in the middle of the ice age.

To the south of the western corner of the mountain protrudes a gray cliff called Silfurberg, which is made of palagonite with light hole fillings that are mainly rayon deposits. To the south is Kögunarhóll and the main road lies between. Ingólfsfjall is named after the settler Ingólf Arnarson. Up on the mountain is a gray stone hill called Inghóll and it is said that Ingólfur is buried there. Below Ingólfsfjall on the south side is Fjallstún.

The Settlement Book states that Ingólfur Arnarson spent his third winter in Iceland on his way to Reykjavík. Later, a large farm called Fjall was built there and was deserted in the 18th century. Remains of ancient structures can still be seen on the site and are now protected.

On May 29, 2008, the source of the Suðurlandsskjálfi earthquake was 6.3 on the Richter scale below Ingólfsfjall.