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A lighthouse was first built at Streitishvarf in 1922 and it operated until 1958, when it was removed due to the building of a new lighthouse in Breiðdalsvík. The Streitisviti lighthouse operating today was built in 1984.  Streitishvarf is a great outdoor area, suitable for the whole family. A beautiful, short hiking trail offers a brilliant insight to the geological history of Austurland, especially the dikes that are characteristic for the area. Although the hiking trail is short, it is a great place to stop for a few hours; to play and enjoy the nature. 

In Breiðdalsá, close to the farm Brekkuborg in Breiðdalur valley, is the Beljandi waterfall. In fact, there are two waterfalls; Ytri Beljandi and Innri Beljandi, and eponymous pools. The waterfalls are not very high, but they are beutiful and well worth the short hike from the road through Breiðdalsvík. The whole area is extremely beautiful and suitable for outdoor activities.

Flögufoss is the highest waterfall in Breiðdalur valley, around 60 meters high. The waterfall is in the river Flöguá that runs through the Flöguskarð mountain pass. Just above Flögufoss is another small waterfall that falls to a ledge, from where the river runs under a small rock arch.  The hiking path leading to the waterfall is easy and short.

Streitishvarf is a great outdoor area, suitable for the whole family. A beautiful, short hiking trail offers a brilliant insight to the geological history of Austurland, especially the dikes that are characteristic for the area. Although the hiking trail is short, it is a great place to stop for a few hours; to play and enjoy the nature. A lighthouse was first built at Streitishvarf in 1922 and it operated until 1958, when it was removed due to the building of a new lighthouse in Breiðdalsvík. the Streitisviti lighthouse operating today was built in 1984.

In the summer 2000, a project was started in Iceland to celebrate the turn of the century and the 70th anniversary of Iceland Forestry Society. Five Millennium Forests (Aldamótaskógur) were planted in Iceland; one tree for each living Icelander.  The plants, representing the inhabitants of Austurland, where planted by Tinnudalsá river (Tinna), at Eydalir. A few decades before, some trees had been planted in that same area turning it into a great outdoor recreational area. A beautiful marked hiking trail runs through the forest, along Tinna. 

Breiðdalur central volcano is an ancient volanic area above Breiðdalur valley and Berufjörður. It was the object of extensive research carried out by the English geologist George D.L. Walker who made East-Iceland teritary volocanologic phenomenons the main object of his professional work. The Breiðdalur area of volcanism is set with rhyolithic-inserts producing the mainstay of majestic mountain range searating Breiðdalur and Berufjörður, e.g. Mt. Flögutindur, Mt. Smátindar, Mt. Röndólfur, Mt. Slöttur and Mt. Stöng. The southern side of the volanic formation is highly colorful and the instrusions assume an irregular aspect, set with tephra-layers. The site of the central volcano extends between Mt. Fossárfjall, south of Berufjörður to Mt. Bæjartindur, which towers above farm Þorgrímsstaðir in Breiðdalur. The western slope runs along Mt. Ófærunafir towards the west, whereas the eastern side - although highly eroded - extends east of Mt. Kerlingartindur, S-Breiðdalur. The southern region of Breiðdalur - the very centre of area - forms a basin where the excruciating heat has transformed the rock to such an extent that the basalt and the andestite have turned pale-green, making it problematic to tell them apart from the rhyolite. This can be clearly detected at river Innri-Ljósá Blágil ravine. The beforementioned chain of mountains was formed at a later date as the rhyolite wielded its way to the surface through the basalt layers, forming insertions on top of the massive tephra layers along the edges of the crater. Their remnants are visible in rhyolithic-rocks throughout the Breiðdalur region. This central volcano is considered to be of later date than its Álfta- and Reyðarfjörður counterparts. The Reyðarfjörður ignimbrite, a pyroclastic flow made as a burning hot mixture of about 430 km2 with a diameter of about 6 m. thickness. This layer is linked the Mt. Skessa south of Reyðarfjörður, best known as the Skessulag. The immense volcanism of the area has resulted in a great variety of rare minerals and semi-precious stones on display at Petra´s wonderful stone collection in Stöðvarfjörður and the Breiðdalur miniral museum in Breiðdalsvík.

There has been a vicarage at Heydalir since early Christianity in Iceland and several renowned vicars have served there through the ages. Among them was the vicar and hymn poet Einar Sigurðsson (17th century) whose poetry is still venerated among the nation. A pillar stone has been erected in his memory at Heydalir. The church that now stands in Heydalir was hallowed July 13th in 1975 and the old church was unchurched that same day. The old church was built in 1856 but it burned to the ground on June 17th, 1982. The name of the place is somewhat erratic; some people talk say Haydalir and Heydalir is mentioned in some of Iceland’s old Sagas. Others talk about Eydalir, especially older locals, and the vicar Einar Sigurðsson is associated with Eydalir. In the church´s record book, which has been in use since 1909, both names are used equally. Today the official name of this place is Heydalir. 

Höskuldsstaðir is a farmstead of distinction, located in the south branch of valley Breiðdalur, close to highway no. one. A post office up to 1947 and a relay for the postmen on their way across Berufjöður pass. Höskuldsstaðir was the birthplace of the venerated scholar Dr. Stefán Einarsson, former professor at the John Hopkins University of Baltimore. Einarsson is remembered for his literary achievements as well as for his research in the sphere of the Icelandic language.

Meleyri is a charming shoreline near Breiðdalsvík. This is an outdoor area, a colorful birdlife arena and popular among locals and tourists alike. The locals use this area a lot, especially during winter because snow des not stick to the sand.