It contains calcium, niobium, tantalum, cerium, titanium, yttrium, and typically uranium and thorium, with some other metals. The chemical formula is: (Y,Ca,Ce,U,Th)(Nb,Ta,Ti)2O6. It is commonly partially amorphous due to radiation damage.
It was first described in 1870 and named for from the Greek (ε?ξεινο?), hospitable or friendly to strangers, in allusion to the many rare elements that it contains.
It occurs in granite pegmatites and detrital black sands.
It is found in many locations worldwide, notably its type locality in J?lster, Sunnfjord, Norway. Other locations include include the Ural Mountains of Russia; Sweden; Minas Gerais, Brazil; Ampangabe, Madagascar; Ontario, Canada; and in Arizona, Wyoming and Colorado in the U. S. A.
Euxenite is used as an ore of the rare earth elements it contains. Rare large crystals have also been used in jewelry.