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Vallarsa (Cimbrian: Brandtal) is a comune (municipality) in Trentino in the northern Italian region Trentino-Alto Adige/Südtirol, located about 30 kilometres (19 mi) south of Trento. As of 31 December 2004, it had a population of 1,409 and an area of 78.3 square kilometres (30.2 mi2). The municipality of Vallarsa contains many frazioni (subdivision), the townhall is the frazione of Raossi. Vallarsa borders the following municipalities: Rovereto, Trambileno, Ala, Valli del Pasubio and Recoaro Terme.

Trambileno (Trambelém in local dialect) is a comune (municipality) in Trentino in the northern Italian region Trentino-Alto Adige/Südtirol, located about 25 kilometres (16 mi) south of Trento. Trambileno borders the following municipalities: Rovereto, Terragnolo, Vallarsa, Posina and Valli del Pasubio. It is known as the location of the Eremo di San Colombano monastery, a church set on a rock ledge.

Vallagarina (German: Lagertal) is one of the sixteen districts of Trentino in the Italian region of Trentino-Alto Adige/Südtirol. Its administrative seat and major town is Rovereto.

Eremo di San Colombano is a hermitage in Trambileno, Italy, notable for its location in the side of a mountain. Some natural caves, halfway up the rock wall of the gorge formed by the stream of Leno Vallarsa were certainly used from 753 (the date inscribed on the rock) from a Monaco hermit.

In the 1800s, when the Austro-Hungarian Empire controlled the territories of the upper Adige valley in northern Italy, a tobacco plant was built in the town of Borgo Sacco, now part of the city of Rovereto. An earlier name for this tobacco factory was Imperia Regia Manifattura d'Austria-Ungheria (translation: Imperial and Royal Tobacco Manufacturing of the Austro-Hungarian Empire).

Gruppo della Carega is a massif in Veneto, Italy. Its highest peak, Cima Carega, has an elevation of 2,259 metres.

The Rovereto Courthouse (Palazzo di Giustizia) is a building located on Corso Antonio Rosmini in Rovereto, Italy. It houses the local court and is one of the city's most significant examples of late-Austro-Hungarian civic architecture.

The Museum of Modern and Contemporary Art of Trento and Rovereto (MART) (Museo d'Arte Moderna e Contemporanea di Trento e Rovereto, in Italian) is a museum centre in the Italian province of Trento. The main site is in Rovereto, and contains mostly modern and contemporary artworks, including works from renowned Giorgio Morandi, Giorgio de Chirico, Antonio Rotta, Felice Casorati, Carlo Carrà, and Fortunato Depero. Fortunato Depero's house in Rovereto (known as Casa d'Arte Futurista Depero) is also part of the Museum. The permanent collection contains more than 15,000 artworks, including paintings, drawings, engravings, and sculptures.

Rovereto railway station (Italian: Ferrovie Stazione di Rovereto) serves the Comune of Rovereto in the autonomous province of Trentino, northeastern Italy. The station was opened in 1859 by the Austrian Empire's Südbahn and transferred to Italy in 1919. Rovereto station is located on the trans-Alpine Brenner Railway connecting Verona and Innsbruck. The station is currently managed by Rete Ferroviaria Italiana (RFI). The commercial area of the passenger building, however, is managed by Centostazioni, whereas train services are operated by Trenitalia and ÖBB-DB.

Isera (Iséra in local dialect) is a comune (municipality) in Trentino in the northern Italian region Trentino-Alto Adige/Südtirol, located about 20 kilometres (12 mi) southwest of Trento. As of 31 December 2004, it had a population of 2,496 and an area of 14.1 square kilometres (5.4 sq mi).The municipality of Isera contains the frazioni (subdivisions, mainly villages and hamlets) Marano, Cornalé, Reviano, Folaso, Patone, Lenzima and Bordala. Isera borders the following municipalities: Villa Lagarina, Ronzo-Chienis, Rovereto, Nogaredo and Mori.

The Rotzo Formation (also known in older literature as the Noriglio Grey Limestone Formation) is a geological formation in Italy, dating to roughly between 192 and 186 million years ago and covering the Pliensbachian stage of the Jurassic Period in the Mesozoic Era. Has been traditionally classified as a Sinemurian-Pliensbachian Formation, but a large and detailed dataset of isotopic 13C and 87Sr/86Sr data, estimated the Rotzo Formation to span only over the Early Pliensbachian, bracketed between the Jamesoni-Davoei biozones, marked in the Loppio Oolitic Limestone–Rotzo Fm contact by a carbon isotope excursion onset similar to the Sinemu-Pliens boundary event, while the other sequences fit with the a warm phase that lasts until the Davoei biozone. The Rotzo Formation represented the Carbonate Platform, being located over the Trento Platform and surrounded by the Massone Oolite (marginal calcarenitic bodies), the Fanes Piccola Encrinite (condensed deposits and emerged lands), the Lombadian Basin Medolo Group and Belluno Basin Soverzene Formation (open marine), and finally towards the south, deep water deposits of the Adriatic Basin. The also Pliensbachian Aganane Formation of Morocco represents a regional equivalent, both in deposition and faunal content. Fossil prosauropod tracks have been reported from the formation. This formation was deposited within a tropical lagoon environment, similar to modern Bahamas which was protected by oolitic shoals and bars from the open deep sea located to the east (Belluno Basin) and towards the west (Lombardia Basin). It is characterized by a rich paleontological content. It is notable mostly thanks to its great amount of big aberrant bivalves, among which is the genus Lithiotis, described in the second half of the nineteenth century. The unusual shape of Lithiotis and Cochlearites shells, extremely elongated and narrow, characterized by a spoon-like body space placed in a high position, rarely preserved, seems to suggest their adaptation to soft and muddy bottoms with a high sedimentation rate. The Bellori outcrop displays about 20 m of limestones with intercalated clays and marls rich in organic matter and sometimes fossil wood (coal) and amber. The limestones are well stratified, with beds 10 cm to more than one metre thick, whereas the clayey levels range between 3 and 40 cm in thickness.

Dente Italiano (German: Italienische Platte) (2220 m) is one of the ridges of the Pasubio summit highlands in the Vicentine Alps. Located on the line of ridges between the Cosmagnon basin and the Pasubio Alps, to the south the Damaggio pass separates it from Cima Palon, to the north the Denti pass (for the Austro-Hungarians Eselsrücken i.e. donkey's back) separates it from the Austrian Dente.