Red Island (Crveni otok), one of the most renowned tourist locations in Rovinj. Actually, it consists of two artificially connected islands: St. Andrew’s Island (Otok Sv. Andrije) and Maškin Island (Otok Maškin).
Red Island is a fifteen-minute sail away from the town center. Taxi boats arrive from and depart for Red Island every hour, from a small pier on the main town square, and from Delfin pier. The sail to the island is very pleasant, passing by Katarina Island, Lona and Zlatni rt bays that will surely enchant you with their beauty.
Dense Mediterranean underbrush and old coniferous forest are predominant on the island, and there are cultivated flower parks with paths near the hotels and annexes. In 2002, Red Island was hit by a heavy storm, almost entirely destroying the 100-year-old pine forest, which has been providing shade and shelter from summer heats for numerous tourists. The biggest damage was caused on Maškin Island. A lot has been done towards cleaning and renovating the island since last year so that you could enjoy its beauty and intimacy again.
You can find a really large number of beaches on the island. They are mainly stony beaches with typical coves covered with pebbles. The most frequented beaches are the ones situated on the south side of St. Andrews Island, near the hotel and the annexe. Numerous services are offered nearby, namely: a restaurant, a pool, miniature golf courses, a diver centre and others. A small part of the shore near the little port has been covered with gravel, making it suitable for children and seniors. https://www.inforovinj.com/eng/rovinj/plaze/crveni-otok.asp
Near the road Rovinj-pula, about 2 kilometres far from the centre of the City of Rovinj, in the locality of Monfiorenzo, is situated the quarry phantasy, a geological park of remarkable beauty and importance. According to the expert opinion of numerous scientists, it is one of the most significant natural monuments in the world in the perspective of the karst phenomenon. The lime-stone of the quarry phantasy, like the open book pages, illustrate the history of the evolution of the terrestrial crust.
Various layers give evidence of the existence of the fossilized meadows consisting of sea-weeds, which, blended with lime-stone silt, were drifted on the shore by strong currents during the last 130 million years.
The quarry phantasy will reveal to a more careful visitor a considerably big number of furrows made of black and white dolomiti layers. Furthermore, there are fissures formed by tightening and exsiccation of the silt that had been squeezed into the previously created sediment.
The lower part of these stony layers was formed below the sea level, while the upper part is the result of the high-tide. https://www.inforovinj.com/eng/rovinj/znamenje/monfiorenzo.asp