The geomorphological, geological, and archaeological objects of the Sian Lowlandhave been studied, and their significance as potentially popular geotourist attractions has been substantiated. The Sian Lowlandis located in the northwestern part of the Ukrainian Carpathian Foreland and is a constituent geomorphological element of the Sian-Dniester interfluve. The lowland’s relief is smooth, characterized by the alternation of ridge-like elevations of the Vyshnia‒Vizhomlia, Vizhomlia‒Shklo, Shklo‒Zavadivkainterstreams and shallow trough-shaped river valleys with gently inclined non-terraced slopes and often waterlogged bottoms. The topography of the Vyshniaand Shklo valleys is varied with dunes concentrated in two strips – one stretches along the right side of the Vyshnia river valley through the villages of Malniv, Martyny, Sokolia, ArlamivskaVolia, Khorosnytsia and Zarichchia, and the other one is developed in the Shklo river valley between Krakivets and Yavoriv. The northeastern part of the Sian Lowland has undergone a significant anthropogenic transformation – the Shklo River channel has been regulated, and a complex of anthropogenic landforms and deposits has been formed within the boundaries of the Yavoriv mining district: karst processes and phenomena have been activated. Less large-scale anthropogenic changes have occurred in the lowland’s southern part, which is proposed to be covered by a geotourist route that will run through Rodatychi ‒ SudovaVyshnia ‒ Zarichchia‒Khorosnytsia ‒ ArlamivskaVolia ‒ Sulkivshchyna. The main geotourist attractions here are the following geological, geomorphological and archaeological objects: the preserved valley of glacial meltwater runoff between Rodatychi and SudovaVyshnaya, which is now drained by the Rakivriver, as well as the dunes spread in the valley and the archeological monument KniazhyiMist; eolian, fluvial landforms and deposits, outcrops of fluvioglacial accumulations and archaeological sites developed in the vicinity of the villages of Zarichchiaand Pisky:a complex of eolian and fluvial landforms and deposits, as well as archaeological sites, developed nearKhorosnytsia village; eolian landforms and deposits, an archaeological site near the village of ArlamivskaVolia; glacial accumulations, which were discovered in a quarry located east of the village of Sulkivshchyna (north of Mostyska). These settlements are connected to each other and to Lviv by the M-11 highway (Lviv‒Mostyska‒Shehyni) and/or the Lviv‒Shehynirailway line, which provides convenient access to the proposed geotourist attractions. The developed geotourist route also makes it possible to unite the so far separate Carpathian, Carpathian Foreland and Roztoczegeotourist routes into a single network. Key words: geotourist attractions; Sian Lowland; eolian deposits; dune; terrace; fluvial landform; archaeological site.