Located at the transitional zone between the Qinghai-Tibet Plateau and the Loess Plateau, Linxia UNESCO Global Geopark is rich in diverse geoheritage. The most prominent geological highlights are abundant palaeontological fossils and their strata in the geopark. The palaeontological fossils can be divided into two major categories. One is the Liujiaxia footprint fossils distribute in the Yellow River basin of the northeast geopark. Represented by dinosaurs (theropod, sauropod, ornithopod), pterosaurs and birds tracks, Liujiaxia footprint fossils were unearthed in Hekou Formation of Lower Cretaceous. At least nine kinds of palaeovertebrates’ footprints have been discovered in the geopark. It is the first time footprints of Mesozoic vertebrates were discovered in Gansu province, China. A large number of parallel ornithopod tracks evidence that dinosaurs lived in groups. There are tracks of a running sauropod, which is rare in world’s records. Tracks of symbiotic ornithopod and sauropod are rare in Asia even globally. The site was excavated manually and scientifically and was protected since the excavation. So the whole assemblages have been well preserved without weathering. The fossil footprints are precious materials for studying the physiology and living habits of dinosaurs. They provide important basis for studying the living environment and biological categories of dinosaurs and clues for further studying the categories of dinosaurs and the relationship between footprints and organisms.The other is Hezheng Cenozoic mammalian fossils in the South of the Geopark. At present, there are nearly 100 fossil sites of Cenozoic mammals found in the geopark and fossil specimens are more than 30,000 pieces. These mammalian fossils reflect that since the Cenozoic, effected by the uplift of the Qinghai-TibetPlateau, the mammalian fauna had been replaced at least 4 times. Rhinoceros constituted the majority of the Indricotherium Fauna in the late Oligocene and predators were quite primitive. Great changes took place in the composition and structure of the middle Miocene Platybelodon fauna. And the fossil’s difference between the north and south sides of the Qinghai-Tibet Plateau reflects that the elevation of Qinghai-Tibet Plateau had hindered animal’s communication in the middle Miocene. The late Miocene Hipparion fauna indicates that the earliest Hipparion migrated from North America to Asia by acrossing the Bering Land Bridge. The composition of the early Pleistocene Equus fauna is typical. Small mammalian is few and fossils of carnivore are rich. These mammalian fossils in Linxia Geopark provide key evidence for studying the classification, ontogenesis, heteromorphosis, phylogeny, geological age, paleogeography, paleo-climate and paleoecology. The late Cenozoic stratigraphic sequence is the most complete late Cenozoic terrestrial sections in Eurasia, which evidence the uplift history of the Qinghai-Tibet Plateau and is of great significance for the study of contemporaneous stratigraphic correlation worldwide. Yellow River, the second longest river in China, crosses Linxia Geological Park and forms Three Gorges composed of Bingling Gorge, Liujia Gorge and Yanguo Gorge.and Yanguo Gorge. The Danxia landform dominated by Cretaceous sandy conglomerates distributes along the both sides of Yellow River, with different shapes and complete geomorphologic types after long-term erosion and cutting. World Cultural Heritage -- the Bingling Temple Grottoes with a history of more than 1600 years, built on the cliff of Danxia landform on the bank of the Yellow River, are a good example of combination between cultural heritage and geoheritage. Linxia Geopark is one of the important birthplaces of Chinese Civilization, with many ancient cultural relics. Because of being an important station of southern thoroughfares of ancient Silk Road, Linxia is known as the Western Land Trading Centre, and the home of Chinese painted pottery. Represented by Dongxiang and Baoan minorities, minorities have formed a distinctive local culture in the Geopark. The geopark is also the cradle of folk song Hua’er, a kind of World Intangible Cultural Heritage. In 2004, Yongjing in the geopark was identified as the “Place for folk song investigation and collection” by UNESCO. Ba Fang Shi San Hang( Bafang thirteen lanes) within the geopark is famous cultural landscape combing local culture, architectural art with villeggiatura.Integrating science, rareness and uniqueness, Linxia Geopark is of high scientific, aesthetic and tourism development value. Moreover, the geopark boasts profound culture, strong ethnic feature and captivating natural scenery. Therefore, Linxia Geopark will be an ideal place to conduct scientific investigation and education, enjoy recreation and entertainment and experience diverse ethnic cultures.