A geosyncline (originally called a geosynclinal) is an obsolete geological concept to explain orogens, which was developed in the late 19th and early 20th centuries, before the theory of plate tectonics was envisaged. A geosyncline was described as a giant downward fold in the Earth's crust, with associated upward folds called geanticlines (or geanticlinals), that preceded the climax phase of orogenic deformation. History The geosyncline concept was first conceived by the American geologists James Hall and James Dwight Dana in the mid-19th century, during the classic studies of the Appalachian Mountains. Émile Haug further developed the geosyncline concept, and introduced it to Europe in 1900. Eduard Suess, a leading geologist of his time, disapproved the concept of geosyncline, and in 1909 he argued against its use due to its association with outdated theories. This did not prevent further development of the concept in the first half of the 20th century by Leopold Kober and Hans Stille, both of whom worked on a contracting Earth framework. The continued development of the geosyncline theory by Stille and Kober following the publication of Eduard Suess' Das Antlitz der Erde from 1885 to 1909 was not unchallenged, as another school of thought was led by Alfred Wegener and Émile Argand. This competing view rejected the premise of planetary contraction, and argued that orogeny was the result of continental drift. These two views can be called "fixist", in the case of geosyncline theory, and "mobilist" for the support of continental drift. Even as continental drift became generally accepted, the concept of geosynclines persisted in geological science. In 1970, John F. Dewey and John M. Bird adapted the geosyncline to plate tectonics. The term continued to have usage within a plate tectonics framework in the 1980s, although as early as 1982, Celâl Şengör argued against its use, in light of its association with discredited geological ideas. Geosynclinal theory Dana and Stille supposed that the collapse of geosynclines into orogens was result of the Earth's contraction over time. In Stille and Kober's view, geosynclines and orogens were the unstable parts of the Earth's crust, in stark contrast with the very stable kratogens. Stille theorized that the contractional forces responsible for geosynclines also formed epeirogenic uplifts, resulting in a pattern of undulation in the Earth's crust. According to this view, regular, episodic global revolutions caused geosynclines to collapse, forming orogens. According to Kober and Stille, developing geosynclinal depressions