ONE DAY IN 2084 EARTH’S ORIGINAL MOUNTAINS SUDDENLY REAPPEARED ON THE PLANET—AS 85,000 DOMED CANOPIES OF LIGHT FROM THE STARS. The story of this return is told by Blaise, a well-informed but mysterious figure who claims to be an engineer 134 years old and part of an ancient team that first designed the planet. It’s a chronicle of his last field assignment, a unique career retrospective, and a firsthand account of the momentous return of the domes. These are giant half-spheres of Light that originally helped create the biosphere and were the Earth’s first mountains. They generated the Earth’s sacred sites and the mythic homes of the gods and linked them all in a global pattern of Light. The domes arrived all at once and started to reorganize the global landscape. It was their fourth visit, and it would be several perilous years as the planet adjusts to it. Blaise and his team of geomancers travel across the Earth and time to deal with the unprecedented perturbations set in motion by this celestial rescue of the planet. Problems are rife—the revolt of Pan and the Nature Spirits, the continuing dark interference by humanity’s ghostly forebears, the resurgence of Babylon and its imperious agenda, and the planet’s dangerous drift towards becoming flattened like a hockey-puck. But the opportunities are fabulous too as the planet enters an era of unceasing Light and beatific conditions. The return of the domes lays bare the true history of the Earth, how it diminished from perfection, the benign superintendents of this bold experiment, and who its earliest inhabitants were and the massive problems they created which still affect us today. It is a genuinely apocalyptic moment, as the Earth reveals its original bright pattern of energy and consciousness and starts at last to fulfill its destiny.

This volume summarizes the state of the art of Variscan geology from Iberia to the Bohemian Massif. The European Variscan belt consists of two orogens: the older, northern and the younger, southern. The northern Variscan realm was dominated by Late Devonian–Carboniferous rifting, subduction and collisional events as defined by sedimentary records, crustal growth, recycling of continental crust and large-scale deformations. In contrast, the southern European crust was reworked by major Late Carboniferous collision followed by Permian wrenching. The Late Carboniferous–Permian orogeny overprinted the previously accreted system in the north, but with much lower intensity, resulting in magmatic recycling and extensional tectonics. These two main orogenic cycles do not reflect episodic evolution of a single orogenic system but a complete change in orientation of stress field, thermal regime, degree of reworking and recycling of European crust, reflecting a major switch in plate configurations at the Early–Late Carboniferous boundary.

"This memoir brings together results from a multidisciplinary study of the processes that have formed the highest, widest part of the Andean Cordilleran orogenic belt in northern Argentina and Chile. The region features a tectonically erosive forearc, protracted arc magmatism, a high-elevation hinterland plateau and strongly shortened retroarc thrust belt, and a Paleocene-Recent foreland basin system"--

"This volume includes compelling science and field trips in Indiana, Illinois, Kentucky, Michigan, and Ohio. Take a journey through the Heartland to sand dunes, outcrops, quarries, rivers, caves, and springs that connect Paleozoic stratigraphy with the assembly of Gondwana, continental glaciation with Quaternary geomorphology and hydrology, and landscape with the human environment"--

A tectonic synthesis of systematic changes in style and age of deformation; dirction, amount, and rate of tectonic transport, and interaction with magmatism and sedimentation.

"This volume is the product of nearly 25 years of geologic investigations. It is an exposition of two small areas, both less than 25 km from the front of the Mississippian Roberts Mountains thrust, but each displaying a different, unique geologic terrane, previously undocumented in Nevada and perhaps in North America"--

The analysis presented here suggests that nearly all of the Eurasian "intra-cratonic" structures, classically viewed by some geologists to have resulted from primary vertical movements, may be products of horizontal movements caused by repeated orogenies around the periphery of cratons. Understanding the evolution of the Cimtnerides together with their fore- and hinterlands sheds much light on the Mesozoic tectonics of all of Asia and eastern Europe and leads to a number of interesting concepts concerning continental evolution, such as "hidden subduction." Finally, a study on the evolution of ideas on the Cimmerides clearly shows how much we remain under the spell of the Kober-Stillean fixist philosophy.

Students of a phenomenon as common but complex as andesite genesis often are overwhelmed by, or overlook, the volume and diversity of relevant information. Thus there is need for periodic overview even in the absence of a dramatic breakthrough which "solves the andesite problem" and even though new ideas and data keep the issues in a state of flux. Thus I have summarized the subject through mid·1980 from my perspective to help clarify the long-standing problem and to identify profitable areas for future research. Overviews are more easily justified than achieved and there are fundamental differences of opinion concerning how to go about them. It is professionally dangerous and therefore uncom mon for single authors, especially those under 35 such as I, to summarize a broad, active field of science in book-length thor oughness. Review articles in journals, multi-authored books, or symposia proceedings appear instead. The single-authored approach is intimidating in scale and can result in loss of thoroughness or authority on individual topics. The alternatives lack scope or integration or both.