The Geological Evolution of Australia and New Zealand focuses on the stratigraphy of Australia and New Zealand. This compendium covers the stratigraphy, paleogeography, and paleontology of various systems, including the Precambrian, Cambrian, Ordovician, Silurian, Devonian, and Carboniferous systems. Tectonism and igneous activity of these systems are also examined in this collection. Other systems considered are the Permian, Triassic, Jurassic, Cretaceous, Tertiary, and Quaternary systems. This book will be invaluable to archeologists, historians, researchers, and academicians interested in the stratigraphy of Australia and New Zealand, as well as those who wish to study the rock formation of their respective location.

Providing fundamental discussion of regolith properties andchemistry, this book considers many landscape situations andfeatures, whilst linking process to position, geochemistry andtime. Presenting information from an Australian perspective itprovides new insights into the subject, which are developed awayfrom the yoke of traditional Northern Hemisphere ideas andconcepts. * Presents a new approach to the problems of understanding regolithgeology and landscapes * Presents the general aspects and principles of regolith * Chapters present views on landscapes and their evolution, thenature of minerals, the behaviour of water at a landscape level andthe exploration of water behaviour at various scales in regolithmaterials * Investigates methods of conveying information about regolith viamaps and in GIS packages

What sight is more beautiful than a high-energy beach facing lines of rolling white breakers? What battleground is more ferocious than where waves and sand meet? What environment could be more exciting to study than this sandy interface between sea and land? And yet how much do we know about sandy beaches? Open sandy beaches are amongst the most neglected fields of scientific study in the coastal environment. This situation exists despite their great extent along most temperate and tropical coastlines and their value as recreational areas and buffer zones against the sea. The traditional oceanographer does not venture into the surf zone while the terrestrial ecologist stops short at the high water mark. Only a few coastal engineers have grappled with the problem of sand and sediment movement as it influences their construction of harbours and pipelines. The marine biologist on the other hand has regarded estuaries, coral reefs and rocky shores, obviously teeming with life, as more fruitful areas for study than the apparently poor animal life on sandy beaches. Sandy beaches have therefore tended to become a scientific no man's land. Over the last decade this situation has begun to improve. Recent work on high-energy beaches has revealed that they may in fact be rich and productive and fertile areas for study. It has even been suggested that beaches and their adjacent surf zones may constitute viable marine ecosystems.

Rock features are important traces of the formation and development of karst surface. On various karren their record is especially rich, revealing to us the many factors that in diverse conditions formed the karst surface on various carbonate and other rock.We have tried to present the most characteristic rock features and through them the most important factors and processes in the formation of the karst surface, the methods of studying them, and the most outstanding examples.Forty-nine contributing authors offer a wide spectrum of content and examples of rock forms from many karst regions around the world.The first part of the book offers an orderly-organized survey and description of the most characteristic rock forms and presents the physical and chemical corrosion of rock, biocorrosion, the modeling of rock forms, their detailed morphometrics, and numerous descriptions of individual rock forms. The second part is devoted to various examples of rock forms found around the world from Slovenia through North and South America to Australia and Asia.