Pulitzer Prize-winning author John McPhee continues his Annals of the Former World series about the geology of North America along the fortieth parallel with Rising from the Plains. This third volume presents another exciting geological excursion with an engaging account of life—past and present—in the high plains of Wyoming. Sometimes it is said of geologists that they reflect in their professional styles the sort of country in which they grew up. Nowhere could that be more true than in the life of a geologist born in the center of Wyoming and raised on an isolated ranch. This is the story of that ranch, soon after the turn of the twentieth century, and of David Love, the geologist who grew up there, at home with the composition of the high country in the way that someone growing up in a coastal harbor would be at home with the vagaries of the sea.

This memoir summarizes the current knowledge of New Caledonia’s geology, geodynamic evolution, and mineral resources, based on published and unpublished information. It comprises 10 research papers, each addressing a particular geological assemblage or topic. After an introductory chapter, and a review of the published geodynamic models of evolution of the SW Pacific, chapters 3 to 5 focus on the main geological assemblages of Grande Terre: the Pre-Late Cretaceous basement terranes, the Late Cretaceous to Eocene cover, and the Eocene subduction-obduction complex, one of the largest and best-preserved in the world. Chapter 6 is devoted to the Loyalty Islands and Ridge. Chapter 7 deals with the mostly terrestrial post-obduction units including regolith. Chapter 8 deals with palaeobiogeography and discuss plausible scenarios of biotic evolution. Chapters 9 and 10 provide an comprehensive review of New Caledonia’s mineral resources. The volume will interest stratigraphers, sedimentologists, marine geologists, palaeontologists, palaeogeographers, igneous and metamorphic petrologists, geochemists, geochronologists, and specialists in tectonics, geodynamic evolution, regolith, ophiolites, and economic geology.