Book contents
- Frontmatter
- Contents
- Colophon
- Preface
- Acknowledgements
- Maps
- Units of measurement and abbreviations
- 1 Geology: An Australian perspective
- 2 The Earth: A geology primer
- 3 Telling geological time: The great canvas
- 4 The cratons: Building the core of Precambrian rocks
- 5 Mountain building: Paleozoic orogenic rock systems
- 6 Warm times: Tropical corals and arid lands
- 7 Icehouse: Carboniferous and Permian glaciation
- 8 Mesozoic warming: The great inland plains and seas
- 9 The birth of modern Australia: Flowering plants, mammals and deserts
- 10 Fossils: The Australian record of past life in context
- 11 The land stirs: Volcanoes and the eastern highlands
- 12 The outline and submerged terrace: Building the continental shelf and coastlines
- 13 The coral reefs: Unique parts of the continental shelf
- 14 Patterns of change: Cycles in Australia's journey
- Epilogue
- Sources and references
- Index
- References
1 - Geology: An Australian perspective
- Frontmatter
- Contents
- Colophon
- Preface
- Acknowledgements
- Maps
- Units of measurement and abbreviations
- 1 Geology: An Australian perspective
- 2 The Earth: A geology primer
- 3 Telling geological time: The great canvas
- 4 The cratons: Building the core of Precambrian rocks
- 5 Mountain building: Paleozoic orogenic rock systems
- 6 Warm times: Tropical corals and arid lands
- 7 Icehouse: Carboniferous and Permian glaciation
- 8 Mesozoic warming: The great inland plains and seas
- 9 The birth of modern Australia: Flowering plants, mammals and deserts
- 10 Fossils: The Australian record of past life in context
- 11 The land stirs: Volcanoes and the eastern highlands
- 12 The outline and submerged terrace: Building the continental shelf and coastlines
- 13 The coral reefs: Unique parts of the continental shelf
- 14 Patterns of change: Cycles in Australia's journey
- Epilogue
- Sources and references
- Index
- References
Summary
Australia is a continent new to science, of long history, stability, aridity and flatness. This chapter provides a brief review of when, how and why geological knowledge of Australia was obtained. It also describes how the new technologies of the satellite and the computer age, and of subsea exploration, have changed our perspective of the continent.
CONNECTIONS
Some call Australia the world's largest island, but it is a true continent, one of the primary building blocks of planet Earth, with rock systems and history that extend back to the earliest recorded episodes of the Earth's development. Traditional stories of the Aboriginal people tell of the creation of this continent and of many of its landscape features. These stories run parallel to this book, because they emphasise the close spiritual relationship between all of us and the land to which we were born, or by which we were adopted, and which supports us.
This book tells how the rocks formed, and how the present landscape and climate developed over millions of years, from an Australian perspective. As the Reverend John Milne Curran wrote in one of the earliest explanations of Australian geology, in 1898, ‘Australia has a history far more ancient than any written by men – to read this history is one of the objects of geology – records preserved in the great stone-book of nature.’
Early progress
Australia was the last habitable landmass to be discovered by Europeans. Early exploration was undertaken happenstance by navigators and traders, mainly Dutch, reaching out to the spice islands of Indonesia. By the late 1600s much of the coast had been charted, but the first complete maps of Australia, resulting from the French exploration of Louis-Claude de Freycinet and the British voyage of discovery by Matthew Flinders, did not appear until 1811 and 1814. The much-later expedition of discovery by James Cook did more than just put Australia on the map. Thorough documentation of its eastern coast in 1770 provided the basis for the First Fleet and British settlement in 1788. At first the new colony was simply an outpost at the end of the Earth, addressing a perceived home-based social problem. But within 30 years an outward, trade-based outlook was in place, delivering Australian wool to Britain.
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- The Geology of Australia , pp. 1 - 22Publisher: Cambridge University PressPrint publication year: 2016