
What Is a Desert?
How the Atmosphere Influences Aridity
Where Deserts Form
Types of Deserts
Desert Features
Eolian Processes
Types of Dunes
Remote Sensing of Arid Lands
Mineral Resources in Deserts
Desertification
Deserts occupy about one‑third of Earth’s land surface, presenting dry, often dramatic landscapes where rain is scarce and life must adapt to extreme conditions. The opening of the book defines a desert—from shifting sand dunes to rugged stone plains—and shows why these stark worlds have long inspired explorers, storytellers, and scientists alike.
To explain why these regions stay so dry, the author walks listeners through the planet’s tilted axis, seasonal heating, and the global air circulation that creates high‑pressure belts near thirty degrees latitude. The narrative then introduces the Coriolis effect, illustrating how it redirects winds into the prevailing east‑west flows that shape many desert climates.
The early chapters also lay out the main classification schemes—extremely arid, arid and semiarid—based on rainfall thresholds, giving a clear framework for comparing deserts worldwide. With vivid photographs and clear explanations, the book prepares listeners to explore the mineral resources, ecological fragility, and human challenges that make these environments uniquely valuable.
Language
en
Duration
~1 hours (57K characters)
Publisher of text edition
Project Gutenberg
Credits
Produced by Stephen Hutcheson, Dave Morgan and the Online Distributed Proofreading Team at http://www.pgdp.net
Release date
2014-10-14
Rights
Public domain in the USA.
b. 1942
A geologist and science writer, she explored some of the driest places on Earth and helped map worlds far beyond it. Her work connects desert geology, remote sensing, and planetary science in a way that still feels adventurous.
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