Author Description
304p illustrated hardcover, from a Cambridge college library with label on spine, pages unmarked, binding firm, very good
Menrva's Summary
THE THESIS
How do chemical and physical processes interact to break down rock at the Earth's surface? Cliff Ollier, a prominent geomorphologist, provides a comprehensive examination of weathering processes. The text synthesizes geological data and field observations to explain the mechanisms of rock decay, the formation of regolith, and the resulting landforms. It serves as a technical framework for understanding the fundamental role of weathering in landscape evolution.
THE SCOPE MAP
What You Will Find
- Detailed analysis of chemical weathering processes including hydrolysis and oxidation
- Examination of physical weathering mechanisms such as frost wedging and thermal expansion
- Discussion on the relationship between climate, rock type, and weathering rates
- Case studies of specific landforms and soil profiles
Scope Limits
- Does not focus on modern anthropogenic climate change impacts on weathering
- Excludes detailed discussion of planetary geology beyond Earth
THE AUTHORITY PERSPECTIVE
Experts recognize this work as a foundational text in geomorphology due to its technical rigor and clear categorization of weathering phenomena. Readers frequently note the academic density of the prose, which makes it a standard reference for students and professionals in the earth sciences.
Page Count:
304
Publication Date:
1969-01-01
ISBN-10:
0050017950
ISBN-13:
9780050017951
Physical Geography
Geology
Geomorphology
Earth Science