Quantifying denudation rates under different climatic and tectonic settings is fundamental to
understanding landscape evolution. Carbonate rocks may respond differently to climatic and …

Originally published in 1989, Karst Geomorphology and Hydrology became the leading
textbook on karst studies. This new textbook has been substantially revised and updated …

Abstract Earth's Critical Zone (CZ), the near‐surface layer where rock is weathered and
landscapes co‐evolve with life, is profoundly influenced by the type of underlying bedrock …

Carbonate minerals, unlike silicates, have the potential to dissolve almost completely and
with high efficiency. Thus, in carbonate terrains denudation rate and style (the governing …

The weathering of carbonate rocks plays a critical role in the evolution of landscapes, the
erosion of buildings and monuments, and the global-scale shifting of carbon from the …

Ephemeral karst lakes (turloughs) are wetlands at the interface between groundwater and
surface water, and are a characteristic feature of the Irish karst landscape. They are transient …

Carbonate rocks are highly reactive and can have higher ratios of chemical weathering to
total denudation relative to most other rock types. Their chemical reactivity affects the first …

Using cosmogenic isotopes and solute load analysis, we quantify chemical weathering
(solutional erosion) and denudation rates over variable time scales in a tectonically stable …

Carbonate landscapes make up one-fifth of the terrestrial land area, a better understanding
of the coupling relationship between the soil–epikarst form and hydrological function is …

Abstract The Inception Horizon Hypothesis (IHH) postulates that certain stratigraphic
horizons in a limestone sequence, combined with structural surfaces such as joints, provide …