Geological Classification of Aquifers

Geological Classification of Aquifers

Classification of Aquifers: Geologically, they can be classified based on the age and composition of the sediments or rocks that host them. The four main types are: Holocene Aquifers Late Pleistocene-Holocene Aquifers (Unconsolidated to semi-consolidated):...
Geological Applications of Radiometric Dating

Geological Applications of Radiometric Dating

Radiometric Dating: Introduction and Principles In the early part of the 20th century, scientists discovered radioactivity and the radiogenic decay of isotopes, which opened the way for dating rocks by an absolute rather than a relative method. Up to that time,...
Common Mineral Grains in Sandstones

Common Mineral Grains in Sandstones

Mineral Grains in Sandstones: A very large number of different minerals may occur in sandstones, and only the most common are described here. Quartz: Quartz is the commonest mineral species found as grains in sandstone and siltstone. As a primary mineral, it is a...
The Units of Bouma Sequence

The Units of Bouma Sequence

The Bouma sequence specifically describes the ideal vertical succession of structures deposited by low-density (i.e., low sand concentration, fine-grained) turbidity currents. The Bouma sequence is divided into five distinct units, labelled A through E, with A at the...