Introduction
Cuesta ridge slopes, also known as hogback ridges, are a unique geological feature found primarily in the southwestern United States and parts of Mexico. These distinctive landforms are characterized by their long, winding ridges that rise abruptly from the surrounding flatlands, creating a dramatic and visually striking landscape. In this article, we will explore the formation, characteristics, and significance of cuesta ridge slopes, highlighting their geological and ecological importance in the regions they inhabit.
