Definition: The word "acescent" is a term used in the field of geology that refers to an area where two or more mountains are crossed by a valley or depression. The term was originally coined in the 19th century by Carl Schurz, who described it as a kind of mountain range that connects two high peaks located at different elevations. The term "acescent" is not used very often today, but historically it was a common feature of geologic landscapes where multiple mountains were connected by an area of valley or depression. The elevation difference between the two high points in this area could be as low as 50 feet and as high as 1,200 feet. The definition of "acescent" is not very clear and may depend on context. However, it is generally associated with mountain ranges that connect mountains at different elevations but are less than a mile apart. This term has been used historically in the field of geology to describe areas where multiple mountains are crossed by a valley or depression. In modern usage, "acescent" is often used as a way to refer to an area of high elevation with few significant peaks nearby. This type of environment is not always found in a mountain range but can be found in any region where two or more mountains are separated by a relatively shallow valley.
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