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Carlsbad Caverns. A MONG the superb areas included in the national park system of the United States is a series of connected caverns of unusual magnificence and extent called the Carlsbad Caverns. They are located in southeastern New Mexico, in the rugged foothills of the Guadalupe Mountains. The region is picturesque semidesert country, and its unusual cactus vegetation is as strange and interesting to many visitors as are the caverns themselves.
Carlsbad Caverns, like most caves, is a series of openings in a massive limestone which were made by percolating ground water.
The Carlsbad limestone in which these caverns were formed was laid down originally in a sea of muddy water some million years ago. After the great series of chambers forming the main portions of the caverns were formed, nature took up the task of decorating them with a myriad of beautifully sculptured effects in the form of stalagmites, stalactites, more irregular spiral forms known as helectites, enormous columns, curtains seemingly of alabaster, and other limestone ornamentations.
The immensity of the large rooms, the beauty of form, and the impenetrable stillness leave an indelible impression upon all who venture into this fairyland. The most impressive portion of the Carlsbad Caverns is the Big Room, an enormous chamber a mile and a half from the entrance. It is nearly 4, feet long, with a maximum width of feet. At one place the ceiling rises to a height of feet. In this room the limestone formations are superbly beautiful and of an infinite variety of sizes and shapes.
The stalactites vary from almost needlelike proportions to huge chandeliers, and the stalagmites are equally varied, though of different contours. One group of unusually tall and graceful stalagmites resembles the totem poles of the Alaskan Indians and others are like snow-banked forests.