Not just a great valley, but a shrine to human foresight, the strength of granite, the power of glaciers, the persistence of life, and the tranquility of the High Sierra. First protected in 1864, Yosemite National Park is best known for its waterfalls, but within its nearly 1,200 square miles, you can find deep valleys, grand meadows, ancient giant sequoias, a vast wilderness area, and much more.

16 Photos

This dramatic landscape testifies to nature's size, beauty, and diversity--huge mountains, rugged foothills, deep canyons, vast caverns, and the world's largest trees. These two parks lie side by side in the southern Sierra Nevada east of the San Joaquin Valley. Weather varies a lot by season and elevation, which ranges from 1,370' to 14,494'.

16 Photos

Palm Springs is a desert resort city in Riverside County, California, United States, within the Coachella Valley. It is located approximately 55 mi (89 km) east of San Bernardino, 107 mi (172 km) east of Los Angeles, 123 mi (198 km) northeast of San Diego, and 268 mi (431 km) west of Phoenix, Arizona. The population was 44,552 as of the 2010 census. Palm Springs covers approximately 94 square miles (240 km2), making it the largest city in the county by land area. Biking, golf, hiking, horseback riding, swimming, and tennis in the nearby desert and mountain areas are major forms of recreation in Palm Springs. The city is also famous for its mid-century modern architecture and design elements.

16 Photos

Antelope Canyon is a slot canyon in the American Southwest. It is on Navajo land east of Page, Arizona. Antelope Canyon includes two separate, scenic slot canyon sections, referred to individually as "Upper Antelope Canyon" or "The Crack"; and "Antelope Canyon" or "The Corkscrew". The Navajo name for Upper Antelope Canyon is Tsé bighánílíní, which means 'the place where water runs through rocks'. Lower Antelope Canyon is Hazdistazí (called "Hasdestwazi" by the Navajo Parks and Recreation Department), or 'spiral rock arches'. Both are in the LeChee Chapter of the Navajo Nation. Antelope Canyon was formed by erosion of Navajo Sandstone, primarily due to flash flooding and secondarily due to other sub-aerial processes. Rainwater, especially during monsoon season, runs into the extensive basin above the slot canyon sections, picking up speed and sand as it rushes into the narrow passageways. Over time the passageways eroded away, making the corridors deeper and smoothing hard edges in such a way as to form characteristic "flowing" shapes in the rock.

28 Photos