Petrified Forest National Park stretches across the colorful high desert of northeastern Arizona, where grasslands, mesas, badlands, and ancient fossil deposits form an unusual landscape. The park is best known for its extensive petrified wood, much of it preserved from trees that lived in a river environment more than 200 million years ago.

The Peak District National Park occupies a large area in central England, mainly across Derbyshire with smaller sections extending into Cheshire, Staffordshire, and Yorkshire. It is divided broadly into the gritstone moorlands of the Dark Peak, the limestone dales of the White Peak, and the rolling farmland of the South West Peak. Unlike a wilderness park, it is a lived-in landscape containing villages, farms, roads, reservoirs, and historic buildings.

Spello sits high on the slopes of Mount Subasio in the heart of Umbria, where visitors step into a place shaped by centuries of history. Each year, Spello’s streets become a living canvas during the Infiorate di Spello, a long-standing celebration tied to Corpus Christi. Residents work through the night before the feast to lay flower petals along the town’s main thoroughfares, creating patterns and images that stretch for over a mile.

Glastonbury, a town in Somerset, England, is steeped in mysticism and historical allure. Known for its rich Arthurian legends and spiritual significance, Glastonbury is a must-visit for those fascinated by mythology and history. The town’s centerpiece is the majestic Glastonbury Abbey, a grand ruin once one of the most powerful monasteries in England. Founded in the 7th century, the Abbey is famously linked to the legend of King Arthur and his supposed final resting place.

Bryce Canyon, tucked into the high plateaus of southern Utah, offers one of the most unusual landscapes in the American Southwest. It’s not actually a canyon but a series of natural amphitheaters carved into the edge of the Paunsaugunt Plateau. What makes Bryce unique is its dense collection of hoodoos which are tall, thin spires of rock formed over millions of years by frost-wedging and erosion.