An alpine village peppered with an array of modern resorts, Beaver Creek is the perfect weekend getaway destination. A laid-back ambiance of unhurried travelers, here visitors can get away from it all with the area’s world-class skiing and resort amenities. With gorgeous Rocky Mountain views, Beaver Creek is located in the Vail Valley and offers plenty of activities to fill a weekend itinerary. Many people come to try their hand at the 1,815 acres of skiable slopes, catering to both novice and experts alike. The area has plenty of other things to do, however, as visitors can take in a show at the Vilar Performing Arts Center, or indulge in anything from golf courses to pampering spas, shops and restaurants, with the city even home to a large outdoor ice rink in its city center.
Home to the Lake Superior, Lake Michigan, Lake Huron, and part of Lake Erie, Michigan is rich in natural vegetation and beauty. Families looking for an adventure should explore the Upper Peninsula region that houses famous natural attractions such as the Porcupine Mountains, Pictured Rocks, Mackinac Island, Isle Royale, Tahquamenon Falls, and the Seney National Wildlife Refuge. Then there is the heavenly Lower Peninsula region with its placid lakes, rivers, forests, sand dunes and beaches. Canoeing, fishing, sailing, and motorboating are popular activities. You'll love returning to your Michigan cabin rental to unwind after an action-packed day exploring.
If you love the great outdoors but also want luxurious comfort on your vacation, let the Cabins at Rams Horn Village Resort be basecamp for your Rocky Mountain Getaway. Our western-styled Cabins are the definition of Rocky Mountain comfort w/ all the modern conveniences. Each cabin is its own private retreat from everyday cares, allowing families & friends to come & play together, & build lifelong memories. Rams Horn Village Resort Details
Located 75 minutes west of the Resort along with a five-mile stretch of Colorado’s famed Tarryall River, The Broadmoor Fly Fishing Camp is a private escape that pairs world-class fishing with exceptional accommodations and dining. This outstanding retreat borders 120,000 acres of the Lost Creek Wilderness, offering honeymooners who love to fish together the opportunity to experience more than five miles of private waters under the guidance of professional Broadmoor guides. The picturesque camp features a beautifully restored Main Lodge with a wraparound deck and seven rustic yet well-appointed guest cabins dating back to the 1920s. During the evenings, guests gather in the Main Lodge for artfully prepared meals and relaxation. In addition to the exceptional fly fishing, camp guests can enjoy a variety of fun activities such as horseback riding, hiking, and the opportunity to see some of Colorado’s most spectacular wildlife.
There's more to Michigan than its natural legacies. Ann Arbor's University of Michigan is a must-visit for its Law Quadrangle, the Power Center for the Performing Arts, Natural History Museum, and a series of Gothic structures. One of the longest suspension bridges in the world is the Mackinac Bridge, which joins the Lower Peninsula at Mackinaw City to the Upper Peninsula at St. Ignace. Frankenmuth in mid-Michigan is an interesting replica of a German town, where visitors make a customary stop at Zehnder's or The Bavarian Inn, known for their luscious fried chicken.
The park may be accessed through Estes Park or via the western entrance at Grand Lake. Trail Ridge Road, also known as U.S. Route 34, connects the eastern and western sides of the park.[91] The park has a total of five visitor centers. The Alpine Visitor Center is located in the tundra environment along Trail Ridge Road, while Beaver Meadows and Fall River are both near Estes Park, with Kawuneeche in the Grand Lake area, and the Moraine Park Discovery Center near the Beaver Meadows entrance and visitor center.[9]
Precambrian metamorphic rock formed the core of the North American continent during the Precambrian eon 4.5–1 billion years ago. During the Paleozoic era, western North America was submerged beneath a shallow sea, with a seabed composed of limestone and dolomite deposits many kilometers thick.[54] Pikes Peak granite formed during the late Precambrian eon, continuing well into the Paleozoic era, when mass quantities of molten rock flowed, amalgamated, and formed the continents about 1 billion–300 million years ago. Concurrently, in the period from 500–300 million years ago, the region began to sink while lime and mud sediments were deposited in the vacated space. Eroded granite produced sand particles that formed strata—layers of sediment—in the sinking basin.[55]
