Estes Park is one of the most beautiful mountain retreats in all of Colorado — and we’re not just saying that because they’re our neighbors! OutThere Colorado named the village on their list of the 10 Most Beautiful Places to Spend a Weekend in Colorado. It was chosen for its proximity to Rocky Mountain National Park and the stunning views from Estes Park Aerial Tramway.
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]

Southern ColoradoKnown as a heritage town with grand nineteenth-century architecture and brick streets that date to the early 1900s, Trinidad is set in a green valley halfway between Denver and Santa Fe. The town is surrounded by vast state and national recreation areas, including two state parks. Trinidad is the gateway to the Scenic Highway of Legends, where travelers find lakes and stunning dikes that radiate out from the ancient Spanish Peaks. Historic and prehistoric sites abound in every direction.
Imagine taking a trip on a train with your partner, very Old World romantic, isn’t it? The Cumbres & Toltec Scenic Railroad offers several options for guests who are looking for romantic getaways. The railroad runs between Chama, New Mexico and Antonito, Colorado. There are several trips available for you to choose including a full-day trip, a half-day trip, a sunset trip, and galloping goose #5. The sunset trip is probably the most romantic option of all. Depending on the route you choose, the fare starts from 95.75 USD.

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]
Grand Lake is arguably the biggest attraction in the town of Grand Lake, offering boating, sailing, fishing, swimming, kayaking and yachting – it even hosts a Regatta Week in early August. This is also where you’ll find the biggest Fourth of July fireworks display in all of Colorado, as well as a wealth of popular tourist spots like candy shops, old time photo galleries and saloons, an array of gift shops and even mini-golf courses. Plus, as it sits near the western entrance of Rocky Mountain National Park, you’ll be steps away from one of the country’s most spectacular wildlife-filled parks too.
There are more activities, events, vacation opportunities, and fun things to do in Colorado than you can imagine.  Vacations in Colorado can mean hot air balloon rides, jeep, ATV, motorcycle or bicycle rental or tours, snowmobile, sleigh rides, dog sledding, fly fishing for rainbow, brown and brook trout, sailing, jet-skiing, water skiing, boating, kayaking or canoeing (rentals, equipment, instruction, guided tours and floats), or get wet and wild whitewater rafting, tubing, skiing, snow shoeing, and cross country skiing (check out our ski areas, rentals and tours), horseback riding, hiking, bicycling, rock climbing, upland bird hunting, big game hunting for deer, elk, moose, antelope, bear, mountain lion, mountain goat, big horn and dall sheep. Come experience the beauty of our mountains and our western hospitality on your Colorado vacations.

The complex interactions of elevation, slope, exposure and regional-scale air masses determine the climate within the park,[48][49] which is noted for its extreme weather patterns.[49] A "collision of air masses" from several directions produces some of the key weather events in the region. When cold arctic air from the north meets warm moist air from the Gulf of Mexico at the Front Range, "intense, very wet snowfalls with total snow depth measured in the feet" accumulate in the park.[48]

The Mile High City offers something for everyone. Home to seven professional sports teams and a thriving arts and cultural scene, it’s easy to make lasting memories on any given weekend. Stay downtown, in the Lower Highlands (LoHi) neighborhood or River North Art District (RiNo) district to be walking distance to shows, the best restaurants, breweries and night life. Explore even more to do in Denver here .

In the shadow of Great Sand Dunes National Park and Pre­serve, the quirky town of Hooper sits atop a natural artesian hot spring, with water flowing year-round into the family-friendly Sand Dunes Pool. On the same property, The Greenhouse is an all-indoor, all-adult oasis with three small soaking tubs and a 10-by-75-foot zero-entry pool. The Greenhouse also has a 10-person sauna, indoor gardens and an onsite bar to help you stay even toastier. 


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]

The sun made us lazy, and after following Brian as he made his way upstream I found a wider expanse of sand and gravel, promptly plopping down on a pair of flip flops I had brought in my backpack as a make-shift seat. After identifying the northern harrier hawk over my head, and the savannas sparrows and red-winged blackbirds perched precariously on reeds across the water, I took out my knitting project. I didn’t have to worry about losing Brian; in the valley I could see for miles in both directions.
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