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. 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.
At Brynwood on the River we are notorious for our cozy and relaxing cabins nestled on the charming Big Thompson River. But did you know we also offer delightful motel rooms and spacious vacation homes? Whether you are enjoying a weekend getaway or a family vacation, Brynwood on the River will make it special. Book online today! Brynwood on the River Details
Trail easy to follow, mostly a trench with packed down snow. I tacked this onto Cub Lake Trail and made a loop. Fern TH to the pool is super easy (1.7 miles), no need for traction. Elevation starts after the bridge and doesn’t quit until Fern Lake. Last half mile of the trail has deep snow and it’s easy to post hole. Started this today (1/10) at 8AM, only person parked at TH (cub lake), did not see a single person until hiking back down from Fern.
The Lowdown: Just three miles north of downtown Breck, the Silver Pines Cottage has all the essentials you need and then some for a ski vacation without the hassle of resort lodging. With unbeatable mountain views, this cozy cabin retreat is great for families with a children’s playroom but offers a steam shower and whirlpool for the adults. The entire house is yours for unbelievably only $144 a night.
Rocky Mountain National Park is an American national park located approximately 76 mi (122 km) northwest of Denver International Airport in north-central Colorado, within the Front Range of the Rocky Mountains. The park is situated between the towns of Estes Park to the east and Grand Lake to the west. The eastern and westerns slopes of the Continental Divide run directly through the center of the park with the headwaters of the Colorado River located in the park's northwestern region. The main features of the park include mountains, alpine lakes and a wide variety of wildlife within various climates and environments, from wooded forests to mountain tundra.