Sandra & I just wanted you to know how much we enjoy our stays at "Brynwood on the River". It seems like the last stay was even better than the previous ones! We had a wonderful 5 days in EP and Sandra, in spite of her medical issues, did very well. This card has six "THANKS" on the front. Five of them are for five wonderful days and nights and the 6th one is for the friendship that has grown over the many times that we have stayed at your place! Thank you so much for saving my box of goodies for 10 months - that was beyond the call.
Estes Park is always a wonderful escape for anyone looking to get out of Denver for a day or two. There is a lot to do and see here, with plenty of wonderful restaurants, entertainment and shopping. Plus, off-season the rates are very affordable, and you’ll find the town less crowded and easier to explore. Stay at the Fall River Cabins, just two miles east of Rocky Mountain National Park. You’ll find the cozy, country-style wood cabins to be very romantic, with spa hot tubs and fireplaces in each unit. Everything has that rustic, woodsy feel, which adds to the mountain escape that you will enjoy all weekend long.
Plan a weekend of pampering and relaxation at St Julien Hotel in downtown Boulder. The hotel features a 10,000-square-foot spa with 12 treatment rooms, and a two-lane infinity pool with a whirlpool and outside terrace. Guests can get in shape at the fitness center with the latest cardiovascular and aerobic equipment. Choose from 201 rooms and suites with luxury bathrooms with soaking tubs and separate glass showers. Ask for a view of the Flatiron Mountains when you book your stay. All rooms offer complimentary Internet access, wired and wireless.
Rocky Mountain National Park is one of the highest national parks in the nation, with elevations from 7,860 to 14,259 feet (2,396 to 4,346 m),[30] the highest point of which is Longs Peak.[31] Trail Ridge Road is the highest paved through-road in the country, with a peak elevation of 12,183 feet (3,713 m).[32] Sixty mountain peaks over 12,000 feet (3,658 m) high provide scenic vistas.[30] On the north side of the park, the Mummy Range contains a number of thirteener peaks, including Hagues Peak, Mummy Mountain, Fairchild Mountain, Ypsilon Mountain, and Mount Chiquita.[33] Several small glaciers and permanent snowfields are found in the high mountain cirques.[34]
The park's climate is also affected by the Continental Divide, which runs northwest to southeast through the center of the park atop the high peaks. The Continental Divide creates two distinct climate patterns - one typical of the east side near Estes Park and the other associated with the Grand Lake area on the park's west side.[49] The west side of the park experiences more snow, less wind, and clear cold days during the winter months.[49]
Bedrooms enjoy air-conditioning and central heating, mini refrigerators, and free Wi-Fi while private bathrooms have rain showers and Jacuzzi whirlpools. A delicious full English breakfast is served each morning in the inn’s elegant dining room, and lunch and dinner can be taken at the inn on request. The inn is within walking distance of several excellent restaurants in Colorado Springs as well as other entertainment.
Dial (970) 586-1222 for a recorded message on the status of Trail Ridge Road. You may not know that our mountain makes its own weather, so it is not uncommon to have snow in July or August at the top of Trail Ridge Road. Such weather will only last for a few hours to a day, but if you are planning to cross over Trail Ridge Road, weather may hamper your travel. You also may find the road closed due to weather in early June and September/October.
The Pierre Shale formation was deposited during the Paleogene and Cretaceous periods about 70 million years ago. The region was covered by a deep sea—the Cretaceous Western Interior Seaway—which deposited massive amounts of shale on the seabed. Both the thick stratum of shale and embedded marine life fossils—including ammonites and skeletons of fish and such marine reptiles as mosasaurs, plesiosaurs, and extinct species of sea turtles, along with rare dinosaur and bird remains—were created during this time period. The area now known as Colorado was eventually transformed from being at the bottom of an ocean to dry land again, giving yield to another fossiliferous rock layer known as the Denver Formation.[58]
A small town in the southwest corner of Colorado, Durango offers visitors a wealth of fun-filled activities to fill up a weekend away. Explore the downtown area to see a National Historic District lined with charming shops, eateries and hotels in 19th-century buildings. The area also boasts an array of outdoor adventures, including excellent opportunities to hike, bike, fish, while those wanting to kick it up a notch can also indulge in snowboarding, horseback riding and white water rafting. A ride on the famous Durango & Silverton Narrow Gauge Railroad is a must, where visitors can soak in breathtaking mountain views from a steam-powered engine train.

At about 68 million years ago, the Front Range began to rise again due to the Laramide orogeny in the west.[58][59] During the Cenozoic era, block uplift formed the present Rocky Mountains. The geologic composition of Rocky Mountain National Park was also affected by deformation and erosion during that era. The uplift disrupted the older drainage patterns and created the present drainage patterns.[60]
Above tree line, at approximately 11,000 ft (3,400 m), trees disappear and the vast alpine tundra takes over.[69] Over one third of the park resides above the tree line, an area which limits plant growth due to the cold climate and strong winds. The few plants that can survive under such extreme conditions are mostly perennials. Many alpine plants are dwarfed at high elevations, though their occasional blossoms may be full-sized.[73]
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