Jess and I recently visited Colorado, which was my first visit to this wonderfully mountainous part of the US. We were primarily there to attend a travel influencers conference, but we tacked on a few days to do a bit of sight-seeing, starting off in the capital of Denver, where I watched my first ever baseball game, after which we headed out to explore some of those incredible mountains.
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Colorado Cabin Adventures is the perfect mix of comfortable and rustic. For the outdoor enthusiast who loves to explore and wants to climb the highest peak, we are ideally located. For the aficionado of all things fabulous, who hopes to find inspiration, we are nicely decorated. For the rest of the crew, who goes with the flow and wants to just have fun, we are Colorado Cabin Adventures.
There are four ecosystems, or zones, in Rocky Mountain National Park: montane, subalpine, alpine tundra, and riparian. The riparian zone occurs throughout all of the three other zones. Each individual ecosystem is composed of organisms interacting with one other and with their surrounding environment. Living organisms (biotic), along with the dead organic matter they produce, and the abiotic (non-living) environment that impacts those living organisms (water, weather, rocks, and landscape) are all members of an ecosystem.
Where your Rocky Mountain Adventure begins! Our conveniently located, 1910 rambling mountain inn is snuggled in amidst towering pine and aspen with an expansive view of the Estes Valley. The inn consists of four luxury suite, all with private baths with fireplaces and whirlpool tubs for two. Two luxury cabins sleep up to six and have a full kitchen.
The Pool is a large turbulent water pocket formed below where Spruce and Fern Creeks join the Big Thompson River. The winter route is along a gravel road, which leads to a trail at the Fern Lake trailhead. Along the route are beaver-cut aspen, frozen waterfalls on the cliffs, and the Arch Rocks. The trail to Alberta Falls runs by Glacier Creek and Glacier Gorge.
Rocky Mountain National Park, established in 1915, is a living showcase of the grandeur of the Rocky Mountains. Located outside Estes Park, Colorado, Rocky Mountain is a great family vacation destination, offering outdoor experiences for all—from easy nature hikes around crystal clear mountain lakes to daring rock scrambles up waterfalls and mountains.
There is also plenty for you to explore in the surrounding areas. If you head south, you’ll reach Red Rocks Park, which is known for its red rock formations. Head east, and you’ll find yourself in Denver, where you can experience a taste of the city, complete with shopping and dining options. Head west, and you’ll be in the Rocky Mountains, with options to ski.
Timber Creek: The only campground on the park's west side, Timber Creek is often the best bet for those seeking an open spot on a first-come basis. This campground offers 98 sites, accommodations for RVs up to 30 feet, a dump station and water hook-ups. Timber Creek is summer only and access from Estes Park is available only when Trail Ridge Road is open (usually Memorial Day through mid-October, depending on weather) approximate drive time from Estes Park is an hour and a half.
The Mummy Range is a short mountain range in the north of the park. The Mummies tend to be gentler and more forested than the other peaks in the park, though some slopes are rugged and heavily glaciated, particularly around Ypsilon Mountain and Mummy Mountain. Bridal Veil Falls is a scenic point and trail accessible from the Cow Creek trailhead, at the Continental Divide Research Center. West Creek Falls and Chasm Falls, near Old Fall River Road, are also in this region. The Alluvial Fan trail leads to a bridge over the river that had been the site of the Lawn Lake Flood.
Region 4 is the heart of the park with easy road and trail access, great views, and lake hikes including the most popular trails. Flattop Mountain is a tundra hike and the easiest hike to the Continental Divide in the park. Crossing over Flattop Mountain, the hike to Hallett Peak passes through three climate zones, traversing the ridge that supports Tyndall Glacier and finally ascending to the summit of Hallett Peak.
First – Rocky Mountain National Park is open year round, 24 hours a day. So no worries there. However, if you want to drive Trail Ridge Road, you need to visit from around the end of May to early October. July through September are the busiest time of year, so my recommendation to avoid the crowds and still get good weather, plus plenty of light for activities, would be June.
Did some snowshoeing today(2/17/19), great conditions for it! We got to the trail and started about 8:45 am, snow was still fresh. Parking lot wasn’t too crowded and didn’t really see too many others until we were heading back. Only a few spots uphill, relatively even terrain with nice views. Did Copeland Falls and Calypso Cascades, a short part of Ouzel falls to the overlook, which was a good point to turn around.
Our award winning Yogi Bear’s Jellystone Parks have everything you and your family will need to make long lasting camping memories. From amazing water zones including splashparks and splash pads, to mini golf, wagon rides, volleyball and fishing to themed weekends and family camping oriented activities including appearances from Yogi Bear™ and friends – you’ll notice that family fun at our family campgrounds is the main attraction! And with over 80 locations in the United States and Canada, you will have a quality camping experience that is close to home.
This charming cabin is found in Nederland, Colorado, right in the thick of the wilderness. This spacious cabin will give newlyweds the perfect setting to begin the start of married life with the comfort of high-end amenities and gorgeous views of the great outdoors from the comfort of an incredible accommodation. With all the amenities and facilities you would need for a home, a full kitchen, queen sized bed, full entertainment system, and a BBQ, couples will love their escape to this rental. This cabin is nestled into the Rocky Mountains, providing couples with a lot of new adventures to embark on.
Our friendly and knowledgeable event staff is ready to help you set up and organize the wedding reception of your dreams in Estes Park. Feel free to reach out with any questions, no matter where you are in your wedding planning. Give us a call at 970-480-4012 or send us your contact info in our Request For Information form, and our professional event staff will get right back to you.
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.
Staying or coming to Estes Park for your honeymoon? You will find a wide variety of romantic experiences to make your extended stay full of intimate moments and memorable highlights. Many properties off special honeymoon packages that include indulgences like couples massages, chocolates, champagne and more. Whether or not you ever leave your room, Estes Park honeymoons will create memories to last a lifetime.
If you and your partner are looking to get off the grid after months of wedding planning, then head to these cabins located on the banks of Bear Creek. Walk or relax near the creek and share the view with wildlife who live on the land. Have complimentary breakfast brought to you as you lounge in a comfy chair along the water, or spend some time in the hot tub right on the creek to unwind. For dinner, enjoy pizza from the brick oven on the patio and socialize with other couples.
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.
Your wedding night should be as special as the ceremony. Ensure yours is perfect by choosing the right place to stay. Whether you want to retire to a hotel room next to family and friends or escape to a secluded, private cabin, Estes Park lodging properties fulfill your needs. Sink into suites outfitted with personal hot tubs. Lay before a roaring fire, just you and the love of your life. Walk hand-in-hand along wooded paths beside a gurgling river. Estes Park accommodations make it possible to enjoy these experiences and more. Plus, they extend the same hospitality to your wedding guests, turning your ceremony into a true destination wedding. Book suites, hotel rooms, cabins—even private vacation homes for your wedding. From rustic to historic, Estes Park offers a range of accommodations.
Above tree line, at approximately 11,000 ft (3,400 m), trees disappear and the vast alpine tundra takes over. 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.
Glacial geology in Rocky Mountain National Park can be seen from the mountain peaks to the valley floors. Ice is a powerful sculptor of this natural environment and large masses of moving ice are the most powerful tools. Telltale marks of giant glaciers can be seen all throughout the park. Streams and glaciations during the Quaternary period cut through the older sediment, creating mesa tops and alluvial plains, and revealing the present Rocky Mountains. The glaciation removed as much as 5,000 feet (1,500 m) of sedimentary rocks from earlier inland sea deposits. This erosion exposed the basement rock of the Ancestral Rockies. Evidence of the uplifting and erosion can be found on the way to Rocky Mountain National Park in the hogbacks of the Front Range foothills. Many sedimentary rocks from the Paleozoic and Mesozoic eras exist in the basins surrounding the park.
^ Montana State University states in their profile of Rocky Mountain National Park that there has been an increase of 2.5 °F (1.4 °C) in the average park temperature over "the past century" (charts show the period from about 1895-2010). The National Park Service site states that the increase has been 3.4 °F (1.9 °C) over "the last century" (chart shows the period from about 1905-2010).
Back to the Fall River Road, and it’s just another few hundred yards to the Sheep Lakes Information Station. From here you have about the best chance in the park to see the Rocky Mountain Bighorn Sheep, a truly impressive sheep species that is notable for its agility, as well as having enormous horns. Be sure to keep your distance from the sheep and any other animals here, they are wild animals and this is their home!