Glacier Basin: Located on Bear Lake Road, approximately six miles south of the Beaver Meadows Entrance Satation, this 150 site campground provide easy access to many areas of the East side of the park. Reservations are available for this popular summer-only campground which offers a shuttle stop, tent & RV (35 feet) spots and on-site Ranger-led evening programs. 
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]
Slightly strenuous hike. The first portion (after the trail splits from Bear Lake) is primarily uphill. Snowshoes are a great asset to have here. After some breaks to catch our breath, we made it to Nymph Lake, which offered a gorgeous view and prime photo opportunity. Then, across the lake continued the trail. More uphill climbing, followed by a beautiful vista and Dream Lake, which was very windy but gorgeous. Then came a 20-25 minute steep hike up to Emerald Lake, snowshoes REQUIRED for this portion. The steep hike is worth it as you emerge from forest to a view unlike any other. There are plenty of spots to enjoy lunch with an incredible view of tall peaks and the frozen lake.
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The rain started to head in, but we shifted plans a bit (the park is huge - one side can have rain while the other is sunny) and got to Alluvial Fan, Bear Lake, Nymph Lake and Dream Lake among some other spots. We also drove through most of the park and went to the Alpine  Visitor Center - 11,796 feet up! It's the highest elevation Visitor Center in the park. Great views. Such a different feel - it was cold and there was snow on the ground. In July!
The climate change study projects further temperature increases, with greater warming in the summer and higher extreme temperatures by 2050. Due to the increased temperature, there is a projected moderate increase in the rate of water evaporation. Reduced snowfall—perhaps 15% to 30% less than current amounts—and the elimination of surface hail, along with the higher likelihood of intense precipitation events are predicted by 2050. Droughts may be more likely due to increased temperatures, increased evaporation rates, and potential changes in precipitation.[53]
Trail Ridge Road is 48 miles (77 km) long and connects the entrances in Grand Lake and Estes Park.[92][93] Running generally east–west through many hairpin turns,[5] the road crosses Milner Pass through the Continental Divide[93] at an elevation of 10,758 ft (3,279 m).[92][94] The highest point of the road is 12,183 feet (3,713 m),[93] with eleven miles of the road being above tree line which is approximately 11,500 feet (3,505 m).[92] The road is the highest continuously paved highway in the country,[93] and includes many large turnouts at key points to stop and observe the scenery.[92]

If driving Trail Ridge Road or Old Fall River Road is on the top of your list and you have limited time, you may want to enter the park via the Fall River Entrance on the park’s east side. It also is just a few minutes from Estes Park’s downtown. You’ll reach Trail Ridge Road a lot faster than those waiting in line at the Beaver Meadows Entrance during the summer and fall seasons.
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