Region 4 is the heart of the park with easy road and trail access, great views, and lake hikes including the most popular trails.[35] 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.[44]
Have a company outing, family reunion or just a bunch of friends that want to get together on the mountain?  E-Tow Cabin is the perfect place for your next outing.  Reserve the E-Tow Cabin and you and your group will have exclusive access to the cabin for the day. Cook lunch on the propane grill, warm up next to the wood burning stove and enjoy the view from the deck with friends and family. Advance reservations are required.  No taxi rides up or down for guests or supplies.  All guests must ride lift up with skis or snowboard.  Not for overnight use. Rental for groups of 10 or more.
Cassie Abel, 28, of Denton, Texas, pulls her daughter Brynlee, 6, in a sled on a road that would normally be open to cars in Rocky Mountain National Park on Wednesday, Jan. 2, 2019. Abel's father-in-law, Shane Abel, 63, left, said he's frustrated a government shutdown nearly 2,000 miles away was hindering the family vacation.  (Photo: Trevor Hughes, Trevor Hughes-USA TODAY NETWORK)
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.[61] 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.[60] Many sedimentary rocks from the Paleozoic and Mesozoic eras exist in the basins surrounding the park.[62]
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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