Flatirons Geology
Lateral view on flatirons along Tekeze River, Ethiopia The Flatirons (prominences & flat slopes) overlooking Boulder, Colorado Novaculite flatirons on the flank of East Bourland Mountain in the Marathon Uplift of West Texas [1] Colourful flatirons in the Serranía de Hornocal of Jujuy Province, Argentina Traditionally in geomorphology, a flatiron is a steeply sloping triangular landform. Red Rocks and Dinosaur Ridge from the Earth Observatory. Geology of the Boulder Area from the Boulder Area Sustainability Information Network.
The Geology Along the Trails West of NCAR by Emmett Evanoff and Sue E. Hirshfeld, Colorado Scientific Society. Ancient Denvers from the Denver Museum of Nature and Science.
Flatirons | The Flatirons are rock formations near Boulder, … | Flickr
Flatirons from Wikipedia. Geology of Boulder Flatirons The Fountain Formation by Dick Gibson Back to Geology Of. Back to Jefferson County Open Spaces The Fountain Formation is a sandstone of Pennsylvanian age that crops out along the Front Range in Colorado.
The Boulder Flatirons are a striking geological formation located just west of Boulder, Colorado. The Flatirons are a series of steep, triangular rock formations that rise sharply from the foothills of the Rocky Mountains, creating a stunning backdrop for the city of Boulder. With a name like Boulder, you'd expect our beautiful Open Space and Mountain Parks to sport some pretty impressive rocks.
Flatirons Classic Climb: Climb The Flatirons with a Professional Guide
You won't be disappointed-the dramatic Flatirons rise supremely above Chautauqua Meadow, and are a vivid testimony to the incredible geologic forces of nature that have formed and sculpted the magnificent scenery. For many, the Flatirons symbolize Open Space and Mountain. Traditionally in geomorphology, a flatiron is a steeply sloping triangular landform created by the differential erosion of a steeply dipping, erosion-resistant layer of rock overlying softer strata.
Flatirons have wide bases that form the base of a steep, triangular facet that narrows upward into a point at its summit. The dissection of a hogback by regularly spaced streams often results in. The Flatirons were formed when the Permian/Pennsylvanian.
Unique Landscapes: Flatirons of Colorado | Tipsy from the TRIP
The Flatirons, tilted rock slabs pasted on Green Mountain and South Boulder Peak, form Boulder's iconic mountain skyline. The huge red Flatirons were named for their resemblance to flat irons, metal pieces that were heated and used to press clothes by pioneer women in the 19th century. Five main formations-called the First, Second, Third, Fourth, and Fifth Flatirons.
The Flatirons are rock formations in the western United States, near Boulder, Colorado, consisting of flatirons. There are five large, numbered Flatirons ranging from north to south (First through Fifth, respectively) along the east slope of Green Mountain (elev. 8,148 ft or 2,484 m), and the term "The Flatirons" sometimes refers to these five.
Traditionally in geomorphology, a flatiron is a steeply sloping triangular landform created by the differential erosion of a steeply dipping, erosion-resistant layer of rock overlying softer strata. Flatirons have wide bases that form the base of a steep, triangular facet that narrows upward into a point at its summit.
