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      Close to Heaven… Down to Earth


Frontier Pathways

Wetmore to McKenzie Junction

The drive from Pueblo to Wetmore takes you out of the high plains climate zone and
into the low montane zone. This is seen by the effects of the increase in precipitation:
the grasses and cacti give way to the junipers and pinons of the foothills.

Hardscrabble Creek

This section of the Frontier Pathways Scenic & Historic Byway travels up Hardscrabble Canyon to McKenzie Junction.
The canyon is narrow and very rugged here, with large granite outcroppings and lots
of water flowing.

Over 150 years ago this area was populated by French traders, scrappy Americans
and Mexican farmers and their families. In 1844 several Americans from El Pueblo
established a Trading Post at San Buenaventura de los Tres Arrollos, a name changed
a short while later to Hardscrabble. According the George Simpson, this was because
of the “hard scrabbling to get in a crop” in the gravelly soil. In 1846, a dry year
had most of Hardscrabble’s residents packing. When John C. Fremont came through
in 1848 he found the settlement at Hardscrabble almost completely deserted.

The granite that composes most of the Wet Mountains solidified some 1.7+ billion
years ago, in the Pre-Cambrian era (essentially, before any life began on Planet
Earth). It’s the same age as the granite in the Blanca Massif. While most of this mountain range is Pre-Cambrian granite,
there are a couple areas of Cambrian metamorphic rock (north and east of Lake DeWeese)
and the rock deposited at the top of Greenhorn Mountain is only about 25 million years old and solidified about the same
time as the Spanish Peaks and the Silver MountainMt. Mestas group. The mining areas around Querida and Rosita are in rock about the same age as the top of Greenhorn (Oligocene/Middle Tertiary period).