The Magic Gate - Part 2
Four Corners Region
The Colorado Plateau
Mesa Verde
From Durango, we ventured west on Highway 160 to the pre-Puebloan alcove and cliff dwellings at Mesa Verde National Park.  Mesa Verde contains the most famous of the Anasazi (or pre-Puebloan) sites in the Four Corners. 
 In 1965, the archeological sites appeared unchanged since their 
discovery in the 1870s.  With park rangers as our guides, we climbed 
traditional pole-ladders and peered into ancient living spaces and 
granaries.  On hands and knees, we squinted down into dark ceremonial 
chambers, known as kivas.  In contrast, today one views these ruins from
 behind fences, on well-marked trails.
For reasons both known and unknown, the society 
broke down, leading to the complete depopulation the Four Corners.  
Later, in the fifteenth and sixteenth centuries, the Navajo tribe, with 
ancestors traceable to Asia, Alaska and British Columbia, repopulated much of the area.
 British Columbia, repopulated much of the area.
Returning to Durango that night in 1965, we saw live
 television reports of riots in South Los Angeles.  Large areas of Watts
 and the Central City were ablaze.  Not unlike the pressures experienced
 by the pre-Puebloan cultures of 1250 CE, summer heat, overpopulation 
and competition for resources had led to violence in LA.  Unlike the 
pre-Puebloan, who could simply migrate south in search of water and new 
farmland, there was nowhere for the residents of South Los Angeles to 
go.  In a metaphor to the actions of the ancients, some Los Angelenos 
sacked and burned their own commerce and cultural centers.
The Disappearance
Rather than assuming that the pre-Puebloan tribes 
irrationally destroyed their own cultural landmarks, might we trace the 
initial cause of that destruction to large-scale seismic activity?  Even the largest earthquakes leave few 
long-term traces in the natural environment.  Toppled towers and 
caved-in kivas might be the best indicators we have that cataclysmic 
seismic activity provided impetus to the complete abandonment of the 
Four Corners area.
 large-scale seismic activity?  Even the largest earthquakes leave few 
long-term traces in the natural environment.  Toppled towers and 
caved-in kivas might be the best indicators we have that cataclysmic 
seismic activity provided impetus to the complete abandonment of the 
Four Corners area.  
 large-scale seismic activity?  Even the largest earthquakes leave few 
long-term traces in the natural environment.  Toppled towers and 
caved-in kivas might be the best indicators we have that cataclysmic 
seismic activity provided impetus to the complete abandonment of the 
Four Corners area.
 large-scale seismic activity?  Even the largest earthquakes leave few 
long-term traces in the natural environment.  Toppled towers and 
caved-in kivas might be the best indicators we have that cataclysmic 
seismic activity provided impetus to the complete abandonment of the 
Four Corners area.  Today, we find potsherds at many Four Corners 
sites.  Intact pottery is so rare that we find it only in museums and 
private collections.  Were the pre-Puebloan so careless as to destroy 
essentially all of their useful pottery or did seismic activity play a 
larger role than previously assumed?
Today, the consensus is that the last pre-Puebloan migrated away from the Four Corners, later to “reemerge” as the Hopi, Zuni and other Pueblo tribes.  The Hopi creation myth centers on the “sipapu”,
 a hole in the earth from which their ancestors arose.  Every ceremonial
 kiva in the Four Corners includes a symbolic sipapu in its floor.  
The great kivas provided communal warmth and shelter to the pre- Puebloan. 
 Since an earthquake could collapse their roof timbers, kivas also 
carried the risk of unexpected and immediate death.  After a swarm of 
catastrophic earthquakes around 1250 CE, did the pre-Puebloan survivors 
reemerge from the metaphorical sipapu of their collapsed kivas, only 
then to leave the land that had caused them so much death and 
destruction?
Puebloan. 
 Since an earthquake could collapse their roof timbers, kivas also 
carried the risk of unexpected and immediate death.  After a swarm of 
catastrophic earthquakes around 1250 CE, did the pre-Puebloan survivors 
reemerge from the metaphorical sipapu of their collapsed kivas, only 
then to leave the land that had caused them so much death and 
destruction?
 Puebloan. 
 Since an earthquake could collapse their roof timbers, kivas also 
carried the risk of unexpected and immediate death.  After a swarm of 
catastrophic earthquakes around 1250 CE, did the pre-Puebloan survivors 
reemerge from the metaphorical sipapu of their collapsed kivas, only 
then to leave the land that had caused them so much death and 
destruction?
Puebloan. 
 Since an earthquake could collapse their roof timbers, kivas also 
carried the risk of unexpected and immediate death.  After a swarm of 
catastrophic earthquakes around 1250 CE, did the pre-Puebloan survivors 
reemerge from the metaphorical sipapu of their collapsed kivas, only 
then to leave the land that had caused them so much death and 
destruction?Silverton
 Leaving Durango, we traveled north on Highway 550, also known as The Million Dollar Highway. 
 Whether the road derived its name from its initial construction cost or
 from silver-bearing ore crushed into its asphalt mixture is still a 
subject of conjecture.  In 1965, its new surface reflected light like a 
million diamonds in the afternoon sunshine.
Leaving Durango, we traveled north on Highway 550, also known as The Million Dollar Highway. 
 Whether the road derived its name from its initial construction cost or
 from silver-bearing ore crushed into its asphalt mixture is still a 
subject of conjecture.  In 1965, its new surface reflected light like a 
million diamonds in the afternoon sunshine.After negotiating the 10,910-foot Molas Divide, we descended into Silverton, Colorado, a former mining town now famous as the northern terminus of the Durango & Silverton Narrow Gauge Railroad. 
 Although winter sports are now a factor, the summer tourist trade 
generates most of the town’s revenue.  In late May 2008, a spring 
snowstorm closed Highway 550 near Silverton, forcing us to make a 
low-elevation detour in order to reach Moab, Utah.
 terminus of the Durango & Silverton Narrow Gauge Railroad. 
 Although winter sports are now a factor, the summer tourist trade 
generates most of the town’s revenue.  In late May 2008, a spring 
snowstorm closed Highway 550 near Silverton, forcing us to make a 
low-elevation detour in order to reach Moab, Utah.  
 terminus of the Durango & Silverton Narrow Gauge Railroad. 
 Although winter sports are now a factor, the summer tourist trade 
generates most of the town’s revenue.  In late May 2008, a spring 
snowstorm closed Highway 550 near Silverton, forcing us to make a 
low-elevation detour in order to reach Moab, Utah.
 terminus of the Durango & Silverton Narrow Gauge Railroad. 
 Although winter sports are now a factor, the summer tourist trade 
generates most of the town’s revenue.  In late May 2008, a spring 
snowstorm closed Highway 550 near Silverton, forcing us to make a 
low-elevation detour in order to reach Moab, Utah.  By James McGillis at 12:10 PM | Travel | Comments (0) | Link


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