Arches National Park Utah
Arches National Park Moab Utah
Arches
National Park is located in Southeastern Utah in Grand County. Arches contains
one of the largest concentrations of natural sandstone arches in the world. The
arches and numerous other extraordinary geologic features, such as spires,
pinnacles, pedestals and balanced rocks, are highlighted in striking foreground
and background views created by contrasting colors, landforms and textures.
With the addition of the Lost Spring Canyon area, the park is 76,519 acres in
size.
Arches
National Park is open year-round. The majority of park visitors come March
through October, with lowest visitation in December and January. You can enjoy
sightseeing by personal car, hiking, biking (established roads only),
picnicking (3 designated picnic areas in park), and camping.
Geologic
Features and Processes: Over
two thousand natural sandstone arches, the greatest concentration of rock
arches in the world, are preserved in Arches National Park. Most arches are
formed in three named geologic units (the Dewey Bridge Member of the Carmel
Formation, the Slick Rock Member of the Entrada Sandstone, and the Moab Member
of the Curtis Formation). In addition to the arches, Arches National Park is
home to an extraordinary collection of balanced rocks, salt dissolution
structures, folds resulting from salt tectonics, petrified dune fields, and a
maze of deep narrow canyons.
The
arches are a result of a unique geologic history. This history involves the
formation of salt deposits (back in Middle Pennsylvanian to Late Triassic time;
circa 300 million - 228 million years ago), and other sedimentary deposits
(from Middle Pennsylvanian to Late Cretaceous time; circa 300 million to 70
million years ago), as well as the folding and faulting of these deposits in
Tertiary time (circa 65 million to 2 million years ago) and finally to Quaternary
(last 2 million years) erosion and salt dissolution. At Arches, the proper
conditions for arch formation all coalesce.
These include the following:
·
Presence
of massive hard brittle sandstones jointed by faulting activity
·
Resting
on or containing soft layers or partings
·
Located
near salt-cored anticlines experiencing dissolution
·
A
dry climate
Arches
National Park contains many "classic" or “iconic” geological sites.
Among these are the following:
·
Landscape
Arch
·
The
Windows Section
·
Devils
Garden
·
The
Great Wall
·
Klondike
Bluffs
·
Moab
Fault
·
Fiery
Furnace
·
Cache
Valley
·
Elephant
Butte Folds
·
Petrified
Dunes
·
The
La Sal Mountains viewpoint (though well south of Arches NP; it is an important
viewshed feature)
Arches
National Park has over 2,000 stone arches, this particular free-standing arch
has become a widely recognized symbol of the state of Utah and one of the most
famous geologic features in the world.
How to
Reach: Arches
National Park is located in Moab, Utah and is accessible by air or car from Las
Vegas, Salt Lake City, and Grand Junction. Here’s how we recommend getting to
Arches.
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