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Sunset in Arches, Utah Custom Invites
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Sunset in Arches, Utah Custom Invites
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Product Details

Sold by Zazzle
Designed by hikingviking
Size: 5" x 7" Invitation

Make custom invitations and announcements for every special occasion! Add photos and text to both sides of this flat card for free.

  • 5" x 7" (portrait) or 7" x 5" (landscape). Additional sizes available.
  • High quality, full-color, full-bleed printing on both sides.
  • 20 unique paper types and colors.
  • Standard white envelope included.
  • Premium Envelopments pocket folds, colored envelopes, and envelope liners available.
  • Postage rate for this size invitation (up to 1 oz.) is $0.49.
  • Designer Tip: To ensure the highest quality print, please note this product’s customizable design area measures 5" x 7". For best results please add 1/16" bleed.
Paper Type: Basic
Our basic smooth paper features a semi-glossy finish designed for vibrant full-color photo printing. 110lb cover-weight, 12.4 point thickness. 50% recycled content (10% post-consumer and 40% pre-consumer waste).
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About the Design

Sunset in Arches, Utah
Arches National Park is a U.S. National Park in eastern Utah. It is known for preserving over 2000 natural sandstone arches, including the world-famous Delicate Arch, in addition to a variety of unique geological resources and formations. The park is located just outside of Moab, Utah, and is 76,679 acres (31,031 ha) in area. Its highest elevation is 5,653 feet (1,723 m) at Elephant Butte, and its lowest elevation is 4,085 feet (1,245 m) at the visitor center. Forty-three arches have collapsed due to erosion since 1970. The park receives 10 inches (250 mm) of rain a year on average. The national park lies atop an underground evaporite layer or salt bed, which is the main cause of the formation of the arches, spires, balanced rocks, sandstone fins, and eroded monoliths in the area. This salt bed is thousands of feet thick in places, and was deposited in the Paradox Basin of the Colorado Plateau some 300 million years ago when a sea flowed into the region and eventually evaporated. Over millions of years, the salt bed was covered with debris eroded from the Uncompahgre Uplift to the northeast. During the Early Jurassic (about 210 Ma) desert conditions prevailed in the region and the vast Navajo Sandstone was deposited. An additional sequence of stream laid and windblown sediments, the Entrada Sandstone (about 140 Ma), was deposited on top of the Navajo. Over 5000 feet (1500 m) of younger sediments were deposited and have been mostly eroded away. Remnants of the cover exist in the area including exposures of the Cretaceous Mancos Shale. The arches of the area are developed mostly within the Entrada formation.[4] The weight of this cover caused the salt bed below it to liquefy and thrust up layers of rock into salt domes. The evaporites of the area formed more unusual salt anticlines or linear regions of uplift.[4] Faulting occurred and whole sections of rock subsided into the areas between the domes. In some places, they turned almost on edge. The result of one such 2,500-foot (760 m) displacement, the Moab Fault, is seen from the visitor center. As this subsurface movement of salt shaped the landscape, erosion removed the younger rock layers from the surface. Except for isolated remnants, the major formations visible in the park today are the salmon-colored Entrada Sandstone, in which most of the arches form, and the buff-colored Navajo Sandstone. These are visible in layer cake fashion throughout most of the park. Over time, water seeped into the surface cracks, joints, and folds of these layers. Ice formed in the fissures, expanding and putting pressure on surrounding rock, breaking off bits and pieces. Winds later cleaned out the loose particles. A series of free-standing fins remained. Wind and water attacked these fins until, in some, the cementing material gave way and chunks of rock tumbled out. Many damaged fins collapsed. Others, with the right degree of hardness and balance, survived despite their missing sections. These became the famous arches. Source Wikipedia http://en.wikipedia.org/wiki/Arches_National_Park
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Designed By hikingviking :

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Make custom invitations and announcements for every special occasion! So much more than quality paper with vibrant, full-color printing, these invitations set the tone for your big event. Pick from 8 sizes and 5 paper types for a correspondence piece as unique as the celebration itself. Start the party right with invites and RSVP cards so cool they call for a toast of their own! Zazzle Invitations are produced out of our brand new, state-of-the-art printing facility in San Jose, California. We use quite literally the most cutting-edge digital printing technologies in the world in order to offer the highest quality, greatest breadth of options, and fastest turnaround. We're pretty proud to be manufacturing right in the heart of Silicon Valley and we hope you love our products as much as we love making them for you.
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Paper Type:
Our basic smooth paper features a semi-glossy finish designed for vibrant full-color photo printing. 110lb cover-weight, 12.4 point thickness. 50% recycled content (10% post-consumer and 40% pre-consumer waste).
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Other Info

Product ID: 161931674176123143
Made on: 2/27/2012 8:07 AM
Reference: Guide Files