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Bell Rock

Jon Burch Photography

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Bell Rock Photograph  - Bell Rock Fine Art Print
 

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Tags: sedona photographs, arizona photographs, red rocks photographs, jon burch photography photographs, jon burch photographs, sedona canvas prints, sedona iphone cases, arizona canvas prints, arizona iphone cases, red rocks canvas prints, red rocks iphone cases, jon burch photography canvas prints, jon burch photography iphone cases, jon burch canvas prints, jon burch iphone cases

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Accrington, La - United Kingdom

What a stunning image, gosh you live in a fabulous part of the world. Excellent shot.

Thank you very much Irene! I try to get to Sedona when ever I can.

Long Beach, CA - United States

Beautiful work, Jon! Voted

Thank you Heidi! I love it in Sedona.

Farmington, NM - United States

Gorgeous, the complimentary colors...v

Thank you Janis! Going back to Sedona this weekend.

Selah, WA - United States

Beautiful work Jon

Thank you Jeff!!

Loveland, CO - United States

Thank you for the feature in Red Rock Country! I appreciate it.

Azuga, PH - Romania

Wonderful image !

Just found your post. Thank you very much! - JB

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Title

Bell Rock

Artist

Jon Burch Photography

Medium

Photograph - Digital Capture

Description

This is the south side of Bell Rock in Sedona, Arizona - actually it is in Oak Creek, just south of Sedona a couple miles. Either way, if you haven't been there, add it to your 'bucket list!'
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Defining the boundary between the Colorado Plateau to the north, the Basin and Range to the south and the base of the Mogollon Rim, Courthouse Butte, Bell Rock and the other red rocks form an escarpment that runs east-west through the middle of Arizona. The Mogollon Rim is about 200 miles long, and ranges between 2000 and 3000 feet in height. But in the Sedona region, erosion has gradually eaten away at the rim, moving it northward a distance of about four miles and leaving behind some of the most spectacular and picturesque canyons and buttes found anywhere in the world.
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The deep red color for which Sedona is famous is due to the presence of hematite or iron oxide, staining the sandstone of Schnebly Hill and Hermit Shale layers. The steep terrain is due the top layers of the strata being composed of basalt and limestone, which are both harder than the underlying sandstone. Water running off the edge of the escarpment dissolves the lower layers, creating the steep cliffs. Eventually enough soft material is broken down and eroded, undercutting the cap layer, subsequently breaking it off in large slabs allowing it to fall into the canyons. This process exposes new softer material and the process repeats, with the cliff face about twenty feet further north than it was before.
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The red rocks themselves were formed by a layer of rock known as the Schnebly Hill Formation. Schnebly Hill is a thick layer of red to orange-colored sandstone, and a member of the Supai Group, which was deposited during the Permian Period about 299 to 251 million years ago. Approximately 800 to 1000 feet thick, Schnebly Hill is the major component of Sedona's well known "Red Rocks" visible in the area.
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The Schnebly Hill formation is comprised of the Sycamore Pass and Bell Rock members, which are separated by a ten to twelve foot thick layer of grey-colored limestone called the Fort Apache Member, formed during a major incursion of an ancient Sea. There are no fossils in the Schnebly Hill sandstones, and virtually none in the thin limestone layers.
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Photograph copyright Jon Burch Photography

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March 30th, 2012

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