close iframe icon
Banner

Fractured

The rocks at the Tessellated Pavement are Permian ( Malbina Formation) with beds which vary in thickness and composition ( some are mudstones, some are sandston...
Read more

The rocks at the Tessellated Pavement are Permian ( Malbina Formation) with beds which vary in thickness and composition ( some are mudstones, some are sandstones, all are poorly sorted and pebbly, and were formed during the Permian glacial period). The deposits have been compacted and deeply buried and are, only now, being exposed to erosion. The modern pavements at about mean sea level, reflect the erosion which has taken place since sea levels stabilised about 6,000 years ago. The cliffs have retreated since that time and continue to collapse in an irregular, fairly unpredictable way.
These rocks have been compacted and loaded by up to 3 km of other rocks since their formation. They were also deposited across an old escarpment formed along the early north-south boundary of a granite intrusion. The variations in thickness of the sequence and its compaction have produced a rock mass which has been pre-stressed with a variation in load stresses from west to east.When the load is released, by uplift and erosion, it tends to break north-south preferentially.
Also, the rocks, as they are exposed are attacked by the elements and the presence of salt is a key factor. Chemical processes may change the composition and lead to expansion of the rock, and it cracks. These minor cracks tend to have preferred orientations determined by the pre-stressing, or they trend toward those preferred orientations. Also, as the salt crystals form in each tidal cycle as the water on the surface evaporates, they expand and stress the rock surface.. The pores are enlarged and the rock is slowly blown apart, grain by grain.
The incipient joints link and grow with time and, if the beds are nearly horizontal and of the right composition and thickness, yield a regular pattern ultimately determined by the pre-stressing factors. The joints tend to straighten as they are widened by weathering and the patterns grow downward from the surface demonstrating their weathering-stress release origin. Patterns vary from bed to bed since bed properties are crucial. The complete combination of characters is rare and hence "tessellated" patterns are not common.
Nikon D700, Nikkor 17-35 mm @ 17 mm,
8.0 s @ f/18, ISO 100,
Singh Ray GND's

Read less

Views

270

Likes

Awards

Peer Award
scouthunt2778 Pblais petrpolach stevenwatkins unbrokenworld Saeva blairknoxphoto +6
Superb Composition
fotosbybh ericrporcher JoshuaVince Nilesh_P buzman
Magnificent Capture
lynhope loveMustangs tinyspike11
Absolute Masterpiece
jodieb75
All Star
Capture-Life
Outstanding Creativity
jamesgiles
Top Choice
OliverSteinPhotography

Top Ranks

Epic Puddles Photo ContestTop 10 rank
Epic Puddles Photo ContestTop 10 rank week 1
Nature And Patterns Photo ContestTop 20 rank
Nature And Patterns Photo ContestTop 20 rank week 2
Nature And Patterns Photo ContestTop 10 rank week 1
Composing With Leading Lines Photo ContestTop 20 rank

Categories


1 Comment |
fotosbybh PRO+
 
fotosbybh February 09, 2018
Beautiful. Our earth is so amazing. Thank you for sharing this and your detailed description!
See all
It’s your time to shine! ☀️

Share photos. Enter contests to win great prizes.
Earn coins, get amazing rewards. Join for free.

Already a member? Log In

By continuing, you agree to our Terms of Service, and acknowledge you've read our Privacy Policy Notice.