On test server
Ramesh
ಚತುರ್ಮುಖ ಬಸದಿ / Jain Temple
Bahubali / Gomatashwara
Bahubali / Mahavera
View of a tropical town
View of Karkala
View of Karkala
ಕುಡ್ ಚಂಪ Tree
Vana Bhojan
Towards Kitchen - Vana bhojana
Last of the season
Halloween
Halloween
Got it
Lalbagh
Stream
Alma Mater
SVT
ವಸಂತಾ ಸಾಳ / Temple veranda
Construction / Remodeling
Elephant door /ಆನೆ ಬಾಗಿಲು
Elephant entrance
ಆನೆ ಬಾಗಿಲು
Sunrise in a French door
Autumn light in a thicket
Red squirrel and Autumn leaves
ಭೂತ ಗುಡಿ ಮೈದಾನ್ / Gandhi Maidan
Neighbours - roots
Neighbours - roots
Neighbours - roots
Roof tops / sky line
North West - view - roots
Looking West - roots
Looking East II ~ roots
Looking East ~ roots
Leaves
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Keywords
Authorizations, license
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- Photo replaced on 19 Dec 2016
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175 visits
Steps to Bahubali rock
Granite domes are domical hills composed of granite with bare rock exposed over most of the surface. Generally, domical features such as these are known as bornhardts. Bornhardts can form in any type of plutonic rock but are typically composed of granite and granitic gneiss.[1] As granitic plutons cool kilometers below the Earth's surface, minerals in the rock crystallize under uniform confining pressure. Erosion brings the rock closer to Earth's surface and the pressure from above the rock decreases; as a result the rock fractures. These fractures are known as exfoliation joints, or sheet fractures, and form in onionlike patterns that are parallel to the land surface. These sheets of rock peel off the exposed surface and in certain conditions develop domical structures.[2] Additional theories on the origin of granite domes involve scarp-retreat and tectonic uplift.
One hypothesis is that granite domes are uplifted blocks. This is the case with some granite domes but the fracture related exfoliation joints are what controls the steep slopes. Another theory that regards isolated bornhardts is that they remain after long-distance scarp recession. Moisture related weathering is what causes scarp recession. In the case of granite in a dissected landscape the dry granite high on a slope remains stable and acts as caprock. Granite below this is more easily weathered and eroded because it has been exposed to moisture and has weathered. This ultimately leads to the steepening of the slope and the collapse of higher slope elements as well as the maintenance of scarps of essentially constant inclination and morphology during backwearing.[4] ~ Source Wiki
HFF YE ALL, HAVE A GREAT FRINDAY, AND THE WEEKEND
Trudy Tuinstra, Diana Australis, Erika+Manfred, Marco F. Delminho and 7 other people have particularly liked this photo
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Happy weekend!
HFF and keep safe.
HFF and a good weekend
Dinesh club has replied to Trudy Tuinstra clubSorry for the belated HFF and have a nice week ahead!
Dinesh club has replied to Annalia S. clubSign-in to write a comment.