Unlock the joy of Easter with our extensive range of travel packages.
Inquire Now
Customize Your Dream Vacation
Get in touch with our local experts for hassle-free trip planning.

Al Khoud Unconformity in Oman

Need help in building your itinerary?
Contact us and unlock an unforgettable adventure with the help of our local experts.
Join Our Newsletter
Suggested Tours
Around 34 to 23 million years ago, this part of Oman was much lower than it is today and covered by a shallow sea. The Mid Tertiary limestone originally formed in horizontal layers on the sea floor. Over time the rock layers became slightly titled. If you take a closer look you can see this by following the grey lines in the limestone. The land was later uplifted. Then, in the last 2 million years, a large wadi deposited layers of gravels of various sizes and of different origins, burying the marine formation. These gravels became cemented together to form a rock called conglomerate.
 
Here, as there is a gap in time between the deposition of the limestone and conglomerate, the meeting of the two layers of rock is called an unconformity.