Gugerd Mountain

🧭What kind of place is it?

The mountain formed as the forces building the Alborz compressed desert rock layers. An anticline is an upward fold in those layers. Erosion removed some overlying muddy sediments and exposed the older central gypsum. The mountain rises about 600 m above the surrounding plain.

🏛️What was it built for?

The attraction is the desert landscape and geology. The ridge, folded strata and contrast between central rocks and surrounding sediments help explain how the mountain formed.

👀What you will see

• The central gypsum core was exposed as the overlying sedimentary cover eroded away.
• Bent rock layers reveal the anticline's folded form in the landscape.
• The highest summit, at 1,489 m, stands east of the gypsum ridge.
• The eastern anticline is called Kuh-e Taghi, with a highest point of 1,274 m.

🎒Good to know before you go

• Ask the local environment office about permits and permitted routes, and go with a guide who knows the desert.
• Carry enough water and sun protection, and plan to return before dark.
• Do not enter channels, soft ground or unfamiliar salt flats, and do not collect rocks or sediment.