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Gobustan Mud Volcanoes

Gobustan Mud Volcanoes

Volcanoes & CratersAzerbaijanQaradağ District, Baku,Azerbaijan

Twenty-odd cold mud cones on a cracked Azerbaijani plain by the Caspian, driven not by heat but by gas pushing clay and brine from below.

September·Peaking now

Sep–Oct

Autumn is the other walkable window: the fierce heat breaks to highs near 27°C in September and 21°C in October, and the plain is quiet. The low light off the Caspian suits the long loop out to the furthest cones.



Year-round The cones bubble cold mud all year — gas-driven, not weather-driven, so the eruptions never pause. What turns with the season is the steppe's colour and how bearable the shadeless, windy plain is to walk.

The Gobustan Mud Volcanoes are twenty-odd cones of cold grey mud on a cracked plain by the Caspian Sea in the Qaradağ district south of Baku, in Azerbaijan, driven not by heat but by gas pushing clay and brine up from below, and they are walked among on the plain, watched one at a time from a few metres back as they gurgle and spit, and climbed for the sea on the horizon. Azerbaijan holds nearly half the mud volcanoes on Earth, some four hundred, because the country sits on the oil and gas that push them up, and where a mud volcano stands, oil usually lies far beneath it, which is how the industry followed the mud; the cones at Dashgil are a metre or a few metres high, each with a crater of grey slurry that bulges, breaks and slumps as a bubble of gas comes through, cold to the touch and slow enough that a single crater is timed from five metres back, and where the mud spilled out and dried the surface has shrunk into a tight mosaic of polygonal plates that crunch and tilt underfoot. The cones only gurgle, but the big ones of the region catch fire, when the gas ignites and throws flames hundreds of metres up, as one did in the Caspian in 2021. Planetary scientists come to these flows to understand Mars, where landforms long read as lava are now thought to be mud that erupted much the same way, and the field is reached by a rough track from the main road. A marked track runs out across the plain for quad bikes between clusters of cones the footpaths never reach, and the taller cones at the far edge are enough for the Caspian on the horizon. For a few weeks in spring the bare semi-desert greens and flowers with steppe irises, and the rock engravings of Gobustan are on the same road. The Gobustan volcanoes are the earth belching cold mud, and the oil underneath is the reason.

Worth knowing

Good to know

  • Everything runs through the tourism complex now — park off the E119 highway, then cross the field on foot or take a quad bike along the marked track out to the further, more active cones.
  • Wear shoes you will not miss — the grey clay is greasy while wet, sets like cement once dry, and never really comes out of fabric again.
  • Go at opening — the day-tour buses from Baku roll in around midday, and there is no shade on the plateau at all, so the first hour is both the emptiest and the coolest.
  • Walk past the busy craters near the entrance — from the cones at the far edge of the field, the grey plain opens straight onto the flat blue of the Caspian.
  • Carry your own water — there is none out on the plateau, and the loop to the furthest cones is longer and far more exposed than it looks from the car park.

Things to do

  1. 1

    Time a single cone from five metres back

    Time a single cone from five metres back

    Pick one crater and wait. The mud swells into a dome, holds, then bursts with a wet plop, and the interval is different for every vent. Between the cones lie wide soupy pools where the gas comes up in slow rings instead, breaking the surface without ever building a cone at all.

  2. 2

    Climb a cone for the Caspian on the horizon

    Climb a cone for the Caspian on the horizon

    The taller cones at the far edge of the field are only a few metres high, but that is enough. From the lip, the grey volcanic plain runs out ahead of you and drops away to the flat blue of the Caspian — the view that makes sense of where all this mud comes from.

  3. 3

    Ride the quad-bike track across the field

    Ride the quad-bike track across the field

    A marked track runs out across the cracked plain, between clusters of cones the footpaths never reach. It is the quickest way to feel how far the volcanic field really stretches, and how completely empty the steppe around it is.

  4. 4

    Read the cracked crust of an old mud flow

    Read the cracked crust of an old mud flow

    Where mud spilled out and dried, the surface has shrunk into a tight mosaic of polygonal plates that crunch and tilt underfoot. Fresh flows are still soft and grey-wet; older ones curl at the edges, a record of every eruption the cone has had.

Watch

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