Schematic route — shows stop order only, not geography.
Approved photograph neededA GeoAstro photo of Coral Park will appear here.
Stop 1 of 5
Coral ParkOptional
From our programme
Starting point and a general explanation of the tour.
GeoAstro tour informationDraft · pending geologist reviewSources: GeoAstro Oman
Interactive What’s ahead on this route
Pillow-shaped lava structures, preserved in the rock.
Mountains of metamorphic rock that look like the Moon’s surface.
A single view of the stratigraphy from oldest to youngest.
Stromatolite, snowball and travertine rock in Al Ain village.
GeoAstro tour informationDraft · pending geologist reviewSources: GeoAstro Oman
Approved photograph neededA GeoAstro photo of Pillow lava basalt will appear here.
Stop 2 of 5
Pillow lava basalt
From our programme
Pillow-shaped lava structures, preserved in the rock.
GeoAstro tour informationDraft · pending geologist reviewSources: GeoAstro Oman
What the geologist sees
When basalt lava erupts under water, its surface chills instantly into a skin; lava pushes out in rounded lobes that pile up as “pillows”. Pillow shapes are evidence of an underwater eruption.
Approved photograph of Metamorphic rock outcrop needed
Scientific illustration Concept sketch: heat and pressure change a rock without melting it, lining its minerals up. Not a photograph of this stop.
Stop 3 of 5
Metamorphic rock outcrop
From our programme
Mountains of metamorphic rock that look like the Moon’s surface.
GeoAstro tour informationDraft · pending geologist reviewSources: GeoAstro Oman
What the geologist sees
Metamorphic rocks are existing rocks transformed by heat and pressure without melting. Their minerals often grow aligned, giving the rock a layered texture.
Minerals in random orientations.Heat and pressure begin to act.Grains rotate and recrystallise.Aligned grains give a layered “foliation” — without melting.
Approved photograph of Full super-sequences view needed
Simplified geological model Simplified column: glacial and carbonate Precambrian rocks, the angular unconformity, then Permian and Triassic limestones and young travertine. Not a photograph of this stop.
Stop 4 of 5
Full super-sequences view
From our programme
A single view of the stratigraphy from oldest to youngest.
GeoAstro tour informationDraft · pending geologist reviewSources: GeoAstro Oman
Simplified model Read an eroded dome
Flat layers: oldest at the bottom.The layers are folded up into a dome.Erosion slices off the top: the oldest layers appear in the middle.
A WhatsApp message is an enquiry, not a confirmed booking. Our team will reply to confirm availability, details and the programme. Experiences depend on sky and weather conditions.
A WhatsApp message is an enquiry, not a confirmed booking. Our team will reply to confirm availability, details and the programme. Experiences depend on sky and weather conditions.