Earth Science Conservation Review

Hill's Port, The Gobbins, Island Magee - MineralogyAntrim
Hill’s Port, The Gobbins, Islandmagee, Co.Antrim, June 1997.
Summary Full report
Site Type: Coastal section, Roadside section
Site Status: ASSI
Council area: Mid & East Antrim Borough Council
Grid Reference: J485971
Bing maps: 54.80019,-5.69078
Google maps: 54.80019,-5.69078
Rocks
Rock Age: Tertiary
Rock Name: Antrim Lava Group, Lower Basalt Formation
Rock Type: Amydaloidal Basalt, Olivine Basalt
Interest
Minerals: Analcime, Analcite, Calcite, Chabazite, Gobbinsite, Natrolite, Zeolites, Heulandite, Levyne, Cowlesite, Mesolite, Gonnardite, Travertine
Other interest: amygdales
Summary of site:
Zeolites are a group of hydrated aluminosilicate minerals that commonly occur in basic volcanic rocks, particularly basaltic lavas. They are found in amygdales, mineral-filled bubbles trapped in the cooling lava and in fissures. They occur in zones that indicate their depth of burial, a phenomenon first recognised and described in Northern Ireland. The coastal cliffs around Hill’s Port, and further north at the Gobbins, contain a variety of zeolites including gobbinsite (a new zeolite mineral, discovered here in the late twentieth century).
The Antrim basalts are famous for the quantity and diversity of zeolites they contain.
The only threat to these coastal cliffs is from marine erosion which is just as likely to reveal more zeolites as it is to destroy them.

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