The Giant's Causeway is a UNESCO World Heritage site located in Northern Ireland, composed of approximately 40,000 hexagonal basalt columns resulting from volcanic activity 60 million years ago. The columns formed as lava slowly cooled and contracted, cracking in a hexagonal pattern. Some columns reach 12 meters high. The site owes its existence and distinctive coastal features to the interaction of geology, glacial and coastal erosion history. Scientists used an experiment mixing water, corn starch and heat to model and explain the formation of the hexagonal columns, establishing a relationship between cooling rate and column size.
The Giant's Causeway is a UNESCO World Heritage site located in Northern Ireland, composed of approximately 40,000 hexagonal basalt columns resulting from volcanic activity 60 million years ago. The columns formed as lava slowly cooled and contracted, cracking in a hexagonal pattern. Some columns reach 12 meters high. The site owes its existence and distinctive coastal features to the interaction of geology, glacial and coastal erosion history. Scientists used an experiment mixing water, corn starch and heat to model and explain the formation of the hexagonal columns, establishing a relationship between cooling rate and column size.
The Giant's Causeway is a UNESCO World Heritage site located in Northern Ireland, composed of approximately 40,000 hexagonal basalt columns resulting from volcanic activity 60 million years ago. The columns formed as lava slowly cooled and contracted, cracking in a hexagonal pattern. Some columns reach 12 meters high. The site owes its existence and distinctive coastal features to the interaction of geology, glacial and coastal erosion history. Scientists used an experiment mixing water, corn starch and heat to model and explain the formation of the hexagonal columns, establishing a relationship between cooling rate and column size.
The Giant's Causeway is a UNESCO World Heritage site located in Northern Ireland, composed of approximately 40,000 hexagonal basalt columns resulting from volcanic activity 60 million years ago. The columns formed as lava slowly cooled and contracted, cracking in a hexagonal pattern. Some columns reach 12 meters high. The site owes its existence and distinctive coastal features to the interaction of geology, glacial and coastal erosion history. Scientists used an experiment mixing water, corn starch and heat to model and explain the formation of the hexagonal columns, establishing a relationship between cooling rate and column size.
The Giants Causeway is described in the 1985 UNESCO new inscribed property as a sea level promontory carved by the sea from the lowest colonnade of the Middle Basalts between Port Ganny and Port Noffer. It is constituted of 3 promontories which are the Grand, the Middle and the Little Causeways.
This place is known for
its 40,000 hexagonal columns, gently inclined or completely vertical. One of the most impressive formation is The Organ. These columns are due to the slow cooling and gradual contraction of the basalt. The resistance of this basalt to marine erosion explains the exceptional preservation of the place.
As can be seen on this
map of Northern Ireland, the Giant causeway is on a basalt rocks area, which were laid down around 60 million years ago, in the Tertiary age. Those basalts are due to the cooling of tertiary lava. The Antrim plateau were the Giant's causeway is located was formed above big cracks and fissures in the earth's crust.
Giants Causeway
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The work of a Giant ?
The Giants causeway is the result of an important volcanism activity that occurred 62 millions years ago in Antrim.
The Causeway is composed
of 40 000 basalts columns up to 12 meters high. The lower part of these columns is rich in olivine, a green mineral. The upper columns were formed by rain and erosion. The site is composed of columns because lava was trapped in valleys (which were dig by a river) and cooled really slowly
then, it contracted and cracks
propagated in depth. The size of the columns depends on the time the lava took to get cold. Some of the rocks of the Giant's Causeway are red (as the ones in the photo). This color comes from the alteration of the rocks because of the water or of the tropical climate which present in this era. Ice during the ice age also damaged the rocks and the columns were a little bit higher 2 millions years ago.
This spectacular landscape
owes its existence to the interactions of: - A varied geology comprising two major episodes of superimposed, Early Tertiary lava flows separated by a thick palaeosol suggestive of humid Tropical like conditions, all of which are cut through by numerous dykes. -A complex late- and postglacial history that saw ice retreat from the area, sea level rise and fall and the paraglacial adjustment of marine cliffs to create, for example, the many bays and the
extensive scree found along
the coast. -The Long-term exposure of the site to high-energy coastal conditions that worked with the underlying geology to erode and emphasise the distinctive embayed coastline and are now actively attacking the headlands they created. -A long, and ongoing history of human intervention including: stone extraction, footpath construction and road building, the construction and demolition of various buildings and the running of a high profile transport system.
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Solving the mystery of the hexagonal
column formations The secret of the formation of the Giant's Causeway was discovered by physicists at the University of Toronto.
Now they can predict the shapes
of other fracture networks such as drying mud, cracking paint or the patterns of fracture in permafrost.
They used water, corn starch,
and a heat lamp to explain the formation of hexagonal columns forming this touristic site.
This simple experience
permitted to develop the study of the cooling process of materials.
The key to understanding the
shape of the columns was to reproduce the phenomenon in a lab. You need to mix water and corn starch, then heat it all and carefully control the drying process. Corn starch crack as it dries out and forms very similar columns. Then physicists established a relationship between the size of the columns and the speed at which it cooled. They observed that the columns formed by the starch and the columns formed by lava are the same. They also found the ratio of speed, the slower the cooling process, the larger the resulting columns would be. This ratio permitted a lot of deduction about the cooling rate.