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Agiofarango Gorge EarthCache

Hidden : 10/22/2009
Difficulty:
1.5 out of 5
Terrain:
2.5 out of 5

Size: Size:   not chosen (not chosen)

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Geocache Description:

In Agiofarango with a trail thru a Gorge on Crete

Description / Geology

The same geological forces that have created the mountain ranges of Crete also created a large number of truly remarkable gorges throughout the island.

The geological composition of the island and centuries of seismic activity have caused it to be literally honeycombed with an estimated 3,500 caves, many of which are of extreme archaeological and religious significance. In the past and even more recently, caves were used by Cretans as places of refuge, cult sites and centres of resistance to invaders. There are believed to be over one hundred churches in caves around the island. According to legend, the Dikteon Andron on the Lassithi plateau was the birthplace of Zeus, the supreme deity who later grew up in the Ideon Andron on Mount Psiloritis.

The Agiofarango Gorge is situated in the south of Odighitria Monastery and was formed by two streams, one of them begins in the north-northeast at Ghialomonochoro, and the other in the northeast, at Odighitria. The two streams meet near Aghia Kiriaki Church and end up at Porofarango, which marks the beginning of the Agiofarango Gorge, which in turn leads to the Libyan Sea. A small enchanting beach frames the gorge's debouch.

Many visitors to the Cretan gorges are wondering how these gorges were formed. Since the late Miocene period, 5 to 10 million years ago, the intense uplift of the whole Cretan area, due to plate tectonics, accelerated karstic weathering, forming these many gorges and caves and plateaus.

The gorges are formed mainly in carbonate rocks, i.e. limestone and marble, as a result of continuous land uplift and erosion by water of the rivers. The land uplift is usually caused by faults, or 'cracks in the earth':

Early stage: Coastal limestone planes crossed by a river, which brings rain water and melted snow down from the mountains:

Middle stage: The fault or crack is breaking, due to geological uplift and pressure. A gorge is beginning to be formed. The river in its bed causes immense erosion:

Final stage: Immense erosion by the river and rising of the stone floor continues, widening the gorge. This can be seen at most of the gorges in Crete now, like at Samaria and Imbros gorge. Sometimes a wide coastal plane is formed, like in Frangokastello, Sfakia:


Tasks to do

As usual for an EarthCache there is no logbook at the coordinates! To log this cache, please follow the trail and answer the following questions, with help of the signs along the way.

You need no Internet to solve the Questions.

1.) How high is the open conical dome inside the Ghoumenospilio Cave?
2.) What is the meaning of the name Agiofarango in english?
3.) Make a picture of you with your GPS on the following coordinates N34 55.780 E024 46.747

The Answers you will need as a prefix for the E-Mail Address. Example: if the height is 14m and the name would be "Gorge of Geocacher" the E-Mail Address would be: 14_gorgeofgeocacher(at)geo-cacher.com

Send your answers to following E-Mail-address: (answer...)(at)geo-cacher.com
If your answer is right, you’ll get the log permission automatically per E-Mail. Please do not log without the permission otherwise I will delete your log.

Additional Hints (No hints available.)