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The measured length of the fault is approximately 350 km and is the longest fault in Guatemala. Motion of the fault and others in the plate boundary have formed north–south trending grabens across the region that show evidence of counter-clockwise rotation over time. Guatemala City lies in one of these grabens, which may contribute to the ...
A map of Guatemala. Guatemala is mountainous, except for the south coastal area and the vast northern lowlands of Petén department. The country is located in Central America and bounded to the north and west by Mexico, to the east by Belize and by the Gulf of Honduras, to the east by Honduras, to the southeast by El Salvador, and to the south by the Pacific Ocean.
The Motagua Fault, which crosses through Guatemala, is a transform boundary between the southern edge of the North American plate and the northern edge of the Caribbean plate. New Zealand's Alpine Fault is another active transform boundary. The Dead Sea Transform (DST) fault which runs through the Jordan River Valley in the Middle East.
see also Chixoy-Polochic Fault: 1902-04-18 1902 Guatemala earthquake: Quetzaltenango, Guatemala City: 7.5 M w: IX 800–2,000 see also 1902 eruption of Santa María: 1914-03-08 1913 Guatemala earthquake Cuilapa: 5.0 M s: 60 Destroyed the town of Cuilapa: 1917-12-26 1917 Guatemala earthquake: Antigua Guatemala, Guatemala City: 5.6 M w: VII–IX ...
The geology of Guatemala encompasses rocks divided into two tectonic blocks. The Maya Block in the north has igneous and metamorphic North American Craton basement rocks , overlain by late Paleozoic metasedimentary rocks, which experienced deformation during the Devonian .
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The Motagua River, whose principal head stream is called the Rio Grande, has a course of about 400 kilometres (250 mi), and is navigable to within 140 km (90 mi) of Guatemala City which is situated on one of its confluents, the Rio de las Vacas. It empties in the Gulf of Honduras, an arm of the Caribbean.
Along the Motagua Fault trace (1976 Guatemala earthquake) where it crosses the Gualán soccer field. This zigzag type of fault trace is known as "mole track", which is best developed in hard-packed, brittle surface materials. The San Andreas fault trace runs along the base of the Temblor Range of mountains near Bakersfield, California. (The ...