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Distance on a map of Barcelona – Guatemala

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Distance on a map of Barcelona – Guatemala

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Web of information: Vuelos a Ciudad de Guatemala.

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Quaternary volcanism in Northern Central America occurs along a WNW-trending belt consisting of a linear chain of relatively small volume, basalt-andesite composite volcanoes spaced at an average interval of 28 km (Stoiber and Carr, 1974). In 1922, after 20 years of relative quiet, lava extrusion began in the center of the 1902 crater

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The area is also active in terms of earthquakes, which have been suffered some many damages due to this phenomena, for instance we can refer the earthquakes happened in 1863, 1902 and 1942, all of them produced major damages to the buildings in Retalhuleu

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2 escales

06:25 – 08:05         1 h 40 min

Barcelona (BCN) - Zúrich (ZRH)

Swiss 1951 · Airbus A321

Distance: 836 km

Escala en Zúrich ZRH         1 h 55 min

10:00 – 13:05           9 h 05 min

Zúrich (ZRH) - Newark (EWR)

United 135 · Boeing 767

Distance: 6339 kilometers

Escala en Newark EWR    5 h 14 min

18:19 – 21:25           5 h 06 min

Newark (EWR) - Ciudad de Guatemala (GUA)

United 1207 · Boeing 737

Distance: 3,305.76 km

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by destroying bridges and key roads, lahars can also trap people in areas vulnerable to other hazardous volcanic activi

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Velocity

Bercelona – Zurich
V = D / T    V = 836 / 100 = 8,36 km/h

Zurich - Newark
V = D / T    V = 6339 / 545 = 11, 631 km/h

Newark – Cuidad de Guatemala
V = D / T    V = 3,305.76 / 314 = 10, 528 km/h

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The direct impact of a lahar's turbulent flow front or from the boulders and logs carried by the laharscan easily crush, abrade, or shear off at ground level just about anything in the path of a lahars. Evenif not crushed or carried away by the force of lahars, buildings and valuable land may become partiallyor completely buried by one or more cement-like layers of debris as happened in El Palmartown during 1984 

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The direct impact of a lahar's turbulent flow front or from the boulders and logs carried by the laharscan easily crush, abrade, or shear off at ground level just about anything in the path of a lahars. Evenif not crushed or carried away by the force of lahars, buildings and valuable land may become partiallyor completely buried by one or more cement-like layers of debris as happened in El Palmartown during 1984 

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After a volcanic eruption, the erosion of new loose volcanic deposits in the headwaters of rivers can lead to severe flooding and extremely high rates of sedimentation in the lowest part of the catchment areas downstream of the volcano. Lahars and high-sediment discharge triggered by intense rainfall deposit debris that buried entire towns and valuable agricultural land. Such lahar deposits may also block tributary stream valleys

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Lahars move downslope from the Santiaguito volcano through the Nima I, Nima II and El Tambor river valleys and spread across Samala flood plains around twenty kilometers downstream from the volcano. Volcanic eruptions, earthquakes, precipitation, also trigger mass movement.