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Earth quake in Morocco

Why is it in the news?

A rare, powerful earthquake struck Morocco recently, killing hundreds of people and damaging buildings, including in the historic city of Marrakesh.

Morocco shares its borders with the following countries and regions

  • North: Spain (with water border through the Strait of Gibraltar) and small Spanish-controlled exclaves, including Ceuta, Melilla, and PeĆ±Ć³n de VĆ©lez de la Gomera.
  • East: Algeria.
  • South: Western Sahara.
  • De facto southern boundary with Mauritania due to Morocco’s control over most of Western Sahara.

Uncommon Earthquakes in North Africa

  • Earthquakes are infrequent in North Africa, and seismicity rates are relatively low.
  • Marrakesh, including the historic old city (UNESCO World Heritage Site), experienced building collapses and structural damage.

Shallow and dangerous Earthquake

  • Magnitude of the earthquake: 6.8
  • Followed by an aftershock of magnitude 4.9 just 19 minutes later.
  • Epicentre located in the town of Ighil, approximately 70 km southwest of Marrakech.
  • Epicentre depth: 18.5 km (shallow earthquake).
  • Shallow earthquakes are more dangerous as they carry more energy than deeper ones.
  • Deeper earthquakes spread seismic waves farther but lose energy while traveling greater distances.

Causes of the Morocco Earth quake

  • While seismicity rates are indeed lower in the region, making earthquakes rarer, they are not completely unheard of.
  • According to the US Geological Survey (USGS), large destructive earthquakes have been recorded and reported from Morocco in the western Mediterranean.
    • Such quakes occur due to the ā€œnorthward convergence of the African plate with respect to the Eurasian plate along a complex plate boundary.ā€
  • With respect to current quake, the USGS attributed it to ā€œoblique-reverse faulting at shallow depth within the Moroccan High Atlas Mountain rangeā€.
  • TheĀ Atlas MountainsĀ span aboutĀ 2,300 kilometresĀ acrossĀ Morocco, AlgeriaĀ andĀ Tunisia.
    • Known asĀ fold mountains,Ā they were created by theĀ collision of tectonic masses:Ā theĀ Eurasian PlateĀ to theĀ northĀ and theĀ African PlateĀ to theĀ south.

About Fault Classification

  • A fault is a fracture or zone of fractures between two blocks of rock.
    • Faults allow the blocks to move relative to each other, causing earthquakes if the movement occurs rapidly.
    • During a quake, the rock on one side of the fault suddenly slips with respect to the other.
  • Scientists use the angle of the fault with respect to the surface (known as the dip) and the direction of the slip along the fault to classify faults.
    • Faults which move along the direction of the dip plane are dip-slip faults, whereas faults which move horizontally are known as strike-slip faults.
  • Oblique-slip faults show characteristics of both dip-slip and strike-slip faults.
  • The term ā€˜reverseā€™ refers to a situation that the upper block, above the fault plane, moves up and over the lower block. This type of faulting is common in areas of compression ā€” when one tectonic plate is converging into another.

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