네팔과 히말라야 충돌 지대

Tectonic Setting: The Roof of the World in Motion

Nepal sits at the epicenter of the Himalayan collision zone, where the Indian Plate is driving northward into the Eurasian Plate at approximately 4 to 5 centimeters per year — a Plate CollisionThe process of two continental plates converging, creating massive mountain ranges like the Himalayas. Continental collision zones produce shallow but powerful earthquakes. that has been ongoing for approximately 50 million years and has built the highest mountain range on Earth. The collision is accommodated by the Main Himalayan Thrust (MHT), a gently dipping Fault (Geology)A fracture in rock along which movement has occurred. Faults range from millimeters to thousands of kilometers long. Major faults that produce earthquakes are called active faults. that dips northward beneath the Himalayas and represents one of the largest Convergent BoundaryA plate boundary where two plates move toward each other. Can produce subduction zones (ocean-continent), mountain building (continent-continent), or deep trenches (ocean-ocean). fault systems in the world. Occasionally, the MHT ruptures in great earthquakes that cause intense ground shaking across the narrow, heavily populated mountain valleys of Nepal, Bangladesh, northeastern India, and Bhutan.

The Himalayan Convergent BoundaryA plate boundary where two plates move toward each other. Can produce subduction zones (ocean-continent), mountain building (continent-continent), or deep trenches (ocean-ocean). differs from Pacific Subduction ZoneA region where one tectonic plate dives beneath another into the mantle. Subduction zones produce the world's largest earthquakes (M8.5+) and are associated with deep ocean trenches and volcanic arcs. settings in an important way: both colliding plates are continental crust (unlike oceanic-continental subduction), meaning neither descends cleanly into the mantle. Instead, the Indian crust underthrusts the Eurasian Plate to a degree, but the collision primarily produces mountain building through crustal thickening. The MHT is "locked" over much of its length, accumulating elastic strain at the rate of plate convergence, while the Himalayan range itself rises millimeters per year as material is added to the growing mountain pile. This Locked FaultA section of a fault where friction prevents movement, causing stress to accumulate. When a locked fault finally ruptures, it can produce a major earthquake. behavior implies periodic large earthquakes as the accumulated strain exceeds the fault's static friction.

The 2015 Gorkha Earthquake: A Modern Case Study

The April 25, 2015 Gorkha Earthquake (magnitude 7.8) ruptured approximately 150 kilometers of the MHT, generating strong shaking across central Nepal and killing approximately 8,900 people. The earthquake struck on a Saturday morning when many people were outdoors rather than inside buildings — a circumstance that probably saved many lives, since a weekday daytime earthquake would have had more people inside schools and workplaces. The MainshockThe largest earthquake in a sequence, which defines the overall magnitude of the event. Preceded by foreshocks (sometimes) and followed by aftershocks (always). was followed on May 12 by a major AftershockA smaller earthquake that follows the mainshock in the same fault region. Aftershock sequences can last weeks to years, with the largest aftershock typically 1.0-1.2 magnitudes below the mainshock. (magnitude 7.3) that killed additional hundreds of people and caused further building collapses in areas already damaged by the main event.

Kathmandu Valley, built on the sediments of a former glacial lake, experienced strong Soil Amplification (Site Effect)The increase in shaking intensity caused by soft soil or sediment layers amplifying seismic waves. Structures built on soft soil can experience 2-10 times stronger shaking than those on bedrock. that significantly increased shaking relative to surrounding rock sites. The Valley's dense concentration of Unreinforced Masonry (URM)Brick or block construction without steel reinforcement, which is extremely vulnerable to earthquake shaking. URM buildings account for the majority of earthquake fatalities worldwide. buildings — both historic temples and pagodas and more recent but still unreinforced brick construction — performed poorly, with thousands of structures collapsing or suffering major damage. The UNESCO World Heritage Site of Kathmandu Durbar Square, Patan, and Bhaktapur sustained severe damage, destroying buildings that had stood for centuries.

Historical Seismicity: The 1934 Nepal-Bihar Earthquake

The January 15, 1934 Nepal-Bihar Earthquake (estimated magnitude 8.1) was one of the largest earthquakes to strike the Himalayan region in modern times, causing widespread destruction across Nepal and northern India. The earthquake was generated by a much larger rupture of the MHT than the 2015 event, killing approximately 10,600 people in Nepal and 7,253 in Bihar, India. The city of Bhaktapur was severely damaged, and Kathmandu suffered major losses. The 1934 event has been extensively studied by PaleoseismologyThe study of prehistoric earthquakes through geological evidence such as fault trenches, uplifted terraces, and tsunami deposits. Extends the earthquake record back thousands of years. researchers attempting to understand the recurrence behavior of the MHT, and evidence suggests that an even larger earthquake — magnitude 8.5 or greater — may have struck the region in 1255.

PaleoseismologyThe study of prehistoric earthquakes through geological evidence such as fault trenches, uplifted terraces, and tsunami deposits. Extends the earthquake record back thousands of years. investigations using trenching across surface fault breaks and analysis of deformed landforms suggest that the western Nepal segment of the MHT has not ruptured in a great earthquake for several centuries, representing a significant Seismic GapA section of an active fault that has not produced an earthquake for a long time compared to neighboring sections. Seismic gaps may indicate increased probability of a future earthquake.. A rupture of this western segment could produce a magnitude 8 to 8.5 earthquake centered closer to Pokhara and western Nepal than the 2015 event, potentially causing even greater casualties given population growth since 1934.

Building Vulnerability and Reconstruction

Nepal's building stock at the time of the 2015 earthquake consisted largely of Unreinforced Masonry (URM)Brick or block construction without steel reinforcement, which is extremely vulnerable to earthquake shaking. URM buildings account for the majority of earthquake fatalities worldwide. construction — stone masonry in rural and mountainous areas, brick masonry in the Kathmandu Valley — that performed catastrophically. Rural stone houses, often with heavy stone or clay tile roofs and minimal or no mortar, collapsed readily in strong shaking, causing a disproportionate share of deaths in mountain villages distant from Kathmandu. The Building Code (Seismic)A set of legal requirements governing the design and construction of buildings to ensure minimum levels of earthquake safety. Updated after major earthquakes reveal new vulnerabilities. situation in Nepal was characterized by a formal code that had been adopted but was rarely enforced in practice, particularly in rural areas.

Post-earthquake reconstruction has attempted to introduce more earthquake-resistant techniques while respecting cultural building traditions. The Government of Nepal and international partners developed guidelines for "Build Back Better" reconstruction emphasizing confined masonry — masonry with reinforced concrete columns at corners and intersections that dramatically improves seismic performance while using familiar materials and techniques. Implementation has been uneven, and concerns persist that some reconstruction has reverted to traditional vulnerable forms, particularly in remote areas where supervision is difficult.

What Makes Nepal Unique

Nepal's earthquake challenge is defined by the intersection of extreme seismic hazard, severe poverty, and extraordinary cultural heritage. The country sits above one of the world's largest locked Fault (Geology)A fracture in rock along which movement has occurred. Faults range from millimeters to thousands of kilometers long. Major faults that produce earthquakes are called active faults. systems, with great earthquakes — magnitude 8+ — being geologically inevitable on a multi-century timescale. Nepal has essentially no margin for economic loss from such events, with a GDP per capita among the lowest in the world. The simultaneous imperative to preserve extraordinary cultural heritage (Kathmandu Valley's medieval temple complexes, mountain monasteries, traditional architecture) and to build more resistant structures creates a profound challenge that involves cultural values, economic resources, technical capacity, and governance in equal measure.