Javascript must be enabled to continue!
Damage to structures and buildings from the Chi-Chi (Taiwan) earthquake
View through CrossRef
In the early morning hours of 21 September 1999, a devastating earthquake struck the central region of Taiwan. This earthquake became known as the 921 earthquake or the Chi-Chi (Taiwan) earthquake. The magnitude of the Chi-Chi (Taiwan) earthquake was Ms = 7·6 magnitude of surface wave (US Geological Survey (USGS)) or ML = 7·3 Richter magnitude (Central Weather Bureau (CWB) of Taiwan) and the main shock lasted for about 40 s. The epicentre of the earthquake was located at 120·82° east and 23·85° north near the town of Chi-Chi, Nantou County. The focal depth was 8·5 km. A surface rupture along the Chelungpu fault with a length of about 105 km was observed, with the largest measured vertical offset reaching more than 9 m. After the main shock there were over ten aftershocks with magnitudes greater than 6. The powerful thrust forces moved mountains, cut off rivers, caused liquefaction, damaged bridges, cracked highways as well as concrete dams, and toppled buildings. As a direct result of this earthquake, 2469 lives were lost, 10 002 people were injured, there were 17 484 totally/partially collapsed buildings, and an estimated property loss of US$ 10 billion. The post-quake investigations concluded that most of the collapsed buildings were designed in accordance with the Taiwan Building Codes but were constructed with serious deviations. The improper lap splices of rebars, column tie hooks without 135° bend, and poor concrete quality control at job sites have been cited as the main reasons for most of the damage to buildings.
Title: Damage to structures and buildings from the Chi-Chi (Taiwan) earthquake
Description:
In the early morning hours of 21 September 1999, a devastating earthquake struck the central region of Taiwan.
This earthquake became known as the 921 earthquake or the Chi-Chi (Taiwan) earthquake.
The magnitude of the Chi-Chi (Taiwan) earthquake was Ms = 7·6 magnitude of surface wave (US Geological Survey (USGS)) or ML = 7·3 Richter magnitude (Central Weather Bureau (CWB) of Taiwan) and the main shock lasted for about 40 s.
The epicentre of the earthquake was located at 120·82° east and 23·85° north near the town of Chi-Chi, Nantou County.
The focal depth was 8·5 km.
A surface rupture along the Chelungpu fault with a length of about 105 km was observed, with the largest measured vertical offset reaching more than 9 m.
After the main shock there were over ten aftershocks with magnitudes greater than 6.
The powerful thrust forces moved mountains, cut off rivers, caused liquefaction, damaged bridges, cracked highways as well as concrete dams, and toppled buildings.
As a direct result of this earthquake, 2469 lives were lost, 10 002 people were injured, there were 17 484 totally/partially collapsed buildings, and an estimated property loss of US$ 10 billion.
The post-quake investigations concluded that most of the collapsed buildings were designed in accordance with the Taiwan Building Codes but were constructed with serious deviations.
The improper lap splices of rebars, column tie hooks without 135° bend, and poor concrete quality control at job sites have been cited as the main reasons for most of the damage to buildings.
Related Results
Study on Earthquake Damage Distribution of Multistory Masonry Buildings
Study on Earthquake Damage Distribution of Multistory Masonry Buildings
The main components which affect the earthquake damage grades classification of multistory masonry buildings
and the damage characters are summarized and analyzed through the stati...
Comparison of 5 and 10 Storey Frame Buildings and 5 and 10 Storey Shear Wall-Frame Buildings Under the Effect of Maras Earthquake According to the Turkish Building Earthquake Code 2018
Comparison of 5 and 10 Storey Frame Buildings and 5 and 10 Storey Shear Wall-Frame Buildings Under the Effect of Maras Earthquake According to the Turkish Building Earthquake Code 2018
In this study, the differences in the displacements, base shear forces, relative storey drifts and foundation stresses under different earthquake data on different storeys of shear...
Aftershocks of the 2 April 2024 Mw 7.4 Hualin, Taiwan Earthqauke
Aftershocks of the 2 April 2024 Mw 7.4 Hualin, Taiwan Earthqauke
ABSTRACT
A devastating Mw 7.4 earthquake occurred in Taiwan on the 2 April 2024 at 23:58:11 UTC claiming 14 human lives, injuring over 1000 and causing wide spread s...
Responses of the Earthquake Engineering Research Community to the Chi-Chi (Taiwan) Earthquake
Responses of the Earthquake Engineering Research Community to the Chi-Chi (Taiwan) Earthquake
In the early morning of 21 September 1999, a devastating earthquake struck the central region of Taiwan. This earthquake became known as the “Chi-Chi” Taiwan earthquake. Immediatel...
A unified geodetic data-based earthquake catalog of Taiwan from 2006 to 2018
A unified geodetic data-based earthquake catalog of Taiwan from 2006 to 2018
A unified geodetic data-based earthquake catalog may provide the asperity information to improve the seismic hazard assessment. Therefore, we propose a unified geodetic data-based ...
Taiwan's Miracle Development: Its Economy over a Century
Taiwan's Miracle Development: Its Economy over a Century
It is well known that, since World War II, Taiwan has achieved two miracles, an “economic miracle” and a “political miracle.” Economically, after Taiwan recovered from the destruct...
US policy on Taiwan 2002–2018
US policy on Taiwan 2002–2018
The Taiwan issue has always been the most sensitive and difficult in
China – US relations. This article examines the US policy on Taiwan from 2002 to
2018 in the context of the Sin...
Analysis of maxillofacial fracture victims in the Wenchuan earthquake and Yushu earthquake
Analysis of maxillofacial fracture victims in the Wenchuan earthquake and Yushu earthquake
Abstract – Objective: To analyze retrospectively 419 patients after the Wenchuan earthquake and 46 after Yushu earthquake with maxillofacial fractures so as to provide reference o...

