UTC time | 1927-07-11 13:04:10 |
---|---|
ISC event | 909378 |
USGS-ANSS | ComCat |
Local date | July 11, 1927 |
Local time | 15:04:10 [1] |
Magnitude | 6.3 Mw [2] |
Depth | 15 km (9.3 mi) [2] |
Epicenter | 31°55′N35°38′E / 31.92°N 35.63°E |
Areas affected | Mandatory Palestine Transjordan |
Total damage | Serious damage to Jericho, Ramla, Tiberias, Nablus and Jerusalem |
Max. intensity | MSK-64 IX (Destructive) [3] [4] MMI VIII (Severe) [5] |
Casualties | 287–500 [1] [6] |
The 1927 Jericho earthquake was a devastating event that shook Mandatory Palestine and Transjordan on July 11 at 15:04 local time. The epicenter of the earthquake was in the northern area of the Dead Sea. The cities of Jerusalem, Jericho, Ramle, Tiberias, and Nablus were heavily damaged and at least 287, as many as 400 [7] , were estimated to have been killed.
Vered and Striem (1977) located the earthquake epicenter to be near the Damya Bridge in the Jordan Valley, and close to the city of Jericho. [8] Later research by Avni (1999), located the epicenter to be around 50 km south of this location near the Dead Sea. [9]
The death toll in Jerusalem included more than 130 people and around 450 were injured. About 300 houses collapsed or were severely damaged to the point of not being usable. The earthquake also caused heavy damage to the domes of the Church of the Holy Sepulchre and the al-Aqsa Mosque.
The earthquake was especially severe in Nablus where it destroyed around 300 buildings, including the Mosque of Victory and the historic parts of the Great Mosque of Nablus. [8] The death toll in Nablus included more than 150 people and around 250 were injured.
In Jericho, a number of houses collapsed, including several relatively new hotels. In one of the hotels, three female tourists from India were killed. [10] Ramla and Tiberias were also heavily damaged.
The most affected city in Transjordan was Salt in which 80 people were killed. In the rest of Transjordan another 20 people were killed.
An earthquake affected several villages in the Kerman province of Iran on February 22, 2005, at 05:55:23 local time. The shock measured 6.4 on the moment magnitude scale and had a maximum Mercalli intensity of VIII (Severe). Zarand is located 740 km southeast of Tehran. The maximum recorded peak ground acceleration was 0.51 g at Shirinrud dam. The United States' National Earthquake Information Center and the Belgian' Centre for Research on the Epidemiology of Disasters both show that 612 died and 1,411 were injured in the event.
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The 2003 San Simeon earthquake struck at 11:15 PST on December 22 on the Central Coast of California, about 7 miles (11 km) northeast of San Simeon. Probably centered in the Oceanic fault zone within the Santa Lucia Mountains, it was caused by thrust faulting and the rupture propagated southeast from the hypocenter for 12 miles (19 km).
The 1931 Nicaragua earthquake devastated Nicaragua's capital city Managua on 31 March. It had a moment magnitude of 6.1 and a maximum MSK intensity of VI (Strong). Between 1,000 and 2,450 people were killed. A major fire started and destroyed thousands of structures, burning into the next day. At least 45,000 were left homeless and losses of $35 million were recorded.
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The Galilee earthquake of 1837, often called the Safed earthquake, shook the Galilee on January 1 and is one of a number of moderate to large events that have occurred along the Dead Sea Transform (DST) fault system that marks the boundary of two tectonic plates; the African Plate on the west and the Arabian Plate on the east. Intensity assessments for the event were VIII (Damaging) on the Medvedev–Sponheuer–Karnik scale and VIII on the European Macroseismic Scale.
The 1980 El Asnam earthquake occurred on October 10 at 13:25:23 local time with a moment magnitude of 7.1 and a maximum Mercalli intensity of X (Extreme). The shock occurred in the Algerian town of El Asnam. The shocks were felt over 550 km (340 mi) away, with the initial earthquake lasting 35 seconds. It was the largest earthquake in Algeria, and was followed three hours later by a magnitude 6.2 aftershock. The earthquake created about 42 km (26 mi) of surface rupture and had a vertical slip of up to 4.2 m (14 ft). No foreshocks were recorded. The earthquake was found to have occurred very close to the epicenter of the 1954 Chlef earthquake using joint epicenter determination techniques. It occurred at a previously unknown reverse fault.
A devastating earthquake known in scientific literature as the Earthquake of 749 struck on January 18, 749, in areas of the Umayyad Caliphate, with the epicenter in Galilee. The most severely affected areas were West and East of the Jordan River. The cities of Tiberias, Beit She'an, Pella, Gadara, and Hippos were largely destroyed while many other cities across the Levant were heavily damaged. The casualties numbered in the tens of thousands.
The 2010 Papua earthquake occurred on June 16 at 12:16 local time in Papua province of Indonesia. The magnitude 7.0 mainshock was preceded by an Mw 6.2 foreshock 10 minutes earlier, and was followed 42 minutes later by an Mw 6.6 aftershock.
The 1995 Gulf of Aqaba earthquake occurred on November 22 at 06:15 local time and registered 7.3 on the Mw scale. The epicenter was located in the central segment of the Gulf of Aqaba, the narrow body of water that separates Egypt's Sinai Peninsula from the western border of Saudi Arabia. At least 8 people were killed and 30 were injured in the meizoseismal area.
The 1967 Mudurnu earthquake or more correctly, the 1967 Mudurnu Valley earthquake occurred at about 18:57 local time on 22 July near Mudurnu, Bolu Province, north-western Turkey. The magnitude 7.4 Mw earthquake was one of a series of major and intermediate quakes that have occurred in modern times along the North Anatolian Fault since 1939.
Events in the year 1927 in the British Mandate of Palestine.
The 2011 Fergana Valley earthquake affected Uzbekistan, Kyrgyzstan and Tajikistan at 01:35 KGT on 20 July. The dip-slip shock had a moment magnitude of 6.1 and a maximum Mercalli intensity of VIII (Severe). Its epicenter was located just inside Kyrgyzstan's border in the Fergana Valley region. Fourteen people were killed and eighty-six were injured in the earthquake.
The 1969 Sharm El Sheikh earthquake occurred on March 31 off the southern Sinai Peninsula in northeastern Egypt. The epicenter was located near Shadwan island, southwest of the city of Sharm El Sheikh, at the confluence of the Red Sea and the Gulf of Suez. This normal-slip shock measured 6.6 on the moment magnitude scale, had a maximum reported intensity of VII on the Mercalli intensity scale, and was responsible for several deaths and injuries.
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