Magnitude 4.7 Earthquake of Firuzabad, Iran 2015-04-10

2015-04-10 06:23:13 (UTC) :SouthWest of Firuzabad, Iran

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Magnitude : 4.7

Event Time: Time and Date Starting of Earthquake Rupture 

• 2015-04-10 06:23:13 (UTC)

Earthquake data:

Location : Position of Epicenter 

28.243°N 51.844°E

Depth : Depth of starting Rupture 

10.0 km

Region : Firuzabad, Iran

Directions and Distances :Directions and Distances from Geographical Reference in Close Proximity Which can be effected by Location Uncertainty

a) 97km (60mi) SW of Firuzabad, Iran

b) 127km (79mi) SE of Bandar Bushehr, Iran

c) 128km (80mi) SSE of Borazjan, Iran

d) 143km (89mi) SW of Akbarabad, Iran

e) 257km (160mi) NNE of Manama, Bahrain

Location Uncertainty: 

Parameter	Value	Uncertainty
Magnitude	4.7 mb	± 0.1
Location	28.243°N 51.844°E	± 4.8 km
Depth	10.0 km	± 1.8
Number of Phase Applied1	50
Minimum Distance2	567.84 km (5.10°)
Travel Time Residual3	1.23 sec
Azimuthal Gap4	46°

¹Number of phase Applied: 

In determining location of hypocenter, applied number of observations on P waves and S waves. The greater the more accurate prediction of EQ.

²Minimum Distance:

 Horizontal distance of nearest Station measured in Km from epicenter. The smaller the more accuracy in prediction of depth of EQ.

³Travel Time Residual:

 A way of measurement of fit of arrival time observed to arrival time predicted for particular location. The smaller the better fit of data.

⁴Azimuthal Gap: 

Expressed in degree; the smaller the smaller the error in horizontal positioning of EQ. Large uncertainty is considered when exceeds 180° (both depth and location)

Magnitude 4.5 Earthquake of Dehloran, Iran 2014-08-28

2014-08-28 00:00:45 UTC :Dehloran, Iran EARTHQUAKE

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Magnitude: 4.5

Event Time: Time and Date Starting of Earthquake Rupture 

1. 2014-09-28 00:00:45 UTC

1. 2014-09-28 03:30:45 UTC+03:30 at epicenter

Earthquake data:

Location : Position of Epicenter 

32.641°N 47.553°E

Depth : Depth of starting Rupture 

44.1km (27.4mi)

Region : Dehloran, Iran

Directions and Distances :Directions and Distances from Geographical Reference in Close Proximity Which can be effected by Location Uncertainty

a)  27km (17mi) ESE of Dehloran, Iran

b)  40km (25mi) SSE of Abdanan, Iran

c)  81km (50mi) NW of Shush, Iran

d)  83km (52mi) ENE of `Ali al Gharbi, Iraq

e)  304km (189mi) ESE of Baghdad, Iraq

Location Uncertainty: 

Parameter	Value	Uncertainty
Magnitude	4.5 mb	± 0.07
Location	32.641°N, 47.553°E	--
Depth	44.1 km	± 8.6 km
Number of Phase Applied1	75
Minimum Distance2	750.4 km (6.74°)
Travel Time Residual3	0.83 sec
Azimuthal Gap4	66°

¹Number of phase Applied: 

In determining location of hypocenter, applied number of observations on P waves and S waves. The greater the more accurate prediction of EQ.

²Minimum Distance:

 Horizontal distance of nearest Station measured in Km from epicenter. The smaller the more accuracy in prediction of depth of EQ.

³Travel Time Residual:

 A way of measurement of fit of arrival time observed to arrival time predicted for particular location. The smaller the better fit of data.

⁴Azimuthal Gap: 

Expressed in degree; the smaller the smaller the error in horizontal positioning of EQ. Large uncertainty is considered when exceeds 180° (both depth and location)

Magnitude 4.5 Earthquake of Shahrud, Iran 2014-09-06

2014-09-06 21:34:20 UTC : Shahrud, Iran EARTHQUAKE

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Magnitude: 4.5

Event Time: Time and Date Starting of Earthquake Rupture 

1. 2014-09-06 21:34:20 UTC

1. 2014-09-07 02:04:20 UTC+04:30 at epicenter

Earthquake data:

Location : Position of Epicenter 

36.693°N 54.883°E

Depth : Depth of starting Rupture 

10.0km (6.2mi)

Region : Shahrud, Iran

Directions and Distances :Directions and Distances from Geographical Reference in Close Proximity Which can be effected by Location Uncertainty

a)  31km (19mi) NNW of Shahrud, Iran

b)  43km (27mi) ESE of Gorgan, Iran

c)  50km (31mi) SSW of Shah Pasand, Iran

d)  66km (41mi) SSW of Gonbad-e Qabus, Iran

e)  330km (205mi) ENE of Tehran, Iran

Location Uncertainty: 

Parameter	Value	Uncertainty
Magnitude	4.5 mb	± 0.06
Location	36.693°N, 54.883°E	--
Depth	10.0 km	± 1.9 km
Number of Phase Applied1	129
Minimum Distance2	318.1 km (2.86°)
Travel Time Residual3	1.28 sec
Azimuthal Gap4	52°

¹Number of phase Applied: 

In determining location of hypocenter, applied number of observations on P waves and S waves. The greater the more accurate prediction of EQ.

²Minimum Distance:

 Horizontal distance of nearest Station measured in Km from epicenter. The smaller the more accuracy in prediction of depth of EQ.

³Travel Time Residual:

 A way of measurement of fit of arrival time observed to arrival time predicted for particular location. The smaller the better fit of data.

⁴Azimuthal Gap: 

Expressed in degree; the smaller the smaller the error in horizontal positioning of EQ. Large uncertainty is considered when exceeds 180° (both depth and location)

Magnitude 4.3 Earthquake of Shiraz, Iran 2014-09-04

2014-09-04 23:51:23 UTC :Shiraz, Iran EARTHQUAKE

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Magnitude: 4.3

Event Time: Time and Date Starting of Earthquake Rupture 

1. 2014-09-04 23:51:23 UTC

1. 2014-09-05 04:21:23 UTC+04:30 at epicenter

Earthquake data:

Location : Position of Epicenter 

29.495°N 52.184°E

Depth : Depth of starting Rupture 

23.6km (14.7mi)

Region : Shiraz, Iran

Directions and Distances :Directions and Distances from Geographical Reference in Close Proximity Which can be effected by Location Uncertainty

a)  36km (22mi) WSW of Shiraz, Iran

b)  53km (33mi) ESE of Kazerun, Iran

c)  64km (40mi) WNW of Akbarabad, Iran

d)  81km (50mi) NNW of Firuzabad, Iran

e)  396km (246mi) NNE of Manama, Bahrain

Location Uncertainty: 

Parameter	Value	Uncertainty
Magnitude	4.3 mb	± 0.08
Location	29.495°N, 52.184°E	--
Depth	23.7 km	± 4.7 km
Number of Phase Applied1	65
Minimum Distance2	642.6 km (5.77°)
Travel Time Residual3	1.05 sec
Azimuthal Gap4	121°

¹Number of phase Applied: 

In determining location of hypocenter, applied number of observations on P waves and S waves. The greater the more accurate prediction of EQ.

²Minimum Distance:

 Horizontal distance of nearest Station measured in Km from epicenter. The smaller the more accuracy in prediction of depth of EQ.

³Travel Time Residual:

 A way of measurement of fit of arrival time observed to arrival time predicted for particular location. The smaller the better fit of data.

⁴Azimuthal Gap: 

Expressed in degree; the smaller the smaller the error in horizontal positioning of EQ. Large uncertainty is considered when exceeds 180° (both depth and location)

Magnitude 4.8 Earthquake of Dehloran, Iran 2014-08-25

2014-08-25 06:01:36 UTC :Dehloran, Iran EARTHQUAKE

earthquake monitor, Iran earthquake, earthquake realtime

Magnitude: 4.8

Event Time: Time and Date Starting of Earthquake Rupture 

1. 2014-08-25 06:01:36 UTC

1. 2014-08-25 10:31:36 UTC+04:30 at epicenter

Earthquake data:

Location : Position of Epicenter 

32.586°N 47.783°E

Depth : Depth of starting Rupture 

10.0km (6.2mi)

Region : Dehloran, Iran

Directions and Distances :Directions and Distances from Geographical Reference in Close Proximity Which can be effected by Location Uncertainty

a) 49km (30mi) ESE of Dehloran, Iran

b) 56km (35mi) SE of Abdanan, Iran

c)  61km (38mi) NW of Shush, Iran

d) 62km (39mi) WNW of Dezful, Iran

e)  327km (203mi) ESE of Baghdad, Iraq

Location Uncertainty: 

Parameter	Value	Uncertainty
Magnitude	4.8 mb	± 0.08
Location	32.586°N, 47.783°E	--
Depth	10.0 km	± 1.9 km
Number of Phase Applied1	52
Minimum Distance2	767.1 km (6.89°)
Travel Time Residual3	1.11 sec
Azimuthal Gap4	123°

¹Number of phase Applied: 

In determining location of hypocenter, applied number of observations on P waves and S waves. The greater the more accurate prediction of EQ.

²Minimum Distance:

 Horizontal distance of nearest Station measured in Km from epicenter. The smaller the more accuracy in prediction of depth of EQ.

³Travel Time Residual:

 A way of measurement of fit of arrival time observed to arrival time predicted for particular location. The smaller the better fit of data.

⁴Azimuthal Gap: 

Expressed in degree; the smaller the smaller the error in horizontal positioning of EQ. Large uncertainty is considered when exceeds 180° (both depth and location)