Magnitude 2.6 Earthquake of Hawthorne, Nevada USA 2013 October 17

2013-10-17 02:16:03 UTC: Hawthorne, Nevada USA EARTHQUAKE

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Magnitude: 2.6

Event Time: Time and Date Starting of Earthquake Rupture 

1. 2013-10-17 02:16:03 UTC

1. 2013-10-16 19:16:03 UTC-07:00 at epicenter

Earthquake data:

Location : Position of Epicenter 

38.415°N 118.744°W

Depth : Depth of starting Rupture 

2.3km (1.4mi)

Region : Hawthorne, Nevada

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

a) 16km (10mi) SW of Hawthorne, Nevada

b) 101km (63mi) ESE of Gardnerville Ranchos, Nevada

c) 121km (75mi) SE of Carson City, Nevada

d) 122km (76mi) ESE of South Lake Tahoe, California

e) 139km (86mi) SSE of Fernley, Nevada

Location Uncertainty: 

Parameter	Value	Uncertainty
Magnitude	2.6 ml	--
Location	38.415°N, 118.744°W	± 1.7 km
Depth	2.3 km	± 3.4 km
Number of Phase Applied1	19
Minimum Distance2	5.1 km (0.05°)
Travel Time Residual3	0.2188 sec
Azimuthal Gap4	111°

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 5.3 Earthquake of Maribojoc, Philippines 2013 October 16

2013-10-16 23:37:33 UTC: Maribojoc, Philippines EARTHQUAKE

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Magnitude: 5.3

Event Time: Time and Date Starting of Earthquake Rupture 

1. 2013-10-16 23:37:33 UTC

1. 2013-10-17 07:37:33 UTC+08:00 at epicenter

Earthquake data:

Location : Position of Epicenter 

9.762°N 123.859°E

Depth : Depth of starting Rupture 

35.2km (21.9mi)

Region : Maribojoc, Philippines

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

a) 2km (1mi) NE of Maribojoc, Philippines

b) 12km (7mi) N of Tagbilaran, Philippines

c) 23km (14mi) NNE of Danao, Philippines

d) 23km (14mi) SSW of Tibigan, Philippines

e) 620km (385mi) SSE of Manila, Philippines

Location Uncertainty: 

Parameter	Value	Uncertainty
Magnitude	5.3 mb	± 0.07
Location	9.762°N, 123.859°E	--
Depth	35.2 km	± 5.6 km
Number of Phase Applied1	77
Minimum Distance2	352.9 km (3.17°)
Travel Time Residual3	1.08 sec
Azimuthal Gap4	117°

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 2.7 Earthquake of Soledad, California USA 2013 October 17

2013-10-17 00:53:45 UTC: Soledad, California USA EARTHQUAKE

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Magnitude: 2.7

Event Time: Time and Date Starting of Earthquake Rupture 

1. 2013-10-17 00:53:45 UTC

1. 2013-10-16 17:53:45 UTC-07:00 at epicenter

Earthquake data:

Location : Position of Epicenter 

36.622°N 121.161°W

Depth : Depth of starting Rupture 

8.0km (5.0mi)

Region : Soledad, California

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

a) 26km (16mi) NE of Soledad, California

b) 33km (21mi) SE of Hollister, California

c) 34km (21mi) NNE of Greenfield, California

d) 44km (27mi) E of Salinas, California

e) 219km (136mi) S of Sacramento, California

Location Uncertainty: 

Parameter	Value	Uncertainty
Magnitude	2.7 Md	± 0.10
Location	36.622°N, 121.161°W	± 0.2 km
Depth	8.0 km	± 0.5 km
Number of Phase Applied1	55
Minimum Distance2	5.0 km (0.04°)
Travel Time Residual3	0.13 sec
Azimuthal Gap4	43°

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 3.4 Earthquake of Ferndale, California USA 2013 October 15

2013-10-15 06:48:51 UTC: Ferndale, California USA EARTHQUAKE

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Magnitude: 3.4

Event Time: Time and Date Starting of Earthquake Rupture 

1. 2013-10-15 06:48:51 UTC

1. 2013-10-14 22:48:51 UTC-08:00 at epicenter

Earthquake data:

Location : Position of Epicenter 

40.370°N 125.426°W

Depth : Depth of starting Rupture 

2.5km (1.6mi)

Region : Ferndale, California

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

a) 101km (63mi) WSW of Ferndale, California

b) 110km (68mi) WSW of Fortuna, California

c) 117km (73mi) WSW of Eureka, California

d) 126km (78mi) WSW of Arcata, California

e) 392km (244mi) WNW of Sacramento, California

Location Uncertainty: 

Parameter	Value	Uncertainty
Magnitude	3.4 Ml	± 0.10
Location	40.370°N, 125.426°W	± 6.0 km
Depth	2.5 km	± 42.1 km
Number of Phase Applied1	52
Minimum Distance2	99.0 km (0.89°)
Travel Time Residual3	0.5 sec
Azimuthal Gap4	270°

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 Iwaki, Japan 2013 October 15

2013-10-15 05:58:43 UTC: Iwaki, Japan EARTHQUAKE

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Magnitude: 4.8

Event Time: Time and Date Starting of Earthquake Rupture 

1. 2013-10-15 05:58:43 UTC

1. 2013-10-15 14:58:43 UTC+09:00 at epicenter

Earthquake data:

Location : Position of Epicenter 

37.106°N 141.642°E

Depth : Depth of starting Rupture 

30.9km (19.2mi)

Region : Iwaki, Japan

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

a) 67km (42mi) E of Iwaki, Japan

b) 70km (43mi) SE of Namie, Japan

c) 87km (54mi) ENE of Kitaibaraki, Japan

d) 93km (58mi) ENE of Takahagi, Japan

e) 235km (146mi) NE of Tokyo, Japan

Location Uncertainty: 

Parameter	Value	Uncertainty
Magnitude	4.8 mb	± 0.09
Location	37.106°N, 141.642°E	--
Depth	30.9 km	± 6.3 km
Number of Phase Applied1	52
Minimum Distance2	312.9 km (2.81°)
Travel Time Residual3	0.90 sec
Azimuthal Gap4	167°

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)