Wednesday, October 29, 2014

Magnitude 4.6 Earthquake of Enarotali, Indonesia 2014-10-29

2014-10-29 11:12:34 UTC : Enarotali, Indonesia EARTHQUAKE

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Magnitude: 4.6


Event Time: Time and Date Starting of Earthquake Rupture 


  1. 2014-10-29 11:12:34 UTC
  2. 2014-10-29 20:12:34 UTC+09:00 at epicenter

    Earthquake data:

    Location : Position of Epicenter 


    1. 3.678°S 138.264°E

    Depth : Depth of starting Rupture

    63.0km (39.1mi)


    Region : Enarotali, Indonesia

    Magnitude 4.6 Earthquake of Enarotali, Indonesia 2014-10-29

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

    a) 214km (133mi) E of Enarotali, Indonesia

    b) 282km (175mi) WSW of Abepura, Indonesia

    c)  298km (185mi) WSW of Jayapura, Indonesia

    d) 
    310km (193mi) E of Nabire, Indonesia


    e)  1173km (729mi) WNW of Port Moresby, Papua New Guinea

    Location Uncertainty: 
    Parameter
    Value
    Uncertainty
    Magnitude
    4.6 mb
    ± 0.09
    Location
    3.678°S, 138.265°E
    --
    Depth
    63.0 km
    ± 5.8 km
    Number of Phase Applied1
    45

    Minimum Distance2
    673.7 km (6.05°)

    Travel Time Residual3
    1.01 sec

    Azimuthal Gap4
    64°

    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 3.6 Earthquake of The Geysers, California 2014-10-29

    2014-10-29 04:36:35 UTC :The Geysers, California EARTHQUAKE

    earthquake monitor,California earthquake, earthquake realtime

    Magnitude : 3.6


    Event Time: Time and Date Starting of Earthquake Rupture 

    1. 2014-10-29 04:36:35 UTC
    2. 2014-10-28 21:36:35 UTC-07:00 at epicenter

    Earthquake data:

    Location : Position of Epicenter 


    1. 38.801°N 122.770°W

    Depth : Depth of starting Rupture 

    1.9km (1.2mi)


    Region :The Geysers, California



    Magnitude 3.6 Earthquake of The Geysers, California 2014-10-29




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

    a)  2km (1mi) NNW of The Geysers, California

    b)  21km (13mi) SW of Clearlake, California

    c)  22km (14mi) NNE of Healdsburg, California

    d)  
    28km (17mi) N of Windsor, California


    e)  113km (70mi) WNW of Sacramento, California

    Location Uncertainty: 
    Parameter
    Value
    Uncertainty
    Magnitude
    3.6 mw
    ± 0.10
    Location
    38.801°N, 122.770°W
    ± 0.1 km
    Depth
    1.9 km
    ± 0.2 km
    Number of Phase Applied1
    64

    Minimum Distance2
    1.6 km (0.01°)

    Travel Time Residual3
    0.06 sec

    Azimuthal Gap4
    23°

    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 4.4 Earthquake of Bitung, Indonesia 2014-10-28

    2014-10-28 23:06:45 UTC : Bitung, Indonesia EARTHQUAKE

    earthquake monitor,Indonesia earthquake, earthquake realtime

    Magnitude: 4.4


    Event Time: Time and Date Starting of Earthquake Rupture 

    1. 2014-10-28 23:06:45 UTC
    2. 2014-10-29 07:06:45 UTC+08:00 at epicenter

      Earthquake data:

      Location : Position of Epicenter 

      1. 2.636°N 125.524°E

      Depth : Depth of starting Rupture

      163.8km (101.8mi)


      Region : Bitung, Indonesia

      Magnitude 4.4 Earthquake of Bitung, Indonesia 2014-10-28

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

      a) 137km (85mi) NNE of Bitung, Indonesia

      b) 147km (91mi) NNE of Manado, Indonesia

      c)  162km (101mi) NNE of Tondano, Indonesia

      d) 
      162km (101mi) NNE of Tomohon, Indonesia


      e)  1120km (696mi) WSW of Koror Town, Palau

      Location Uncertainty: 
      Parameter
      Value
      Uncertainty
      Magnitude
      4.4 mb
      ± 0.22
      Location
      2.636°N, 125.524°E
      --
      Depth
      163.8 km
      ± 10.9 km
      Number of Phase Applied1
      21

      Minimum Distance2
      290.8 km (2.61°)

      Travel Time Residual3
      1.32 sec

      Azimuthal Gap4
      134°

      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 4.6 Earthquake of Chichi-shima, Japan 2014-10-28

      2014-10-28 22:50:34 UTC :Chichi-shima, Japan EARTHQUAKE

      earthquake monitor,Japan earthquake, earthquake realtime

      Magnitude : 4.6


      Event Time: Time and Date Starting of Earthquake Rupture 


      1. 2014-10-28 22:50:34 UTC
      2. 2014-10-29 07:50:34 UTC+09:00 at epicenter

      Earthquake data:

      Location : Position of Epicenter 

      27.186°N 140.280°E

      Depth : Depth of starting Rupture 

      471.9km (293.3mi)


      Region : Chichi-shima, Japan


      Magnitude 4.6 Earthquake of Chichi-shima, Japan 2014-09-28




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

      a) 192km (119mi) W of Chichi-shima, Japan

      b) 834km (518mi) SSE of Shingu, Japan

      c) 839km (521mi) S of Shimoda, Japan

      d) 845km (525mi) SSE of Oyama, Japan


      e) 944km (587mi) S of Tokyo, Japan

      Location Uncertainty: 
      Parameter
      Value
      Uncertainty
      Magnitude
      4.6 mb
      ± 0.04
      Location
      27.186°N, 140.280°E
      --
      Depth
      472.0 km
      ± 7.6 km
      Number of Phase Applied1
      116

      Minimum Distance2
      189.1 km (1.70°)

      Travel Time Residual3
      0.64 sec

      Azimuthal Gap4
      57°

      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 2.6 Earthquake of Anthony, Kansas 2014-10-28

      2014-10-28 11:10:35 UTC : Anthony, Kansas EARTHQUAKE

      earthquake monitor,Kansas earthquake, earthquake realtime

      Magnitude: 2.6


      Event Time: Time and Date Starting of Earthquake Rupture 


      1. 2014-10-28 11:10:35 UTC
      2. 2014-10-28 06:10:35 UTC-05:00 at epicenter

      Location : Position of Epicenter 

      37.041°N 97.930°W

      Depth : Depth of starting Rupture 

      5.0km (3.1mi)


      Region : Anthony, Kansas


      Magnitude 2.6 Earthquake of Anthony, Kansas 2014-10-28




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

      a)  15km (9mi) SE of Anthony, Kansas

      b)  71km (44mi) N of Enid, Oklahoma

      c)  77km (48mi) SW of Haysville, Kansas

      d)  
      79km (49mi) W of Arkansas City, Kansas


      e)  178km (111mi) NNW of Oklahoma City, Oklahoma

      Location Uncertainty: 
      Parameter
      Value
      Uncertainty
      Magnitude
      2.6 mb_lg
      ± 0.11
      Location
      37.041°N, 97.930°W
      --
      Depth
      5.0 km
      ± 2.0 km
      Number of Phase Applied1
      41

      Minimum Distance2
      9.1 km (0.08°)

      Travel Time Residual3
      0.55 sec

      Azimuthal Gap4
      39°

      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)

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