
The format of the return is International Monitoring System 1.0 (IMS1.0), a standard that was developed for exchanging data used to monitor the Comprehensive Test Ban Treaty. A 2.8 MB PDF document that includes a description of the format can be downloaded from the Prototype International Data Centre. IMS1.0 is very similar to GSE2.1. Documentation for GSE2.1 is available in a variety of formats from the Swiss Seismological Service's AutoDRM documentation page.
The format used for moment tensors is part of the draft IASPEI Seismic Format (ISF). ISF is an extension of IMS1.0 being developed by the IASPEI Commission on Practice. This document is in PDF form and can be downloaded from the ISC.
A brief description of the format of the relevant data returned by the ISC search, as extracted from the IMS1.0 documentation is given in the following sections:

Bulletins are composed of origin and arrival information. The information is pro-vided in a series of data blocks as shown in Table 38: bulletin title block (Table 39), event title block (Table 40), origin block (Table 41), phase block (Table 42), phase correction block (under development), event screening block (Table 43), and event characterization arrival block (Table 44). The verbosity of a bulletin can be controlled by specifying the subformat, which can be short or long. The default is short. The BULL_TYPE environment and the subformat control the blocks of information that appear in a bulletin. Table 38 lists the blocks that are included for each BULL_TYPE and subformat. A BULLETIN data message contains one bulletin title block and one set of the other block types for each event. The blocks in a BULLETIN data message appear in the order given in Table 38. Examples of the short and long subformats for bulletins are provided in Bulletin (IMS1.0:short Format) on page A16 and Bul-letin (IMS1.0:long Format) on page A16.
| Record | Position | Format | Description |
|---|---|---|---|
| 1 | 1-136 | a136 | bulletin title |

| Record | Position | Format | Description |
|---|---|---|---|
| 1 | 1-5 | a5 | Event |
| 7-14 | a8 | event identification number | |
| 16-80 | a65 | geographic region |

| Record | Position | Format | Description |
|---|---|---|---|
| Origin Sub-block | |||
| 1 | 4-7 | a4 | Date |
| (header) | 15-18 | a4 | Time |
| 27-29 | a3 | Err | |
| 33-35 | a3 | RMS | |
| 37-44 | a8 | Latitude | |
| 46-54 | a9 | Longitude | |
| 57-60 | a4 | Smaj | |
| 63-66 | a4 | Smin | |
| 69-70 | a2 | Az | |
| 72-76 | a5 | Depth | |
| 80-82 | a3 | Err | |
| 84-87 | a4 | Ndef | |
| 89-92 | a4 | Nst | |
| 94-96 | a3 | Gap | |
| 99-103 | a5 | mdist | |
| 106-110 | a5 | Mdist | |
| 112-115 | a4 | Qual | |
| 19-124 | a6 | Author | |
| 131-136 | a6 | OrigID |
| Record | Position | Format | Description |
|---|---|---|---|
| 1-10 | i4,a1,i2,a1,i2 | epicenter date (yyyy/mm/dd) | |
| 12-22 | i2,a1,i2,a1,f5.2 | epicenter time (hh:mm:ss.ss) | |
| 23 | a1 | fixed flag (f = fixed origin time solution, blank if not a fixed origin time) | |
| 25-29 | f5.2 | origin time error (seconds; blank if fixed origin time) | |
| 31-35 | f5.2 | root mean square of time residuals (seconds) | |
| 37-44 | f8.4 | latitude (negative for South) | |
| 46-54 | f9.4 | longitude (negative for West) | |
| 55 | a1 | fixed flag (f = fixed epicenter solution, blank if not a fixed epicenter solution) | |
| 56-60 | f5.1 | semi-major axis of 90% ellipse or its estimate (km, blank if fixed epicenter) | |
| 62-66 | f5.1 | semi-minor axis of 90% ellipse or its estimate (km, blank if fixed epicenter) | |
| 68-70 | i3 | strike (0 <= x <= 360) of error ellipse clock-wise from North (degrees) | |
| 72-76 | f5.1 | depth (km) | |
| 77 | a1 | fixed flag (f = fixed depth station, d = depth phases, blank if not a fixed depth) | |
| 79-82 | f4.1 | depth error 90% (km; blank if fixed depth) | |
| 84-87 | i4 | number of defining phases | |
| 89-92 | i4 | number of defining stations | |
| 94-96 | i3 | gap in azimuth coverage (degrees) | |
| 98-103 | f6.2 | distance to closest station (degrees) | |
| 105-110 | f6.2 | distance to furthest station (degrees) | |
| 112 | a1 | analysis type: (a = automatic, m = manual, g = guess) | |
| 114 | a1 | location method: (i = inversion, p = pattern recognition, g = ground truth, o = other) | |
| 116-117 | a2 | event type: | |
| uk = unknown | |||
| de = damaging earthquake ( Not standard IMS ) | |||
| fe = felt earthquake ( Not standard IMS ) | |||
| ke = known earthquake | |||
| se = suspected earthquake | |||
| kr = known rockburst | |||
| sr = suspected rockburst | |||
| ki = known induced event | |||
| si = suspected induced event | |||
| km = known mine expl. | |||
| sm = suspected mine expl. | |||
| kh = known chemical expl. ( Not standard IMS ) | |||
| sh = suspected chemical expl. ( Not standard IMS ) | |||
| kx = known experimental expl. | |||
| sx = suspected experimental expl. | |||
| kn = known nuclear expl. | |||
| sn = suspected nuclear explosion | |||
| ls = landslide | |||
| 119-127 | a9 | author of the origin | |
| 129-136 | a8 | origin identification |
| Record | Position | Format | Description |
|---|---|---|---|
| Comment Sub-block | |||
| 1 | 2 | a1 | ( |
| 3-M | a(M-2) | comment | |
| M+1 | a1 | ) |

| Record | Position | Format | Description |
|---|---|---|---|
| 1 | 1-3 | a3 | Sta |
| (header) | 9-12 | a4 | Dist |
| 15-18 | a4 | EvAz | |
| 20-24 | a5 | Phase | |
| 33-36 | a4 | Time | |
| 43-46 | a4 | TRes | |
| 49-52 | a4 | Azim | |
| 54-58 | a5 | AzRes | |
| 62-65 | a4 | Slow | |
| 69-72 | a4 | SRes | |
| 74-76 | a3 | Def | |
| 80-82 | a3 | SNR | |
| 90-92 | a3 | Amp | |
| 96-98 | a3 | Per | |
| 100-103 | a4 | Qual | |
| 105-113 | a9 | Magnitude | |
| 118-122 | a5 | ArrID |
| Record | Position | Format | Description |
|---|---|---|---|
| 2-n | 1-5 | a5 | station code |
| (data) | 7-12 | f6.2 | station-to-event distance (degrees) |
| 14-18 | f5.1 | event-to-station azimuth (degrees) | |
| 20-27 | a8 | phase code | |
| 29-40 | i2,a1,i2,a1,f6.3 | arrival time (hh:mm:ss.sss) | |
| 42-46 | f5.1 | time residual (seconds) | |
| 48-52 | f5.1 | observed azimuth (degrees) | |
| 54-58 | f5.1 | azimuth residual (degrees) | |
| 60-65 | f5.1 | observed slowness (seconds/degree) | |
| 67-72 | f5.1 | slowness residual (seconds/degree) | |
| 74 | a1 | time defining flag (T or _) | |
| 75 | a1 | azimuth defining flag (A or _) | |
| 76 | a1 | slowness defining flag (S or _) | |
| 78-82 | f5.1 | signal-to-noise ratio | |
| 84-92 | f9.1 | amplitude (nanometers) | |
| 94-98 | f5.2 | period (seconds) | |
| 100 | a1 | type of pick (a = automatic, m = manual) | |
| 101 | a1 | direction of short period motion (c = compression, d = dilatation, _= null) | |
| 102 | a1 | onset quality (i = impulsive, e = emergent, q = questionable, _ = null) | |
| 104-108 | a5 | magnitude type (mb, Ms, ML, mbmle, msmle) | |
| 109 | a1 | min max indicator (<, >, or blank) | |
| 110-113 | f4.1 | magnitude value | |
| 115-122 | a8 | arrival identification |

| Record | Position | Format | Description |
|---|---|---|---|
| 1 | 1-3 | a3 | Net |
| (header) | 15-18 | a3 | Sta |
| 27-29 | a4 | Type | |
| 33-35 | a8 | Latitude | |
| 37-44 | a9 | Longitude | |
| 46-54 | a9 | Coord Sys | |
| 57-60 | a4 | Elev | |
| 63-66 | a7 | On Date | |
| 63-66 | a8 | Off Date | |
| 2-n | 1-9 | a9 | network code |
| (data) | 11-15 | a5 | station code |
| 17-20 | a4 | 1c = single component | |
| 3c = three component | |||
| hfa = high-frequency array | |||
| lpa = long-period array | |||
| 22-30 | f9.5 | latitude (negative for South) | |
| 32-41 | f10.5 | longitude (negative for West) | |
| 43-54 | a12 | coordinate system (for example, WGS-84) | |
| 56-60 | f5.3 | elevation (km) | |
| 62-71 | i4,a1,i2,a1,i2 | start date of station operation (yyyy/mm/dd) | |
| 73-82 | i4,a1,i2,a1,i2 | end of station operation (yyyy/mm/dd) |

The grouped subtype is used for arrivals that have phase names and have been grouped together, with the implication that they were generated by the same seismic event. Table 36 gives the format for the grouped data subtype.
| Record | Position | Format | Description |
|---|---|---|---|
| 1 | 1-3 | a3 | Net |
| (header) | 11-13 | a3 | Sta |
| 16-19 | a4 | Chan | |
| 21-23 | a3 | Aux | |
| 29-32 | a4 | Date | |
| 39-42 | a4 | Time | |
| 50-54 | a5 | Phase | |
| 60-63 | a4 | Azim | |
| 66-69 | a4 | Slow | |
| 73-75 | a3 | SNR | |
| 83-85 | a3 | Amp | |
| 89-91 | a3 | Per | |
| 93-96 | a4 | Qual | |
| 100-104 | a5 | Group | |
| 106 | a1 | C | |
| 108-113 | a6 | Author | |
| 121-125 | a5 | ArrID |
| Record | Position | Format | Description |
|---|---|---|---|
| 2-n | 1-9 | a9 | network code |
| (data) | 11-15 | a5 | station code |
| 17-19 | a3 | FDSN channel code | |
| 21-24 | a4 | auxiliary identification code | |
| 26-35 | i4,a1,i2,a1,i2 | arrival date (yyyy/mm/dd) | |
| 37-48 | i2,a1,i2,a1,f6.3 | arrival time (hh:mm:ss.sss) | |
| 50-57 | a8 | phase code | |
| 59-63 | f5.1 | observed azimuth (degrees) | |
| 65-69 | f5.1 | observed slowness (seconds/degree) | |
| 71-75 | f5.1 | signal-to-noise ratio | |
| 77-85 | f9.1 | amplitude (nanometers) | |
| 87-91 | f5.2 | period (seconds) | |
| 93 | a1 | type of pick (a = automatic, m = manual) | |
| 94 | a1 | direction of short period motion (c = compression, d = dilatation, _= null) | |
| 95 | a1 | detection quality (i = impulsive, e = emergent, q = questionable, _ = null) | |
| 97-104 | a8 | group identification | |
| 106 | i1 | conflict flag (number of times an arrival belongs to more than one group; leave blank if arrival only belongs to one group) | |
| 108-116 | a9 | author of the arrival | |
| 118-125 | a8 | arrival identification |

Prior to 1996 the ISC bibliography provided a link between events and research papers associated with them. This data block reproduces the ISC bibliography, though please note that the format has not been finalised.

| Record | Position | Format | Description |
|---|---|---|---|
| 1 | 1-4 | a12 | Year |
| (header) | 6-11 | a3 | Volume |
| 13-17 | a6 | Page1 | |
| 19-23 | a3 | Page2 | |
| 25- | a4 | Journal | Record | Position | Format | Description |
| 2 | 1-4 | i4 | Year of publication |
| (data) | 6-11 | a6 | Volume |
| 13-17 | i5 | Start page | |
| 19-23 | i5 | End page | |
| 25-104 | a80 | Journal title |
| Record | Position | Format | Description |
|---|---|---|---|
| Comment Sub-block | |||
| 1 | 2-10 | a9 | (#AUTHORS |
| (data) | 11-90 | a80 | Author , author ... author. |
| 92 | a1 | ) | |
| 2-n | 2-3 | a2 | (+ |
| (continuation) | 11-90 | a80 | Author , author ... author. |
| 92 | a1 | ) |
| Record | Position | Format | Description |
|---|---|---|---|
| Comment Sub-block | |||
| 1 | 2-8 | a7 | (#TITLE |
| (data) | 11-90 | a80 | Title. |
| 92 | a1 | ) | |
| 2-n | 2-3 | a2 | (+ |
| (continuation) | 11-90 | a80 | Title |
| 92 | a1 | ) |

Each moment tensor report is comprised of two header lines and a variable number of pairs of data lines. All of the moment tensors in one report are for the same origin, which precedes the report. Several items are omitted: "Centroid, since it is presumed to precede in an origin line. "The best fitting double-couple, since it could follow as a FAULT_PLANE comment. "Principal axes, since they could follow as a PRINAX comment. "MW, since it could be included in the magnitude sub-block associated with the event. Several redundant items are included: "All three diagonal elements of the moment tensor are included since non-isotropic moment tensors may be reported occasionally "Scalar moment, fraction CLVD and their uncertainties are included since these may be the most frequently used moment tensor parameters.

| Record | Position | Format | Description |
|---|---|---|---|
| 1 | 3-10 | a8 | #MOMTENS |
| Header | 12-13 | a2 | sc |
| 18-19 | M0 | ||
| 21-25 | fCLVD | ||
| 30-32 | MRR | ||
| 37-39 | MTT | ||
| 44-46 | MPP | ||
| 51-53 | MRT | ||
| 58-60 | MTP | ||
| 65-67 | MPR | ||
| 69-72 | NST1 | ||
| 74-77 | NST2 | ||
| 79-84 | Author | Record | Position | Format | Description |
| 2 | 3 | a1 | # |
| (header) | 17-19 | a3 | eM0 |
| 21-25 | a5 | eCLVD | |
| 30-32 | a3 | eRR | |
| 37-39 | a3 | eTT | |
| 44-46 | a3 | ePP | |
| 51-53 | a3 | eRT | |
| 58-60 | a3 | eTP | |
| 65-67 | a3 | ePR | |
| 69-72 | a4 | NCO1 | |
| 74-77 | a4 | NCO2 | |
| 79-86 | a8 | Duration | Record | Position | Format | Description |
| 3 | 3 | a1 | # |
| (data) | 12-13 | i2 | scale factor (log10 of number by which moment tensor components and their uncertainties must be multiplied to obtain Newton-meters) |
| 15-19 | f5.3 | scalar seismic moment | |
| 21-25 | f5.3 | fraction of moment released as a compensated linear vector dipole | |
| 27-32 | f6.3 | radial-radial element of moment tensor | |
| 34-39 | f6.3 | theta-theta element of moment tensor | |
| 41-46 | f6.3 | phi-phi element of moment tensor | |
| 48-53 | f6.3 | radial-theta element of moment tensor | |
| 55-60 | f6.3 | theta-phi element of moment tensor | |
| 62-67 | f6.3 | phi-radial element of moment tensor | |
| 69-72 | i4 | number of stations used, type 1 (Body wave for HRVD) | |
| 74-77 | i4 | number of stations used, type 2 (Mantle or Surface wave for HRVD) | |
| 79-87 | a9 | agency that computed the moment tensor | |
| Record | Position | Format | Description |
| 4 | 3 | a1 | # |
| (data) | 15-19 | f5.3 | uncertainty of scalar seismic moment |
| 21-25 | f5.3 | uncertainty of fCLVD | |
| 27-32 | f6.3 | uncertainty of radial-radial element | |
| 34-39 | f6.3 | uncertainty of theta-theta element | |
| 41-46 | f6.3 | uncertainty of phi-phi element | |
| 48-53 | f6.3 | uncertainty of radial-theta element | |
| 55-60 | f6.3 | uncertainty of theta-phi element | |
| 62-67 | f6.3 | uncertainty of phi-radial element | |
| 69-72 | i4 | number of components used, type 1 | |
| 74-77 | i4 | number of components used, type 2 | |
| 79-86 | f8.2 | presumed or computed source duration (seconds) | |

Either one plane or two may be given.

| Record | Position | Format | Description |
|---|---|---|---|
| 1 | 3-14 | a12 | #FAULT_PLANE |
| (header) | 16-18 | a3 | Typ |
| 20-25 | a6 | Strike | |
| 29-31 | a3 | Dip | |
| 36-39 | a4 | Rake | |
| 42-44 | a2 | NP | |
| 46-47 | a2 | NS | |
| 49-53 | a5 | Plane | |
| 55-60 | a6 | Author | Record | Position | Format | Description |
| 2 | 3 | a1 | # first plane, + second plane |
| (data) | 16-18 | a3 | Fault plane solution computed from: |
| FM = first motions | |||
| BDC = best double couple | |||
| 20-25 | f6.3 | Strike of either nodal plane (degrees, 0 to 360) | |
| 27-31 | f5.3 | Dip of the same nodal plane (degrees, 0 to 90) | |
| 33-39 | f7.3 | Rake of slip vector in the described plane (degrees, -180 to +180; required if only one plane is given) | |
| 41-43 | i3 | number of P polarities (not required for type BDC) | |
| 45-47 | i3 | number of S polarisations (not required for type BDC) | |
| 49-53 | a5 | Plane identification: AUXIL = this is the auxiliary plane = neither plane is preferred at the fault | |
| FAULT = this is the preferred fault plane | |||
| AUXIL = this is the auxiliary plane | |||
| 55-62 | a8 | agency that computed the fault plane solution (neither required nor paresd for second plane) |

Principal axes can be computed from either a moment tensor or a fault plane solution. A bulletin may include the principal axes alone, or as well as the moment tensor or fault plane solution from which they were computed. Principal values are optional since they may not be available if the principal axes are computed from a fault plane solution based on first motions. The error header and error lines are each optional. ISPF writers should write the error header if the error data line is written. ISPF parsers should be able to parse the error line regardless of whether or not the error header line is present.

| Record | Position | Format | Description |
|---|---|---|---|
| 1 | 3-9 | a7 | #PRINAX |
| (header) | 11-12 | a2 | sc |
| 15-19 | a5 | T_val | |
| 21-26 | a6 | T_azim | |
| 29-32 | a4 | T_pl | |
| 35-39 | a5 | B_val | |
| 41-46 | a6 | B_azim | |
| 49-52 | a4 | B_pl | |
| 55-59 | a5 | P_val | |
| 61-66 | a6 | P_azim | |
| 69-72 | a4 | P_pl | |
| 74-79 | a6 | Author | Record | Position | Format | Description |
| 2 | 2 | a1 | + |
| (header) | 17-19 | a3 | eTv |
| 24-26 | a3 | eTa | |
| 30-32 | a3 | eTp | |
| 37-39 | a3 | eBv | |
| 44-46 | a3 | eBa | |
| 49-52 | a3 | eBp | |
| 57-59 | a3 | ePv | |
| 64-66 | a3 | ePa | |
| 70-72 | a3 | ePp | |
| 74-78 | a5 | fCLVD | Record | Position | Format | Description |
| 3 | 3 | a1 | # |
| (data) | 11-12 | i2 | scale factor (log10 of number by which moment tensor components and their uncertainties must be multiplied to obtain Newton-meters; optional) |
| 14-19 | f6.3 | largest principal value (optional) | |
| 21-26 | f6.2 | largest principal value axis azimuth | |
| 28-32 | f5.2 | largest principal value axis plunge | |
| 34-39 | f6.3 | middle principal value (optional) | |
| 41-46 | f6.2 | middle principal value axis azimuth | |
| 48-52 | f5.2 | middle principal value axis plunge | |
| 54-59 | f6.3 | smallest principal value (optional) | |
| 61-66 | f6.2 | smallest principal value axis azimuth | |
| 68-72 | f5.2 | smallest principal value axis plunge | |
| 74-81 | a8 | agency that computed the principal axes | Record | Position | Format | Description |
| 4 | 3 | a1 | # |
| (data) | 15-19 | f5.3 | uncertainty of T principal value (optional) |
| 22-26 | f5.2 | uncertainty of T axis azimuth | |
| 28-32 | f5.2 | uncertainty of T axis plunge | |
| 35-39 | f5.3 | uncertainty of B principal value (optional) | |
| 42-46 | f5.2 | uncertainty of B axis azimuth | |
| 48-52 | f5.2 | uncertainty of B axis plunge | |
| 55-59 | f5.3 | uncertainty of P principal value (optional) | |
| 62-66 | f5.2 | uncertainty of P axis azimuth | |
| 68-72 | f5.2 | uncertainty of P axis plunge | |
| 74-78 | f5.3 | fraction of the moment release as compensated linear vector dipole (optional) |

After the keyword PARAM, each origin parameter comment consists of a set of names from the MSOP list of earthquake parameters followed by an equal sign and a value. Spaces are not allowed before or after the equal sign, but are instead reserved as a separator between measurements. Units are not given for the measurements, but specified for each standard measurement name (e.g., STRESS_DROP must be given in Pascals). Values must be stated as real numbers including a decimal point and may include an exponent, indicated by an upper-case E , e.g., 1.0E27.
| Record | Position | Format | Description |
|---|---|---|---|
| 1 | 3-8 | a6 | #PARAM | (data) | 10-89 | a80 | NAME=VALUE NAME=VALUE .... |
| Name | Units | Description |
|---|---|---|
| STRESS_DROP | Pascals | |
| SCALAR_MOMENT | Newton-meters | |
| SEISMIC_ENERGY | Joules | |
| pP_DEPTH | Kilometers |

The icons included with each suitable event are links to other froms of data about the event, such as moment tensor solutions or waveform data. These links are not to data at the ISC but directly to the event information on the website of the agency or institution concerned. Where possible links have been included in the description to further details of the information displayed on following each link.
Broadband Array in Taiwan for SeismologyBroadband Array in Taiwan for Seismology (BATS) routinely estimates the source parameters of earthquakes occurring in the region. The link provided is to the image file posted on the BATS website.
GeoForschungsZentrum Potsdam (GFZ)The GEOFON SPYDER node presently regularly retrieves the data from about 40 stations e.g. nearly all permanent GEOFON stations and a set of other stations in Central Europe for all global events larger mb 5.5. This system is a common effort with IRIS DMC, ORFEUS DC and several other SPYDER nodes worldwide triggered by NEIC alerts. From GFZ, the GEOFON SPYDER data are distributed to ORFEUS Data Center and IRIS DMC by Internet and their data are copied to Potsdam the same way. Therefore several hours after origin time the event data for up to over 100 stations become available at the GEOFON DC for all major global events.
A more detailed description of the data from the GFZ link and other sevices can be found on the GFZ website.
Incorporated Research Institutions for Seismology (IRIS)The IRIS Fast Archive Recovery Method ( FARM ) provides a source of information about events of magnitude 5.7 or larger or deep events of magnitude 5.5 and larger. Each data set will include atleast:
More information on the FARM data can be found on the IRIS website.
Incorporated Research Institutions for Seismology (IRIS)The IRIS Wilber II interface offers an improved service over the previous FARM system ( detailed above ). More details can be seen about Wilber II at the IRIS website. Data selection can also be made from the Wilber II interface.
MedNet Data CentreRegional Centroid Moment Tensor solutions from the MedNet ( Very-broadband seismographic network in the Mediterranean )
ORFEUS Data CentreProvides direct access to the waveform data at the Royal Netherlands Meteorological Institute as part of the ORFEUS Data Centre. The data is in the form of SUN binary files and contains:
Earthquake Research InstituteThis link is to the Centroid Moment Tensor (CMT) calculated by the Earthquake Research Institute (ERI) at the University of Tokyo. These CMT solutions are automatically calculated and posted on the internet by the ERI. A brief description of the data and a full listing of the available soltuions can be accessed on the ERI website.
University of MichiganThe Department of Geological Sciences at the University of Michigan provides access to summary information on Moment Tensor Rate Functions solutions and Source Time Function solutions (STF) as part of the Seismological Observatory.
The icon shown above provides a link to the STF solution.
Harvard UniversityThe Harvard Seismology, Centroid-Moment Tensor Project routinely calculates Centroid Moment Tensor solutions for events with a moment magnitude (Mw) greater than 5.5. The link provided here is to the solution which matches certain parameters of the event in question. On occaisions more than one solution may be returned if a number of events occur in close proximity.
The icon shown above provides a link to the STF solution.
Xerox Palo Alto Research CenterThe Xerox Palo Alto Research Center (Xerox PARC) provides a server that produces maps from http requests.
The link provides a simple map that shows the position of the station or of the epicentres for an event.
COSMOS Virtual Data CenterThe Consortium of Organizations for Strong-Motion Observation Systems COSMOS provides access to a number of strong-motion data sources.