How quickly is earthquake information posted to the USGS website and sent out via the Earthquake Notification Service (ENS) and other feeds?
USGS earthquake information mechanisms are all triggered by the same system, so they all receive the information at the same time. The time it takes for the system to receive the information primarily depends on the size and location of the earthquake:
An earthquake in California is processed and posted to the system in 2.5 minutes (on average). This is because our seismic network is very extensive in California, where there are many earthquakes and many people.
An earthquake in the U.S. outside of California (where seismic networks are not as dense), is typically posted within 8 minutes.
An earthquake outside the United States, where the seismic network is sparse in some areas, takes 20 minutes (on average) to process and post. Our webpages with realtime information are cached for 60 seconds, so there might be an additional delay of up to 60 seconds for the webpage to be updated.
From the time each system receives the information to the time you receive the information is the same for all systems, usually within a few seconds (unless there are network problems), except for the Earthquake Notification System (ENS) and the earthquake feeds, which can vary.
Since ENS has many thousands of accounts, all customized to receive different notifications, the time between ENS receiving the information and you receiving your notification can vary quite a bit. A large earthquake that generates many notifications might take up to 45 minutes to reach the last account on the list. A small earthquake that generates fewer notifications will take only a matter of several minutes to reach all accounts. The time it takes for the notifications to be sent depends on the capacity of the machines that send the email.
Social media outlets, such as Twitter, might be able to broadcast the occurrence of an earthquake faster than the USGS can using our standard mechanisms, but they cannot provide any quantitative data such as location and magnitude.
For the various Feeds, we cache different feeds for different lengths of time, so it depends on the feed you access. We try to balance data volume, how often the data in the feeds change, and server load so:
- GeoJSON 7-days and less feeds are cached for 1 minute
- Other 7-day and less feeds are cached for 5 minutes
- 30-day feeds and searches are cached for 15 minutes
- Event pages (and geojson detail feeds) are cached for 1 minute for the first 7 days after an event, and for 15 minutes after that
The Earthquake Map/List/Search interface uses GeoJSON feeds.
Related
Why/When does the USGS update the magnitude of an earthquake? Why/When does the USGS update the magnitude of an earthquake?
The USGS often updates an earthquake's magnitude in the hours and sometimes days following the event. Updates occur as more data become available for analysis and more time-intensive analysis is performed. Additional updates are possible as part of the standard procedure of assembling a final earthquake catalog. There are physical and operational constraints on how quickly seismic data are...
Why do so many earthquakes occur at a depth of 10km? Why do so many earthquakes occur at a depth of 10km?
Ten kilometers is a "fixed depth." Sometimes data are too poor to compute a reliable depth for an earthquake. In such cases, the depth is assigned to be 10 km. Why that number? In many areas around the world, reliable depths tend to average 10 km or close to it. For example, if we made a histogram of the reliable depths in such an area, we'd expect to see a peak around 10 km. So if we don't know...
Where can I see current or past seismograms? Where can I see current or past seismograms?
The USGS Earthquake Hazards Program has helicorders (seismogram displays) available for several areas in the United States and the World. Our research partner IRIS (Incorporated Research Institutions for Seismology) has two applications, the Station Monitor and the Global Seismogram Viewer, for viewing seismograms. IRIS also supplies software that allows users to collect and view seismic data from...
Why do USGS earthquake magnitudes differ from those published by other agencies? Why do USGS earthquake magnitudes differ from those published by other agencies?
Magnitude estimates for a given earthquake can vary between reporting agencies due to differences in methodology, data availability, and inherent uncertainties in seismic data. Individual agencies use magnitude estimation procedures designed to meet the agency's specific needs and monitoring capabilities. Even for well-recorded events, differences in magnitude of 0.2 or 0.3 units are common and...
What is UTC, and why do you report earthquakes in UTC? What is UTC, and why do you report earthquakes in UTC?
UTC stands for Coordinated Universal Time, and for this purpose is the same as GMT (Greenwich Mean Time). Since the USGS and other seismic network agencies record earthquakes around the globe in all the various time zones, using a single standard time reference is best for record-keeping and exchange of data. The individual event pages with details about each earthquake use UTC for the reference...
Related
Why/When does the USGS update the magnitude of an earthquake? Why/When does the USGS update the magnitude of an earthquake?
The USGS often updates an earthquake's magnitude in the hours and sometimes days following the event. Updates occur as more data become available for analysis and more time-intensive analysis is performed. Additional updates are possible as part of the standard procedure of assembling a final earthquake catalog. There are physical and operational constraints on how quickly seismic data are...
Why do so many earthquakes occur at a depth of 10km? Why do so many earthquakes occur at a depth of 10km?
Ten kilometers is a "fixed depth." Sometimes data are too poor to compute a reliable depth for an earthquake. In such cases, the depth is assigned to be 10 km. Why that number? In many areas around the world, reliable depths tend to average 10 km or close to it. For example, if we made a histogram of the reliable depths in such an area, we'd expect to see a peak around 10 km. So if we don't know...
Where can I see current or past seismograms? Where can I see current or past seismograms?
The USGS Earthquake Hazards Program has helicorders (seismogram displays) available for several areas in the United States and the World. Our research partner IRIS (Incorporated Research Institutions for Seismology) has two applications, the Station Monitor and the Global Seismogram Viewer, for viewing seismograms. IRIS also supplies software that allows users to collect and view seismic data from...
Why do USGS earthquake magnitudes differ from those published by other agencies? Why do USGS earthquake magnitudes differ from those published by other agencies?
Magnitude estimates for a given earthquake can vary between reporting agencies due to differences in methodology, data availability, and inherent uncertainties in seismic data. Individual agencies use magnitude estimation procedures designed to meet the agency's specific needs and monitoring capabilities. Even for well-recorded events, differences in magnitude of 0.2 or 0.3 units are common and...
What is UTC, and why do you report earthquakes in UTC? What is UTC, and why do you report earthquakes in UTC?
UTC stands for Coordinated Universal Time, and for this purpose is the same as GMT (Greenwich Mean Time). Since the USGS and other seismic network agencies record earthquakes around the globe in all the various time zones, using a single standard time reference is best for record-keeping and exchange of data. The individual event pages with details about each earthquake use UTC for the reference...