A landform class assigned to the whole 250 m mesh and used to estimate AVS30. The name alone does not determine safety, and it is model data rather than a borehole survey at the station.
Aomori earthquake and Shindo history in 2017
青森県
This annual view includes only earthquakes from 2017 for which stations associated with Aomori recorded Shindo.
Data period: 1 January–31 December 2017In 2017, stations associated with Aomori reported local Shindo for 1 earthquakes. The highest local level recorded that year was Shindo 4.
Observation history · 2017
This history counts earthquakes observed at stations in the place, not earthquakes whose epicentre lies inside its boundary. Counts can change as stations are updated and older or corrected observations are added.
Observed events by year
Choose a year to update the event history and local Shindo distribution.
Shindo observed in this place
The highest reading from stations in this place, not the maximum Shindo of the whole event.
Observation history · 2017
1 observed earthquakes
Regional context
The context below uses the place's full available history and reference models; it is not part of the 2017 statistics.
Where the shaking usually comes from
Source regions of earthquakes observed here, ordered by the number of reports.
Ground conditions near an observation station
J-SHIS data for the 250 m mesh containing 青森市花園.
How to read these values
The average speed of an S-wave through the upper 30 metres. A lower value generally indicates softer material that can amplify shaking more. J-SHIS uses this value to estimate the amplification shown to the right. It is not predicted Shindo.
For the same incoming wave, local ground conditions may make peak-motion velocity at the surface about 94% higher than at engineering bedrock (Vs = 400 m/s). This value describes motion velocity—it does not multiply magnitude or forecast ground acceleration.
Ground conditions can change over short distances. These values do not rate the whole place or the safety of a building, and they cannot predict an earthquake. Source: J-SHIS (NIED), V4 model; processed for presentation by JISHINDESU.
Earthquake scenarios affecting this place
Official J-SHIS models ranked for their potential impact on this prefecture.
#1 means the model ranks highest in the J-SHIS result for this place under the same settings. It is not a ranking of which earthquake will happen next.
Magnitude on a card describes the size of the whole earthquake model, not the Shindo expected here. Local shaking also depends on distance, depth and ground conditions.
Modelled magnitude: M6.8
Read about this model #2Subduction-zone earthquakeHuge interplate earthquakes in Aomori-ken-toho-Oki and Northern Iwate-ken-Oki青森県東方沖及び岩手県沖北部のプレート間巨大地震Modelled magnitude: M7.9–8.8
Read about this model #3Major active faultOritsume fault折爪断層Modelled magnitude: M7.0
Read about this model #4Other active faultTsugaru-sanchi-seien fault zone hokubu hoppou enchou津軽山地西縁断層帯北部北方延長Modelled magnitude: M6.8
Read about this model #5Other active faultIwaki-san-nanroku fault zone岩木山南麓断層帯Modelled magnitude: M6.6
Read about this model #6Other active faultNoheji fault zone野辺地断層帯Modelled magnitude: M7.0
Read about this model #7Subduction-zone earthquakeMega earthquakes along the Kuril Trench千島海溝沿いの超巨大地震Modelled magnitude: M8.7–9.2
Read about this model #8Subduction-zone earthquakeHuge interplate earthquakes in Tokachi-oki十勝沖のプレート間巨大地震Modelled magnitude: M8.0–8.6
Read about this model #9Subduction-zone earthquakeAomori-ken-seiho-Oki Earthquake青森県西方沖の地震Modelled magnitude: M7.7
Read about this model #10Major active faultTsugaru-sanchi-seien fault zone (Southern part)津軽山地西縁断層帯南部Modelled magnitude: M6.6
Read about this model #11Major active faultTsugaru-sanchi-seien fault zone (Northern part)津軽山地西縁断層帯北部Modelled magnitude: M6.4
Read about this model #12Subduction-zone earthquakeMega earthquakes along the Japan Trench (Great East Japan Earthquake 2011 type)日本海溝沿いの超巨大地震(東北地方太平洋沖型)Modelled magnitude: M8.6–9.0
Read about this modelJ-SHIS 2020 model, 30-year period and Shindo 6-lower threshold. This is not a prediction of a particular earthquake. Source: J-SHIS (NIED); processed for presentation by JISHINDESU.
Municipalities in this prefecture
Municipalities with an observation history, ordered alphabetically. Counts depend on station coverage and the available data period; they are not a risk ranking.
83 Observed eventsShindo 4
→282 Observed eventsShindo 4
→189 Observed eventsShindo 4
→93 Observed eventsShindo 3
→851 Observed eventsShindo 5+
→170 Observed eventsShindo 5−
→1,132 Observed eventsShindo 6+
→1,240 Observed eventsShindo 6+
→729 Observed eventsShindo 5+
→152 Observed eventsShindo 4
→341 Observed eventsShindo 5−
→116 Observed eventsShindo 4
→121 Observed eventsShindo 4
→144 Observed eventsShindo 4
→120 Observed eventsShindo 4
→116 Observed eventsShindo 4
→122 Observed eventsShindo 4
→417 Observed eventsShindo 5−
→502 Observed eventsShindo 5+
→139 Observed eventsShindo 4
→88 Observed eventsShindo 3
→506 Observed eventsShindo 5+
→509 Observed eventsShindo 6−
→184 Observed eventsShindo 4
→64 Observed eventsShindo 3
→325 Observed eventsShindo 5−
→405 Observed eventsShindo 5−
→221 Observed eventsShindo 4
→511 Observed eventsShindo 5+
→532 Observed eventsShindo 5+
→148 Observed eventsShindo 4
→342 Observed eventsShindo 5−
→240 Observed eventsShindo 4
→552 Observed eventsShindo 5+
→356 Observed eventsShindo 4
→213 Observed eventsShindo 5−
→134 Observed eventsShindo 5−
→340 Observed eventsShindo 5−
→120 Observed eventsShindo 3
→Understand local Shindo in context
Guides to this place’s history, seismic intensity and notification tools.
Learn what Japan’s Shindo earthquake intensity scale measures, what levels 0, 5 Lower, 5 Upper and 7 mean, and why Shindo is different from magnitude.
Read guide →10 min readHow to use the JISHINDESU interactive mapA guide to the redesigned map panel: adding and switching places, ten years of history, filters, local Shindo readings, sharing and notifications.
Read guide →6 min readAre earthquakes becoming more frequent in Japan?How to compare earthquake counts fairly—and why a few active days do not prove a lasting increase.
Read guide →4 min readAway from home? Monitor earthquakes in your Japanese townUse home as the reference point and receive notifications without an account when a station within the selected radius reports your chosen Shindo level.
Read guide →