Magnitude 4.0 Earthquake Struck 9 km ESE of T’q’ibuli, Georgia on October 08, 2014 12:36:18
Last Updated: 2015-01-06 23:49:47On October 08, 2014 12:36:18 an earthquake with magnitude of 4.0 on the richter scale hit 9 km ESE of T’q’ibuli, Georgia. The earthquake originated at a depth of approximately 10.0 kilometers below the Earth's surface on longitude 43.104° and latitude 42.318°. According to documented reports 0 people felt the earth quake, No tsunami was triggered due to the earthquake.
Magnitude & Depth
The earthquake that appeared on October 08, 2014 12:36:18 had a magnitude of 4.0 on the richter scale. Which is considered to be a minor earthquake and is often felt but causes little to no damage.
Shallow earthquakes are considered between 0 and 70 km deep, while intermediate earthquakes range from 70 - 300 km deep and deep earthquakes are between 300 - 700 km deep.
Are shallow earthquakes more destructive?
Shallow quakes generally tend to be more damaging than deeper quakes. Seismic waves from deep quakes have to travel farther to the surface, losing energy along the way.
Nearby Cities and Towns
The nearest significant population center is Tqibuli in Imereti, Georgia, located 9 kilometers or 5 miles ← W of the earthquake's epicenter. Other cities in close proximity include K’alak’i Chiat’ura (Imereti, Georgia) located 12 km (7 mi) → E and Chiat’ura (Imereti, Georgia) located 16 km (10 mi) → E of the epicenter.
In total, we found 31 cities in our database that might have been impacted by the earthquake.
Nearby Power Plants
We found a total 5 utility-scale power plants in the vecinity of the earthquakes epicenter. The closest being Shaori Hydroelectric Power Plants Georgia Hydro power plant, located 9 kilometers (6 miles) ← W from the epicenter.
| Distance | Direction | Power Plant | Type | Capacity |
|---|---|---|---|---|
| 9 km (6 mi) | ← W | Shaori Hydroelectric Power Plants Georgia | Hydro | 38.4 MW |
| 13 km (8 mi) | ↙ SW | Dzevrula (Tkibuki-II) Hydroelectric Power Plants Georgia | Hydro | 80.0 MW |
| 32 km (20 mi) | ← W | Gumati I and II Hydroelectric Power Plants Georgia | Hydro | 68.8 MW |
| 33 km (20 mi) | ↙ SW | Rioni Hydroelectric Power Plant Georgia | Hydro | 48.0 MW |
| 36 km (22 mi) | ↖ NW | Lajanuri Hydroelectric Power Plant Georgia | Hydro | 113.0 MW |
Power Plants & Risks During Earthquakes
We found 1 types of power plants in the vecinity of the magnitude 4.0 earthquake that struck 9 km ESE of T’q’ibuli, Georgia on October 08, 2014 12:36:18. These types were Hydro power plants, below you find information how each type of power plant can pose a risk to you as a person or the ecosytem around you.
None of this information should be used as guidence in an event of an emergency, but rather as additional references to information provided by national, state and local authorities.Hydropower
Hydropower plants are generally considered as safe in many aspects, but when it comes to severe earthquakes they pose a substantial risk that can manifest in the form of dam faliours, landslides and grave impacts on surrounding ecosystems.
Dam Failure
The most significant risk is the potential failure of the dam that holds the water reservoir. Severe ground shaking can damage or breach the dam, leading to downstream flooding and as a result endangering people and wildlife living downstream. Such an event can also have severe impact on key infrastructure that cascades through society.
Landslides
Earthquakes can trigger landslides in the areas surrounding hydropower plants, potentially damaging infrastructure and causing harm to nearby communities.
Damage to Aquatic Ecosystems
Both landslide and dam failures can have a severe impact on upstream and downstream aquatic wildlife, ecosystem and groundwater, resulting in longterm risks for people and industires living and operating in areas near the water supply.
To mitigate these risks, engineering and construction standards for hydropower plants often include earthquake-resistant designs. These designs incorporate measures such as flexible foundations, strengthened dam structures, and advanced monitoring systems to detect early signs of stress. Additionally, emergency plans and evacuation procedures should be in place to protect personnel and downstream communities in the event of a severe earthquake.
Data Information
Information found on this page is a derivative set, based on sources mentioned below.
Data Sources
We aggregate and combine data from USGS (United States Geographical Survey) and the EMSC (European-Mediterranean Seismological Centre). This allow us to get near real-time and historical earthquake data dating back to the year 1950.
Disclaimer
Information or data found on this page should not be used for, or as an early warning system. It is intended as an historical reference or near real-time complementary information to offical and governmental sources. In an event of an emergency it is important closely monitor and follow advice from national, state and local authorities.