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DESCRIPTION An earthquake occurs when two blocks of the earth suddenly slip past one another. The surface where they slip is called the fault or fault plane. Rapid shaking of the earth caused by this slip of the fault or fault plane creates seismic waves. This shaking can cause widescale damage, such as collapsing buildings and bridges and disruption in utility and phone service. Earthquakes are also the primary cause of tsunamis and can sometimes trigger landslides, which may indirectly cause flash floods or fires. Measures The Richter Scale measures earthquake size but is not a well understood concept. Advances in ability and use of this magnitude scale have occurred since it was first developed in the 1930s. Today, seismograph stations around the world measure the body wave and surface wave magnitude of these events. Because of the limitations of the Richter Scale, a new more uniformly applicable extension of the magnitude scale, known as moment magnitude, or Mw, was developed. It is particularly useful for very large earthquakes, while the Richter Scale is mostly effective for regional-sized earthquakes. Moment magnitude measures how much energy is released from a seismic event. The moment can be estimated from seismograms and the scale ranges from 0 to 10. Each increase in number is about 32 times greater than the previous number. Mw provides an estimate of earthquake size that is valid over the complete range of magnitudes, a characteristic that was lacking in other magnitude scales. The Modified Mercalli Intensity Scale (MM) is a value assigned to a specific site after an earthquake and has a more meaningful measure of severity to the nonscientist than the magnitude. This is a measure of intensity, rather than magnitude, and is denoted by Roman numerals. Being far from the epicenter of an earthquake would mean people and structures experience a lower intensity, so the MM value would be lower. Whereas being close to the epicenter of an earthquake would have a higher MM value because people and structures would experience a higher intensity. Structural engineers usually contribute information for assigning intensity values of VIII or above. LOCATION The U.S. Geological Survey (USGS) has an interactive map that shows faults and associated folds in the U.S. The map contains
    information on faults and associated folds in the U.S. that are believed to
    be sources of M>6 earthquakes during the Quaternary (the past 1,600,000
    years). It shows most activity occurs in the western U.S. HISTORIC OCCURRENCES Earthquakes are very rare in Florida and there are no significant recorded
    incidents. Additionally, many of the reports of earthquakes from before
    technological advancements have no proof and the original reports have been
    lost. Many reports of earthquakes felt in Florida are unsubstantiated and
    only known because of personal accounts of “tremblors.” The 1886 Charleston, South Carolina earthquake was felt in Florida. There
    was a shock felt in 1978 and then there was no seismic activity in Florida
    until 2006 when a quake in the Gulf of Mexico was reportedly felt in
    Florida. Shaking in 2016 was thought to be a rare earthquake affecting
    Florida, but the shaking was caused by U.S. Navy explosion tests. USGS has
    an interactive map showing past occurrences of earthquakes. The table below displays notable
    earthquake occurrences in Florida from 1727-2022. PROBABILITY D – Light Brown D1 – Darker Brown D2 – Darkest Brown The map below shows zones of peak ground acceleration as a percentage of gravitational acceleration. There is a two percent probability that the given acceleration range will be exceeded in a 50-year period. Peak ground acceleration refers to the maximum shaking that occurs at a specific location during an earthquake. Generally, a peak ground acceleration of 0.01 m/s^2 is felt by humans and a peak ground acceleration of 0.2 m/s^2 can cause people to lose their balance.  As shown in the map above from USGS, the lower Peninsula would experience 0.20 m/s^2 peak ground acceleration in the event of an earthquake, while the northern half of the state would experience 0.39 m/s^2 or greater. Portions of Escambia, Santa Rosa, Okaloosa, Madison, Hamilton, Suwannee, Columbia, Baker, Union, Bradford, Nassau, Duval, Clay, St. Johns, and Putnam counties would perhaps experience 0.59 m/s^2 peak ground acceleration. To be clear, if an earthquake occurs near Florida, tremors may be felt in some areas. This hazard was determined to occur about every 50 to 100 years, giving it a Probability ranking of Not Likely. CLIMATE CHANGE Climate change is not expected to affect the occurrence or magnitude of seismic events in Florida. IMPACTS The following list shows potential impacts from earthquake to populations, the built environment, natural resources, the economy, and government. Populations Built Environment Natural Resources Economy Government Populations in urban areas may face greater risk, but there is statewide
                exposure to earthquake impacts. Based on previous occurrences, typical
                impacts include: First responders may be more at risk during rescue missions if structures are damaged and become unstable. VULNERABILITY The Enhanced SHMP is required to evaluate the vulnerability of the state and estimate potential losses for each hazard. Below is the vulnerability analysis and loss estimation for the state, by jurisdiction and for state assets, for earthquake. Further, overall vulnerability is calculated based on frequency, probability, and magnitude, and scored up to 15. This information is displayed in the figure below. For more information on how overall vulnerability was calculated, visit the Risk Assessment page. Vulnerability Analysis and Loss Estimation by Jurisdiction Jurisdictional Risk Analysis Jurisdictional Risk and State Resilience LMS Integration Analysis Local and Federal Risk Comparison According to the Peak Ground Acceleration Map above, most of the state has equally low vulnerability. There are small portions of north Florida that may experience slightly more intense shaking; however, vulnerability remains low based on previous occurrences. Due to Florida’s geography and proximity to fault lines, no losses are expected. When looking at resilience throughout the state, it is important to analyze the infrastructure and essential community lifelines that are most vulnerable to hazards. FEMA Community Lifelines include Safety and Security; Food, Water, Shelter; Health and Medical; Energy; Communications; Transportation; and Hazardous Material. This section will analyze how earthquake may impact these lifelines and ultimately impact the resiliency of the state. As shown above, minor impacts from earthquakes have occurred in Florida. However, it is very unlikely that the stability of lifelines or overall state resilience will be impacted by earthquakes. An analysis of all 67 Florida County LMS Plans, and their individual earthquake hazard rankings was completed and mapped (see section below). Only 21 counties profiled seismic events as a hazard. The information below shows the various rankings: Local and Federal Risk Comparison Earthquake LMS Ranking Map Earthquake FEMA NRI Map Vulnerability Analysis and Loss Estimation of State Assets Similarly to the jurisdiction vulnerability and loss estimates, state assets have a low vulnerability to seismic events and minimal to no losses expected. This includes state-owned facilities, critical facilities, and other community lifelines, which are essential for human health and safety and economic security. As mentioned throughout this profile, impacts from earthquake occur rarely in Florida. If events do occur, it is important to consider how populations may be affected. As with other hazards, vulnerable populations may be more at risk than the general population. Vulnerable populations that may be impacted by earthquakes are socioeconomically disadvantaged populations, minority populations, individuals with disabilities, youth, and the elderly. Infants, children, and the elderly face vulnerability due to the lack of mobility if an evacuation is required. Elderly populations may have a more difficult time recovering from a seismic event due to limited finances in retirement. Additionally, chronic health conditions may worsen if one’s dwelling is damaged or becomes unlivable. Individuals with disabilities face many of the same threats. These individuals face evacuation challenges due to mobility, medical reliance, and possible isolation. Each of these populations may require longer evacuation warning times. Socioeconomically disadvantaged populations are vulnerable to earthquake hazards due to their living environment, poverty, and potential lack of insurance coverage. These circumstances may limit the ability of these individuals to recover quickly and fully. Additionally, the socioeconomically disadvantaged neighborhoods are often located in areas with older construction, offering little to no protection. Minority populations often face many of the same issues. Beyond vulnerable populations, emergency professionals that would respond to an earthquake event are more at-risk due to the nature of their jobs. Potential complications can range from minor health issues to fatality. Search and rescue crews are especially at risk from the potential instability of damaged structures. Some of these working professionals include law enforcement, fire services, public health, and health care. Using the data shown throughout this profile, the planning team gave an Overall Vulnerability Score of 5 or Low for earthquake, with no change in score from the 2018 SHMP. This hazard has been determined to have a low frequency of occurrence and will remain low in the future. Additionally, little to no impact to people, environment, infrastructure, or economy has been recorded.

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opendata-ui/config/asset-manifest

ember-cli-head-start

application-name

https://hubcdn.arcgis.com/opendata-ui/assets/hub-components/assets/i18n

hub-components-assets-url

ember-cli-head-end

MarkMonitor Inc.

ARCGIS.COM

Amazon EC2 Abuse

IP Management

Amazon AWS Network Operations

Amazon.com, Inc.

AWS RPKI Management POC

IP Routing

Amazon EC2 Network Operations

AMAZO-CF


      window.__DOMAIN={"domainInfo":{"id":"127047","hostname":"flshmp-floridadisaster.hub.arcgis.com","siteId":"de76ec12c1774a4bb24ad490bfe64242","clientKey":"lI040C9ISSr7WO04","orgKey":"floridadisaster","siteTitle":"2022 SHMP 1","orgId":"3wFbqsFPLeKqOlIK","orgTitle":"Florida Division of Emergency Management","createdAt":"2022-02-04T17:25:21.027Z","updatedAt":"2023-05-22T15:24:12.434Z","sslOnly":true,"permanentRedirect":false,"redirectTo":null,"domain":"flshmp-floridadisaster.hub.arcgis.com"}}
    

FL SHMP


      if (typeof customElements !== 'undefined') {
        customElements.efineday = customElements.define;
      }
    

HSTS

Earthquake | FL SHMP

✅ Low Risk - https://flshmp-floridadisaster.hub.arcgis.com/pages/earthquake

Requests	IP Address	Location	AS Autonomous System
76	3.174.46.121	United States	AS16509Amazon.com, Inc.
76	3.215.20.206	Ashburn, Virginia, United States	AS14618Amazon.com, Inc.
152	2	-	-

Security Scan Report: flshmp-floridadisaster.hub.arcgis.com

Summary

AI Security Verdict

Safe Website

Safety Factors

Details

Screenshot

Page Load Overview

Language Analysis

Primary Language

Detection Details

Website Classification

Primary Category

All Detected Categories

Detected Features

Domain & IP Information

Detected Technologies1

Content Similarity HashesFor malware variant detection

TLSH (Trend Micro Locality Sensitive Hash)

ssdeep (Context Triggered Piecewise Hashing)

sdhash (Similarity Digest Hashing)

Image Hashes

Perceptual Hashes

Other Hashes

Scan History