안탈리아
도시 선택
점수는 세계 공통 척도의 연구 추정치입니다. R은 작업 중을 뜻하며 여행 조언이 아닙니다.
장소 확인
마음에 드는 호텔을 찾으셨나요? 예약 전에 주변 지역을 확인하세요.
검색 서비스 정책
검색 시 입력 내용과 선택 도시를 OpenStreetMap Nominatim에 전송합니다. 사적인 주소나 민감 정보를 입력하지 마세요. 검색 서비스 정책
점수는 세계 공통 척도의 연구 추정치입니다. R은 작업 중을 뜻하며 여행 조언이 아닙니다.
마음에 드는 호텔을 찾으셨나요? 예약 전에 주변 지역을 확인하세요.
검색 시 입력 내용과 선택 도시를 OpenStreetMap Nominatim에 전송합니다. 사적인 주소나 민감 정보를 입력하지 마세요. 검색 서비스 정책
떠나기 전에 알아보세요
출처가 있는 연구 추정치입니다. 지역 자료가 불완전하며 필요시 광역 대체값을 사용합니다.
도시 전체 연구 추정치: 68/100. 모델 척도에서 높을수록 더 안전합니다. 근거 날짜: · 자료 신뢰도: D
연구 추정치: 현지 근거가 있는 한 항목만 달라지고 다른 항목은 도시·국가 기준값을 유지합니다. 무색 지역은 지역 근거가 없으며 안전하다는 뜻이 아닙니다.
5개 지역 표시 ·
경계: OpenStreetMap contributors · Five Antalya central districts (ODbL 1.0; © OpenStreetMap contributors)
도시 점수는 개별 거리·호텔·시간대를 설명하지 않습니다. 레이어의 출처·날짜·한계를 확인하세요.
Compare Antalya central districts, including long-term earthquake exposure and source-linked safety context.
Five central Antalya districts: Muratpaşa, Kepez, Konyaaltı, Aksu and Döşemealtı. The layer does not cover the whole Antalya province or outlying resort districts. ESHM20 mean peak ground acceleration (PGA, units g), annual exceedance probability 0.002103 (approximately 10% in 50 years / 475-year return period), reference rock Vs30=800 m/s. This is long-term modelled shaking, not earthquake prediction, observed damage, local soil amplification or building resistance. The model uses a 0.1-degree grid (roughly 9–11 km here). District values are area-weighted nearest-cell aggregates in UTM 36N. Administrative outlines locate the aggregates and do not imply street-level seismic precision. Only disaster_and_environment varies locally; the citywide estimate and other dimensions retain the existing Türkiye country research calibration. This map does not measure district crime or compare hotels. Danciu et al. (2021), The 2020 update of the European Seismic Hazard Model: Model Overview, EFEHR Technical Report 001, doi:10.12686/a15. CC BY 4.0 https://creativecommons.org/licenses/by/4.0/; Safrom computed district aggregates and research scores. No EFEHR endorsement. OpenStreetMap administrative boundaries retrieved 2026-10-27, generalized 10 m with less than 0.5% area change; © OpenStreetMap contributors, ODbL 1.0.
Five central Antalya districts: Muratpaşa, Kepez, Konyaaltı, Aksu and Döşemealtı. The layer does not cover the whole Antalya province or outlying resort districts. ESHM20 mean peak ground acceleration (PGA, units g), annual exceedance probability 0.002103 (approximately 10% in 50 years / 475-year return period), reference rock Vs30=800 m/s. This is long-term modelled shaking, not earthquake prediction, observed damage, local soil amplification or building resistance. The model uses a 0.1-degree grid (roughly 9–11 km here). District values are area-weighted nearest-cell aggregates in UTM 36N. Administrative outlines locate the aggregates and do not imply street-level seismic precision. Only disaster_and_environment varies locally; the citywide estimate and other dimensions retain the existing Türkiye country research calibration. This map does not measure district crime or compare hotels. Danciu et al. (2021), The 2020 update of the European Seismic Hazard Model: Model Overview, EFEHR Technical Report 001, doi:10.12686/a15. CC BY 4.0 https://creativecommons.org/licenses/by/4.0/; Safrom computed district aggregates and research scores. No EFEHR endorsement. OpenStreetMap administrative boundaries retrieved 2026-10-27, generalized 10 m with less than 0.5% area change; © OpenStreetMap contributors, ODbL 1.0.
Five central Antalya districts: Muratpaşa, Kepez, Konyaaltı, Aksu and Döşemealtı. The layer does not cover the whole Antalya province or outlying resort districts.
ESHM20 mean peak ground acceleration (PGA, units g), annual exceedance probability 0.002103 (approximately 10% in 50 years / 475-year return period), reference rock Vs30=800 m/s. This is long-term modelled shaking, not earthquake prediction, observed damage, local soil amplification or building resistance.
The model uses a 0.1-degree grid (roughly 9–11 km here). District values are area-weighted nearest-cell aggregates in UTM 36N. Administrative outlines locate the aggregates and do not imply street-level seismic precision.
Only disaster_and_environment varies locally; the citywide estimate and other dimensions retain the existing Türkiye country research calibration. This map does not measure district crime or compare hotels.
Danciu et al. (2021), The 2020 update of the European Seismic Hazard Model: Model Overview, EFEHR Technical Report 001, doi:10.12686/a15. CC BY 4.0 https://creativecommons.org/licenses/by/4.0/; Safrom computed district aggregates and research scores. No EFEHR endorsement.
OpenStreetMap administrative boundaries retrieved 2026-10-27, generalized 10 m with less than 0.5% area change; © OpenStreetMap contributors, ODbL 1.0.
alerts are not long-term baseline risk; event footprint may not equal traveler exposure; alert severity cannot be copied directly into Safrom score
country-level only; humanitarian risk framing differs from traveler exposure; composite inputs can overlap Safrom dimensions; current event conditions require separate signals
country-level only; reporting and justice-system differences; latest year differs by country; not traveler-specific
country-level only; availability does not measure emergency accessibility; latest year differs by country; distribution within a country is hidden
country-level only; collection is not annual for every country; some values are modeled estimates; resident exposure differs from traveler exposure
Syria and Iraq border restrictions do not describe Istanbul; legal risk differs from ordinary city crime; advisory level is not an absolute safety score; U.S.-traveler perspective
country-level only; modeled perceptions rather than traveler incidents; cannot represent neighborhood variation or current events; confidence intervals must not be discarded
ESHM20 mean peak ground acceleration (PGA, units g), annual exceedance probability 0.002103 (approximately 10% in 50 years / 475-year return period), reference rock Vs30=800 m/s. This is long-term modelled shaking, not earthquake prediction, observed damage, local soil amplification or building resistance.; The model uses a 0.1-degree grid (roughly 9–11 km here). District values are area-weighted nearest-cell aggregates in UTM 36N. Administrative outlines locate the aggregates and do not imply street-level seismic precision.; Danciu et al. (2021), The 2020 update of the European Seismic Hazard Model: Model Overview, EFEHR Technical Report 001, doi:10.12686/a15. CC BY 4.0 https://creativecommons.org/licenses/by/4.0/; Safrom computed district aggregates and research scores. No EFEHR endorsement.