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土耳其
安塔利亚
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数字是全球统一尺度的研究估算；R 表示研究中。所有内容均非旅行建议。
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非常安全
较安全
谨慎
高风险
很高风险
极端风险
安塔利亚: 68
数字是全球统一尺度的研究估算；R 表示研究中。所有内容均非旅行建议。
找到心仪的酒店了？订房前，先看看周边区域。
点击搜索会把查询内容和所选城市发送给 OpenStreetMap Nominatim，请勿输入私人住址或敏感信息。 搜索服务政策
出发前，先了解
有来源的研究估算；本地覆盖不完整，部分维度沿用更广地理范围的基线。
城市研究估算为 68/100；模型尺度上分数越高越安全。 证据日期: · 置信度: D
研究估算：区域仅调整有当地证据的一个维度，其他维度沿用城市或国家基线。 空白处缺少区域证据，不代表安全。
5 个已映射区域 ·
边界数据: OpenStreetMap contributors · Five Antalya central districts (ODbL 1.0; © OpenStreetMap contributors)
城市估算不能评估某条街道、某家酒店或特定时段。
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.