安塔利亞
選擇一個城市
數字是全球統一尺度的研究估算;R 代表研究中。所有內容均非旅遊建議。
看看這裡怎麼樣
找到心儀的飯店了?訂房前,先看看周邊區域。
搜尋服務政策
點選搜尋會把查詢內容與所選城市傳送給 OpenStreetMap Nominatim,請勿輸入私人住址或敏感資訊。 搜尋服務政策
數字是全球統一尺度的研究估算;R 代表研究中。所有內容均非旅遊建議。
找到心儀的飯店了?訂房前,先看看周邊區域。
點選搜尋會把查詢內容與所選城市傳送給 OpenStreetMap Nominatim,請勿輸入私人住址或敏感資訊。 搜尋服務政策
出發前,先瞭解
有來源的研究估算;當地覆蓋不完整,部分維度沿用更廣地理範圍的基線。
城市研究估算為 68/100;模型尺度上分數越高越安全。 證據日期: · 信賴度: D
研究估算:區域僅調整有當地證據的一個維度,其他維度沿用城市或國家基線。 空白處缺少區域證據,不代表安全。
5 個已映射區域 ·
邊界資料: OpenStreetMap contributors · Five Antalya central districts (ODbL 1.0; © OpenStreetMap contributors)
城市估算不能評估某條街道、某家飯店或特定時段。
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.