Fox M 1.3 | Alaska Earthquake Center

31 Dec 2024 15:06:54 AKST (1 January 2025 00:06:54 UTC)64.9854°N 147.4322°W, depth 1.9 mi (3 km)

This event has not been reviewed by a seismologist

9 miles (14 km) south of Chatanica 11 miles (17 km) northeast of Fort Wainwright 13 miles (21 km) northeast of Fairbanks 16 miles (25 km) north of North Pole 20 miles (32 km) northeast of Esther 24 miles (38 km) ) Northwest of Eielson AFB33 miles (53 km) Southeast of Pumping Station #736 miles (58 km) Northwest of Pumping Station #837 miles (59 km) North of Salcha 49 miles (79 km) Southeast of Livengood 57 miles (92 km) East of Minto 271 miles (439 km) North of Anchorage Strength Type: Ml2 Event Type: Tectonic Earthquake Interior Alaska Setting Earthquakes in Alaska reflect transmission and mass Rotation. Three different types of tectonic structures contribute to the generation of earthquakes in this region: right-slip faults (Denali, Tintina, Kaltag), north-northeast-trending seismic zones (Minto, Fairbanks, Salcha, Dal City, Rampart), and slope faults. North of the Alaska Range. The largest event ever recorded in the interior was the M7.3 Salcha earthquake of 1937. It produced widespread landslides in the central region, but there was no documented evidence of surface rupture. Other notable events include the 1968 M7.1 Rampart earthquake, the 1985 M6.1 Dall City earthquake, and the 1995 M6.0 Minto Flats earthquakes. The Fairbanks Seismic Zone was the site of three M5-6 earthquakes in 1967. An M7 thrust event occurred 2. In 1947 at the leading edge of the northern slopes of the Alaska Range and south of the Salcha seismic zone. This event, combined with current seismic activity, indicates ongoing thrust deformation on the north side of the Central Alaska Range. East of 146°W longitude, seismic activity between the Tintina fault to the north and the Denali fault to the south decreases dramatically.

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