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Denali Park M 1.6 | Alaska Earthquake Center
18 Jun 2024 07:39:56 AKDT (18 Jun 2024 15:39:56 UTC)63.6290°N 148.6014°W, depth 0.6 mi (0 km)
This event has not been reviewed by a seismologist
19 miles (30 km) SE of Healy 20 miles (32 km) NE of Cantwell 52 miles (84 km) S of Clare 66 miles (107 km) S of Nenana 73 miles (118 km) E of Kantishna 77 miles (124 km) SW Salcha 83 miles (134 km) southwest of Pump Station # 885 miles (137 km) southwest of Eielson AFB 86 miles (139 km) south of Ester 86 miles (139 km) southwest of Arctic 88 miles (142 km) south of Fairbanks 172 miles ( 278 km) N Anchorage Type: Event Magnitude: Ml2 Event Type: Tectonic Earthquake Setting of the Denali Fault The Denali Fault is a large right-sided intracontinental strike-slip fault that partially accommodates the oblique collision of the Yakutat Massif in the Alaskan margin, extending from northwestern to central British Columbia and areas Western Alaska. The largest earthquake ever recorded on the Denali fault was a M7.9 on November 3, 2002. Its rupture extended about 270 miles (435 km) along the central Denali fault system. This event was preceded by the M6.7 Mount Nenana earthquake on October 23, which ruptured a 25 mi (40 km) section of the Denali fault west of the M7.9 event. The typical behavior of these major right-sided faults in the interior is to produce very low background levels of seismicity between large faults hundreds of years apart and followed by multi-year aftershock sequences. Another notable feature associated with the Denali Fault System is the Kantishna Seismic Group, which lies north of the main fault path within Denali National Park. This group produces dozens of small, shallow earthquakes every day. The largest known earthquakes in this group are magnitude 5, but they are rare. This group is thought to accommodate deformation between the Denali fault and the Minto Flats seismic zone to the north.
Sources 2/ https://earthquake.alaska.edu/event/0247teizbj The mention sources can contact us to remove/changing this article |
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