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Earthquake 3D provides a fascinating look at recent seismic activity around the globe. While the program provides a great deal of information and options, it suffers from its complete lack of direction. We were initially impressed with the interface. The controls all looked basic, but soon we discovered that the Help file didn't do more than give a description of the product, and some actions we wanted to perform were not intuitive enough. The program itself was a spinning globe with magnitudes and the traditional multiring circles indicating earthquakes. We appreciated how the control panel let us filter quakes by severity and changed the globe's look to better see the quakes.
This all functioned great, but zooming in was impossible. We learned with ease how to rotate the globe using our mouse, but could not get a closer look, even though it's the first thing the description promised. After several fruitless minutes we grew frustrated and gave up. On a more interesting note, the program did have a feature that updated the globe with the newest quakes. But this wasn't enough to rescue this program from its unfortunate lack of direction. Earthquake 3D is a freeware program. The program comes as a compressed file.
Appl Phys Lett 80:353–355 9. Thorsen T, Maerkl SJ, Quake SR (2002) Microfluidic Large Scale Integration. Zhou Z, Xu J, Cheng Y (2008) Surface-enhanced Raman scattering substrate fabricated by femtosecond laser direct writing.
Even though we loved most aspects of this program, its lack of direction makes it hard to recommend. Full Specifications What's new in version 2.92 Version 2.92 updates the program so that it can run on Linux computers using WINE. General Publisher Publisher web site Release Date February 02, 2017 Date Added February 09, 2017 Version 2.92 Category Category Subcategory Operating Systems Operating Systems Windows 98/Me/2000/XP/2003/Vista/Server 2008/7/8/10 Additional Requirements None Download Information File Size 1.23MB File Name equake3d.zip Popularity Total Downloads 122,992 Downloads Last Week 21 Pricing License Model Free Limitations Not available Price Free.
Large intraplate earthquakes in oceanic lithosphere are rare and usually related to regions of diffuse deformation within the oceanic plate. The 23 January 2018 M W 7.9 strike-slip Gulf of Alaska earthquake ruptured an oceanic fracture zone system offshore Kodiak Island.
Bathymetric compilations show a muted topographic expression of the fracture zone due to the thick sediment that covers oceanic basement but the fracture zone system can be identified by offset N-S magnetic anomalies and E-W linear zones in the vertical gravity gradient. Back-projection from global seismic stations reveals that the initial rupture at first propagated from the epicenter to the north, likely rupturing along a weak zone parallel to the ocean crustal fabric. The rupture then changed direction to eastward directed with most energy emitted on Aka fracture zone resulting in an unusual multi-fault earthquake. Similarly, the aftershocks show complex behavior and are related to two different tectonic structures: (1) events along N-S trending oceanic fabric, which ruptured mainly strike-slip and additionally, in normal and oblique slip mechanisms and (2) strike-slip events along E-W oriented fracture zones.
To explain the complex faulting behavior we adopt the classical stress and strain partitioning concept and propose a generalized model for large intra-oceanic strike-slip earthquakes of trench-oblique oriented fracture zones/ocean plate fabric near subduction zones. Taking the Kodiak asperity position of 1964 maximum afterslip and outer-rise Coulomb stress distribution into account, we propose that the unusual 2018 Gulf of Alaska moment release was stress transferred to the incoming oceanic plate from co- and post-processes of the nearby great 1964 M W 9.2 megathrust earthquake.
Some of the world’s largest earthquakes occur in Alaska, such as the great 1964 M W 9.2 earthquake (Fig. ). Most major and great earthquakes are related to rupture of the subduction megathrust. In contrast, many major earthquakes that occur in the oceanic lithosphere near subduction zones are usually bending-related outer-rise normal faulting earthquakes (e.g.,). Oceanic lithosphere strike-slip earthquakes near subduction zones are rare. Two major Pacific Plate N-S trending strike-slip earthquakes (Fig., upper right; M W 7.8/7.7 in 1987/1988) ruptured a composite length of ~250 km in the central Gulf of Alaska. This region has hosted a spatially persistent cluster of diffuse seismicity since then,, where complex N-S aftershock patterns dominate and additionally ENE – WSW trending aftershock clusters reactivated fracture zones (FZs). This cluster of seismicity resulted from a combination of enhanced tensional stress in the Pacific Plate following the 1964 great Alaska earthquake and compressional stress resulting from the collision of the Yakutat Terrane with North America.