Contemporary Seismicity in and Around the Yakima Fold-and-Thrust Belt in Eastern Washington

We examined characteristics of routinely cataloged seismicity from 1970 to the present in and around the Yakima fold-and-thrust belt (YFTB) in eastern Washington to determine if the characteristics of contemporary seismicity provide clues about regional-scale active tectonics or about more localized, near-surface processes. We employed new structural and hydrologic models of the Columbia River basalts (CRB) and found that one-third to one-half of the cataloged earthquakes occur within the CRB and that these CRB earthquakes exhibit significantly more clustered, and swarmlike, behavior than those outside. These results and inferences from published studies led us to hypothesize that clustered seismicity is likely associated with hydrologic changes in the CRB, which hosts the regional aquifer system. While some general features of the regional groundwater system support this hypothesis, seismicity patterns and mapped long-term changes in groundwater levels and present-day irrigation neither support nor refute it. Regional tectonic processes and crustal-scale structures likely influence the distribution of earthquakes both outside and within the CRB as well. We based this inference on qualitatively assessed alignments between the dominant northwest trends in the geologic structure and the seismicity generally and between specific faults and characteristics of the 2009 Wooded Island swarm and aseismic slip, which is the only cluster studied in detail and the most vigorous since regional monitoring began.USGS-NAGTGeological Science

Civil Practice and Procedure

This article surveys recent significant developments in Virginia civil practice and procedure. Part I of this article discusses opinions of the Supreme Court of Virginia from June 2013 through June 2014 addressing noteworthy civil procedure topics. Part II addresses amendments to the Rules of the Supreme Court of Virginia concerning procedural issues during the same period. PartIII discusses legislation enacted by the Virginia General Assembly during its 2014 session that relates to civil practice

Civil Practice and Procedure

This article surveys recent significant developments in Virginia civil practice and procedure. The article discusses opinions of theSupreme Court of Virginia from June 2012 through June 2013 addressing civil procedure topics, significant amendments to the Rules of the Supreme Court of Virginia concerning procedural issues during the same period, and legislation enacted by the Virginia General Assembly during its 2013 session that relates to civil practice

Effects of Various Processing Temperatures on the Utilization of Solvent-Extracted Soybean and Cottonseed Meals by Sheep

Animal Nutritio

Influence of the megathrust earthquake cycle on upper-plate deformation in the Cascadia forearc of Washington State, USA

The influence of subduction zone earthquake cycle processes on permanent forearc deformation is poorly understood. In the Cascadia subduction zone forearc of Washington State, USA, deformed and incised fluvial terraces serve as archives of longer-term (103–104 yr) strain manifest as both fluvial incision and slip on upper-plate faults. We focus on comparing these geomorphic records in the Wynoochee River valley in the southern Olympic Mountains with short-term (101 yr) deformation driven by interseismic subduction zone coupling. We use optically stimulated luminescence dating and high-resolution elevation data to characterize strath terrace incision and differential uplift across the Canyon River fault, which cuts Wynoochee River terraces. This analysis demonstrates reverse slip rates of ∼0.1–0.3 mm/yr over the past ∼12–37 k.y., which agree with rates predicted by a GPS-constrained boundary element model of interseismic stress from Cascadia subduction zone coupling. Similarly, model-predicted patterns of interseismic uplift mimic the overall pattern of incision in the lower Wynoochee River valley, as revealed by strath elevations dated at 14.1 ± 1.2 ka. Agreement between modeled short-term and observed long-term records of forearc strain suggests that interseismic stress drives slip on upper-plate faults and fluvial incision in Cascadia. Consistency over multiple time scales may indicate relative stability in spatial patterns of subduction zone coupling over at least ∼104 yr intervals

Is the central-marginal hypothesis a general rule? Evidence from three distributions of an expanding mangrove species, Avicennia germinans (L.)

The central-marginal hypothesis (CMH) posits that range margins exhibit less genetic diversity 16 and greater inter-population genetic differentiation compared to range cores. CMH predictions 17 are based on long-held ‘abundant-centre’ assumptions of a decline in ecological conditions and 18 abundances towards range margins. Although much empirical research has confirmed CMH, 19 exceptions remain almost as common. We contend that mangroves provide a model system to 20 test CMH that alleviates common confounding factors and may help clarify this lack of 21 consensus. Here, we document changes in black mangrove (Avicennia germinans) population 22 genetics with 12 nuclear microsatellite loci along three replicate coastlines in the United States 23 (only 2 of 3 conform to underlying ‘abundant-centre’ assumptions). We then test an implicit 24 prediction of CMH (reduced genetic diversity may constrain adaptation at range margins) by 25 measuring functional traits of leaves associated with cold tolerance, the climatic factor that 26 controls these mangrove distributional limits. CMH predictions were confirmed only along the 27 coastlines that conform to ‘abundant-centre’ assumptions and, in contrast to theory, range margin 28 A. germinans exhibited functional traits consistent with greater cold tolerance compared to range 29 cores. These findings support previous accounts that CMH may not be a general rule across 30 species and that reduced neutral genetic diversity at range margins may not be a constraint to 31 shifts in functional trait variation along climatic gradients