1,618 research outputs found
Strategic Communications for Influence: Lessons From the Annie E. Casey Foundation and Its KIDS COUNT Initiative
No full text· This article describes how the Annie E. Casey Foundation is using the KIDS COUNT Network in a new way: as a strategic communications tool in its focused efforts toward policy change, broad social change, and improved conditions for vulnerable children and families. An outcome map illustrates links between this strategy and the intended outcomes.
· Case illustrations of KIDS COUNT grantee activities surrounding the release of the 2008 KIDS COUNT Data Book describe the efforts of grantees in six states where the quantity and quality of media coverage surrounding the national data book reflected the kind of coverage that Casey believes will help achieve its desired outcomes.
· Strategic communications approaches such as relationships with journalists, use of locally relevant information, use of locally relevant media advocacy strategies, good preparation, and a solution orientation were present in states demonstrating desirable media coverage.
· Prescribing specific communications tactics matters less than supporting the network’s general capacity to engage in year-round strategic communications approaches to create conditions (e.g., reputations, relationships) that will contribute to successful media advocacy related to a specific event such as the release of the national data book
African American Storyteller, Victoria A. Casey McDonald
No full textIn the deep resonance of storyteller Victoria A. Casey McDonald’s voice, you will hear her tell stories about growing up in Western North Carolina, and the kind of Christmas she had as a child. The late Victoria was our friend, a CSA board member, author, and “Stories of Mountain Folk” interviewer
Peer Networking and Community Change: Improving Foundation Practice
No full text· This article brings together the Annie E. Casey Foundation’s 15 years of experience with peer networking— examining through two research studies the process of peer networking and its impact, both with community-based and funder groups.
· Peer networking helps people with common interests to exchange information, disseminate good practices, and build a leadership structure for work they do together, such as a community change initiative.
· Casey’s research identified 10 good practices for effective peer networking, as well as 10 challenges that can affect its success; a four-level model was created to provide context for these findings.
· The research indicates that peer networking can have significant impact for communities and in meeting philanthropic goals, but it is costly and must be carefully structured if it is to be successful.
· Casey is working to synthesize its peer networking practices into a more strategic framework, and other foundations might use some of its lessons learned to enhance their own practices in this area
The Family History of Casey Christall
No full textCasey Christall authored this family history as part of the course requirements for HIST 550/700 Your Family in History offered online in Spring 2020 and was submitted to the Pittsburg State University Digital Commons. Please contact the author directly with any questions or comments: [email protected]
Fluid-rich damage zone of an ancient out-of-sequence thrust, Kodiak Islands, Alaska
No full textThe Uganik Thrust is a fossil out-of-sequence thrust fault which was active over a period of 3 Ma during the early Tertiary until activity ceased with the subduction of the Kula-Farallon spreading ridge at 57 Ma. During this period the fault experienced at least 1 km of throw and developed a strongly asymmetric damage zone. The brittle damage zone in the footwall of the fault acted as a conduit for fluid advection during the active faulting. A similar asymmetrical footwall damage zone has been interpreted as a fluid conduit at the Nobeoka Thrust, Shimanto Belt, SW Japan. Thermal indicators in the uppermost footwall give similar maximum paleotemperatures to those in the hanging wall (280C), while previous work elsewhere in the footwall formation suggests maximum burial temperatures of 240C. In this case, similar to the Irish Canyon thrust in the Franciscan accretionary complex, the location of the thermal anomaly is spatially offset from the structural fault which caused it owing to thermal overprinting in the vicinity of the fault
Textural record of the seismic cycle: Strain rate variation in an ancient subduction thrust
No full textActive faults slip at different rates over the course of the seismic cycle: earthquake slip (c. 1ms21), interseismic creep (c. 10–100 mm year21) and intermediate rate transients (e.g. afterslip and slow slip events). Studies of exhumed faults are sometimes able to identify seismic slip surfaces by the presence of frictional melts, and slow creep by textures diagnostic of rate-limited plastic processes. The Pasagshak Point Thrust preserves three distinct fault rock textures, which are mutually cross-cutting, and can be correlated to different strain rates. Ultrafine-grained black fault rocks, including pseudotachylyte, were formed during seismic slip on layers up to 30 cm thick. Well-organized S–C cataclasites 7–31 m thick were formed by slow creep, with pressure solution as a dominant, rate-limiting mechanism. These must have formed at strain rates consistent with long-term plate-boundary motion, but solution-creep healing acted to reduce porosity of the cataclasites and eventually restricted fluid connectivity such that creep by this mechanism could not continue. Disorganized, non-foliated, rounded clast cataclasites were formed at shear rates faster than solution creep and are interpreted as representing shear at intermediate strain rates. These could have formed during afterslip or delocalization of slip associated with an earthquake rupture
How Accretionary Prisms Elucidate Seismogenesis in Subduction Zones
No full textEarthquakes occur along the plate-boundary thrusts underlying accretionary prisms and along out-of-sequence thrusts that cut through prisms. Thermal models suggest that the earthquakes on the plate-boundary thrusts initiate in a temperature range of 125oC to ~350oC. Because syndeformational diagenetic and metamorphic alterations recorded in accretionary prisms have specific temperature ranges, the alterations and the associated deformation can be correlated to the temperature range that accretionary prisms are seismogenic. Comparison of accreted rocks deformed above, within, and below the seismogenic zone suggests characteristics of rocks at seismogenic depths that may make them earthquake prone. During passage through temperatures from 50o to 150oC, accretionary prism sediments become rocks, undergoing diagenetic reactions including the transformation of smectite to illite, albitization of detrital feldspar, dehydration of opal, and the generation of hydrocarbons. Although the smectite to illite transition does not change the frictional properties of the prism so that it becomes seismogenic, water and cations (calcium, magnesium, iron) released during this transition and the albitization process foster cementation. Cementation and veining by carbonates becomes common by 125oC, perhaps due to the above-mentioned release of cations. Pressure solution fabrics begin to be apparent at ~150oC, with well-developed cleavages and quartz veining common by 200oC. Pressure solution may be facilitated by the diagenetic formation of illite. Quartz veining and cementation in the 150o–300oC range facilitates the change from a velocity-strengthening, clay dominated to a velocity-weakening, quartz-influenced, earthquake-prone rheology. The diagenetic-metamorphic reactions occurring at temperatures from 125o to ~300oC cement and add rigidity to the thickening upper plate of the accretionary prism. This developing elastic strength of the upper plate is required to store the elastic strain energy required for an earthquake. In accretionary prisms, brittle fabrics are progressively replaced by ductile fabrics through a temperature range of ~150o– 325oC. Although rocks in the seismogenic zone have lost most of their intergranular fluid through consolidation, vein geometries and fluid inclusions suggest high fluid pressures, approaching lithostatic. Strain localization in the form of discrete shear surfaces occurs across the lower aseismic to seismic transition. Strain localization is observed both at outcrop and map scale. At map scale, the seawardmost occurrence of out-of-sequence thrusts define the leading edge of the rigidified accretionary prism that is capable of storing elastic energy
2012 Marguerite Casey Foundation Annual Report: Young Movement Builders
No full textThis year's annual report profiles the 12 inaugural "Youth Poverty Warriors," each of whom exemplifies Shriver's and the foundation's belief that youth can fundamentally change society for the better
Juvenalia, or How I came to own a Blu-Ray of Point Break
No full textAgony Klub and Publication Studio Vancouver are pleased to present Whitney Houston, vol. 2. A continuation of Whitney Houston, et. al., editor/author Casey Wei invites six writers to reflect on their relationship to popular music in film, keeping in mind that popular music has always been as much about the desire for an image as about the catchiness of a song. The resulting essays on Elliot Smith, Amélie, Real Genius, The Pixies, Drive, and The Conversation explore themes of time, love, and evolution.final article publishedReal Genius (1985
Glaciology Data Report, Casey 1981
No full textProgress Code: completedA collection of the data from the 1981 Glaciology program at Casey, collected from several inland traverses. Measurements include accumulation and density, barometric profiling, ice movement, gravity, ice thickness and bedrock profiling, temperatures at 10m depth, surface density, and oxygen isotopes.<br/><br/>These documents have been scanned and are available for download from the provided URL. The dataset download contains the following file:<br/><br/>Glaciology Data Report Casey 1981.pd
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