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Smith College

2012

Articles 1 - 7 of 7

Full-Text Articles in Geology

Geodetic Constraints On San Francisco Bay Area Fault Slip Rates And Potential Seismogenic Asperities On The Partially Creeping Hayward Fault, Eileen L. Evans, John P. Loveless, Brendan J. Meade Mar 2012

Geodetic Constraints On San Francisco Bay Area Fault Slip Rates And Potential Seismogenic Asperities On The Partially Creeping Hayward Fault, Eileen L. Evans, John P. Loveless, Brendan J. Meade

Geosciences: Faculty Publications

The Hayward fault in the San Francisco Bay Area (SFBA) is sometimes considered unusual among continental faults for exhibiting significant aseismic creep during the interseismic phase of the seismic cycle while also generating sufficient elastic strain to produce major earthquakes. Imaging the spatial variation in interseismic fault creep on the Hayward fault is complicated because of the interseismic strain accumulation associated with nearby faults in the SFBA, where the relative motion between the Pacific plate and the Sierra block is partitioned across closely spaced subparallel faults. To estimate spatially variable creep on the Hayward fault, we interpret geodetic observations with …


Response Of A Carbonate Platform To The Cenomanian-Turonian Drowning And Oae 2: A Case Study From The Adriatic Platform (Dalmatia, Croatia), Tvrtko Korbar, B. Glumac, Blanka Cvetko Tesovic, Sarah B. Cadieux Mar 2012

Response Of A Carbonate Platform To The Cenomanian-Turonian Drowning And Oae 2: A Case Study From The Adriatic Platform (Dalmatia, Croatia), Tvrtko Korbar, B. Glumac, Blanka Cvetko Tesovic, Sarah B. Cadieux

Geosciences: Faculty Publications

Global perturbations during the Cenomanian–Turonian boundary (CTB) interval and the Oceanic Anoxic Event 2 (OAE 2) represent one of the most extensively studied past environmental changes. To explore the response of various carbonate-platform depositional systems to such major environmental perturbations, strata of the intra-Tethyan Adriatic carbonate platform (sensu stricto) from the island of Bracˇ (Adriatic Sea, Croatia) provide excellent exposures and a previously well-established Upper Cretaceous lithostratigraphic framework. Within this context, this study integrated lithostratigraphy, biostratigraphy, and chemostratigraphy to describe a drowned-platform succession underlain and overlain by peritidal carbonates. Carbon-isotope stratigraphy of this succession revealed a shift towards positive d13C …


Geology Of New Providence Island, Bahamas: A Field Trip Guide, John E. Mylroie, James L. Carew, H. Allen Curran, Fabienne Godefroid, Pascal Kindler, Neil E. Sealey Jan 2012

Geology Of New Providence Island, Bahamas: A Field Trip Guide, John E. Mylroie, James L. Carew, H. Allen Curran, Fabienne Godefroid, Pascal Kindler, Neil E. Sealey

Geosciences: Faculty Publications

See other Smith authored Field Trip Guides of Gerace Research Centre.


Unusual Holocene Serpulid-Tufu Bioherms, Enriquillo Valley, Dominican Republic: Morphologies And Paleoenvironmental Implications, Kelsey Winsor, H. Allen Curran, Lisa Greer, Bosiljka Glumac Jan 2012

Unusual Holocene Serpulid-Tufu Bioherms, Enriquillo Valley, Dominican Republic: Morphologies And Paleoenvironmental Implications, Kelsey Winsor, H. Allen Curran, Lisa Greer, Bosiljka Glumac

Geosciences: Faculty Publications

During the early Holocene, rising waters of the Caribbean Sea flooded the Enriquillo Valley of southwestern Dominican Republic. A fringing coral reef developed and flourished along the margins of the Enriquillo Seaway for several millennia, until the seaway became restricted due to a combination of slowed sea-level rise, tectonic uplift, and increased sedimentation. Following changes in salinity and death of the coral reef by about 5 ka, meter-scale bioherms composed of the tubes of opportunistic, aggregating serpulid worms and associated with carbonate tufa that precipitated from the ancient lake or declining seaway waters formed along the steep walls of the …


Recovery Of Carbonate Sand Beaches On San Salvador Island, Bahamas From Damage By Hurricane Frances (2004), H. Allen Curran, Mia Schultz-Baer, Kathryn Durkin, Bosiljka Glumac Jan 2012

Recovery Of Carbonate Sand Beaches On San Salvador Island, Bahamas From Damage By Hurricane Frances (2004), H. Allen Curran, Mia Schultz-Baer, Kathryn Durkin, Bosiljka Glumac

Geosciences: Faculty Publications

East Beach and Hanna Bay Beach, located on the northeast coast of San Salvador, were two of the island's beaches most heavily impacted by Hurricane Frances (category 3) on September 2, 2004. A maximum storm surge of 3.1 m was reported for East Beach, with erosion occurring up to 70 m inland from the wave-break line and resulting in scarps cut into dunes of up to 1.5 m height. In January 2005, 5 beach profile stations along 1 km of East Beach and 3 stations along Hanna Bay Beach were established to monitor long-term coastal recovery from hurricane damage. East …


Distribution Of Oolitic Sediment Along A Beach-To-Offshore Transect, Pigeon Cay, Cat Island, Bahamas: New Insights Into Modern Ooid Formation, Bosiljka Glumac, H. Allen Curran, Madeline M. Weigner, Sarah A. Motti, Sara B. Pruss Jan 2012

Distribution Of Oolitic Sediment Along A Beach-To-Offshore Transect, Pigeon Cay, Cat Island, Bahamas: New Insights Into Modern Ooid Formation, Bosiljka Glumac, H. Allen Curran, Madeline M. Weigner, Sarah A. Motti, Sara B. Pruss

Geosciences: Faculty Publications

Ooids are a common component of ancient carbonate rocks, but their origin and distribution in Holocene deposits and modem carbonate sands are not fully understood. Even though ooids are well documented from several localities in the Bahamian Archipelago, their occurrence on Cat Island has not been previously studied in detail. In this study we examined the composition and texture of beach sand and six sediment samples collected from the sea floor at approximately 50-meter intervals along an estimated 300 m transect at Pigeon Cay, Cat Island.


Possible Early Foraminiferans In Post-Sturtian (716-635 Ma) Cap Carbonates, Tanja Bosak, Daniel J.G. Lahr, Sara B. Pruss, Francis A. Macdonald, Andrew J. Gooday, Lilly Dalton, Emily D. Matys Jan 2012

Possible Early Foraminiferans In Post-Sturtian (716-635 Ma) Cap Carbonates, Tanja Bosak, Daniel J.G. Lahr, Sara B. Pruss, Francis A. Macdonald, Andrew J. Gooday, Lilly Dalton, Emily D. Matys

Geosciences: Faculty Publications

Foraminifera are an ecologically important group of modern heterotrophic amoeboid eukaryotes whose naked and testate ancestors are thought to have evolved ~1 Ga ago. However, the single-chambered agglutinated tests of these protists appear in the fossil record only after ca. 580 Ma, coinciding with the appearance of macro scopic and mineralized animals. Here we report the discovery of small, slender tubular microfossils in the Sturtian (ca. 716-635 Ma) cap carbonate of the Rasthof Formation in Namibia. The tubes are 200-1300 μm long and 20-70μm wide, and preserve apertures and variably wide lumens, folds, constrictions, and ridges. Their sometimes fl exible …