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Remote sensing studies and morphotectonic investigations in an arid rift setting, Baja California, Mexico. The Gulf of California and its surrounding land areas provide a classic example of recently rifted continental lithosphere. Thus, extensional tectonics, bedrock lithology, long-term climatic changes, and evolving surface processes have controlled the tectono-geomorphological evolution of the eastern part of the peninsula since that time.

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In this study, digital elevation data from the Shuttle Radar Topography Mission SRTM from Baja California were corrected and enhanced by replacing artifacts with real values that were derived using a series of geostatistical techniques. The next step was to generate accurate thematic geologic maps with high resolution m for the entire eastern coast of Baja California. The main approach that we used to clearly represent all the lithological units in the investigated area was objectoriented classification based on fuzzy logic theory.

The area of study was divided into twenty-two blocks; each was classified independently on the basis of its own defined membership function. Overall accuracies were The third step of this study was to assess the factors that affected the geomorphologic development along the eastern side of Baja California, where thirty-four drainage basins were extracted from a m-resolution absolute digital elevation model DEM. Thirty morphometric parameters were extracted; these parameters were then reduced using principal component analysis PCA. Cluster analysis classification defined four major groups of basins.

We extracted stream length-gradient indices, which highlight the differential rock uplift that has occurred along fault escarpments bounding the basins. Also, steepness and concavity indices were extracted for bedrock channels within the thirty-four drainage basins. Geologic results are described here, while geochemical data used to divide the volcanic rocks into suites are described in an accompanying abstract1. Proximal alluvial fan bajada deposits are debris-flow dominated, with angular clasts up to 1. Distal braided stream deposits have sandstones and cobble conglomerates, with abundant cut and fill structures and rounded clasts.

Adakite trachyandesite block-and-ash-flow tuffs are interstratified with the proximal deposits, representing pyroclastic flows generated by collapse of lava domes plumbed up the basin-bounding fault to the east. The dikes and lava shields include calcalkaline basaltic andesite, andesite and dacite, as well as magnesian trachyandesite and basaltic andesite.

Bojorquez, Ietza; Barnes, Richard F.

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We sought to compare prevalence and determinants of multidrug-resistant tuberculosis MDR-TB between tuberculosis patients in Baja California, Mexico, and Hispanic patients in California. MDR-TB prevalence was 2. Possible explanations include different levels of exposure to resistant strains and inadequate treatment. Though it did not reproduce well, this photo gives scientific information to aid in studying all types of Earth's processes.

It documents ocean features in the sunglint in the Gulf of California, off the Isla Cerralvo, southern Baja , California. Biological oils collect on the surface of the water and take the form of the currents. The sun reflects off the oily surface and shows current patterns, eddies and ship wakes. The small bright spot on the edge of the eddy is a ship dumping oily water from its bilges. The line in the brighter area is a light wind gust roughening the surface.

STS March Though it did not reproduce well, this photo gives scientific information to aid in studying all types of earth's processes. It documents ocean features in the sunglint in the Gulf of California, off the Isla Cerralvo, souther Baja , California. Biological oils collect on the surface and shows current patterns, eddies and ship wakes.

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Whole genome sequencing of Mycobacterium bovis to obtain molecular fingerprints in human and cattle isolates from Baja California, Mexico. To determine genetic diversity by comparing the whole genome sequences of cattle and human Mycobacterium bovis isolates from Baja California.

A whole genome sequencing strategy was used to obtain the molecular fingerprints of isolates of M. Spoligotypes were characterized in silico and single nucleotide polymorphism SNP differences between the isolates were evaluated. A total of 12 M. Two predominant spoligotypes patterns were seen in both cattle and humans: SB and SB When evaluating SNP differences, the human isolates were intimately intertwined with the cattle isolates.

All isolates from humans had spoligotype patterns that matched those observed in the cattle isolates, and all human isolates shared common ancestors with cattle in Baja California based on SNP analysis. This suggests that most human tuberculosis caused by M.


These results reinforce the importance of bovine tuberculosis surveillance and control in this region. Published by Elsevier Ltd.. All rights reserved. In contrast to previous interpretations of the Rosario Formation in other parts of Baja California, a stratigraphic section 6 km north of Ensenada, Baja California, Mexico, contains evidences for deposition in shallow waters during a regressive event in a steep slope basin. Among the sedimentary evidence, the section shows a coarse, shoaling-upward sequence, with high-angle cross-stratification and planar bed lamination.

Load structures with a westward orientation were found only at the base. This sedimentologic and paleontologic evidence suggests nearshore to beach coastal deposits. The contact between the section and a discontinuous thin limestone bed at the top of the section shows an unconformity.

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The absence of well-preserved fossils makes this limestone difficult to date, but the lithology is similar to that of Paleocene Sepultura Formation limestones. Crustal and sub-crustal structure of northwestern Mexico peninsular California resulted from major accretion episodes occurred during the long-lived subduction of the Farallon plate beneath the North American plate, since late Jurassic time. A magnetotelluric profile across central Baja California reveals several electrical conductivity anomalies probably associated to the crustal boundaries of distinct Mezosoic terranes juxtaposed in the current peninsular crust.

It is known that electrical conductivity is significantly increased by the pervasive presence of conductive minerals generated during metamorphic processes in highly sheared zones. We interpret a striking sub-horizontal conductivity anomaly reveled in the model as explained by the presence of high-salinity fluids released after dehydration of the subducted Magdalena microplate Farallon plate?

The presence of fluids at the base of the peninsular crust may produce a zone of weakness, which supports the idea that Baja California lithosphere has not been entirely coupled to the Pacific plate. In addition, crustal thickness is estimated in our model in about 35 km beneath the western Peninsular Ranges batholith PRB and 20 km beneath the eastern PRB. This crustal thickness is in good agreement with independent estimations of a thinner crust in the Gulf of California margin and a thicker crust along the axial PRB. Bradley; Fisher, Robert N.

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Chytridiomycosis is caused by the fungal pathogen Batrachochytrium dendrobatidis Bd and is regarded as one of the most significant threats to global amphibian populations. We visited 33 localities and swabbed wild-caught anurans from 7 species 5 native, 2 exotic across the Mediterranean region of the state of Baja California.

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Using quantitative PCR, Bd was detected in 94 individuals The exotic Xenopus laevis was the only species that tested completely negative for Bd. We found that remoteness, distance to agricultural land, and elevation were the best predictors of Bd presence. Tectonic analysis of Baja California and Parras shear belt in Mexico. The author has identified the following significant results. ERTS-1 imagery was used to check the validity of the existence of major trans- Baja fault zones. ERTS-1 imagery also shows that high albedo sediments similar to known late Tertiary marine sediments are widespread in southern and middle Baja and extend in places to the eastern side of the Peninsula.

Major faults in northern Mexico and across the border in the United States were mapped, and ample evidence was found that the Parras and parts of the Texas lineament are belts of major transverse shear faults in areas outside the supposed limit of the Texas and Parras lineaments.

A fundamental concept which may help explain many complexities in the tectonic development is beginning to emerge: The southwestern part of North America was torn by massive left-lateral shear of transverse trend east-west during the compressive stage of the late Mesozoic and early Cenozoic. This tectonic style has changed into tensional rifting Basin and Range and right-lateral shear later in the Cenozoic and Quaternary.

Michaud, F. The pioneering work on spreading-ridge subduction Dickinson and Snyder, describes the evolution of slab geometry beneath southwestern US and northwestern Mexico since the Middle Miocene. This work develops the slab-window concept and the tectonic and magmatic effects of the slab-free geometry on the Cordilleran system.

This area exhibits the effects of slab-free development on the time distribution of magmatism and tectonism within the overriding continental block. Moreover, recent fieldwork conducted along the southern Baja California volcanic belt supports that slab melting under relatively shallow and warm conditions occurred during Upper Miocene time. When combined with the Miocene-Recent volcanic record of Baja California, a parallel drawn between the Chile and Mexico triple junction areas substantiates slab window development beneath southern Baja California peninsula during the past m. Also, three magnetic deep-tow profiles were performed to provide a higher resolution of the magnetic signal and age of the corresponding oceanic crust.

This document includes the text of presentations given at the First Binational Conference on Libraries in California and Baja California, as well as minutes from four roundtables held at the conference. Following a prologue and a brief background on the conference, the following presentations are included: 1 "State Support for Public…. The archaeology of the Pericue Indians inhabiting the Cape region of Baja California has long been an area of interest. The dolichocranic traits exhibited by this population have lead to suggestions that these people were a relic population of an early coastal migration into North America.

The antiquity of directly dated Pericue human remains only reaches 3, B.