Henry C. “Hank” Smith and the Cross B Ranch: The First Stock Operation on the South Plains by M. Scott Sosebee

2022 ◽  
Vol 125 (3) ◽  
pp. 322-323
Author(s):  
Michael M. Miller
Keyword(s):  
1941 ◽  
Vol 7 (1) ◽  
pp. 68-68 ◽  
Author(s):  
Douglas S. Byers

In the recently published paper Two Sites on Martha's Vineyard, the section devoted to the Squibnocket Cliff site included speculation as to the manner of accumulation of the midden deposit, and included a statement that of the portion of the site remaining, the most complicated in structure lay near the edge of the cliff. It was further implied that the center of the deposit had vanished into the sea, and that only the outer fringes remained.Doubtless these passages created an impression that the authors felt that there was a center of occupation on which the site grew up, perhaps not in concentric layers, for it was specified that horizontal overlapping of strata occurred, but in eccentric overlapping layers. Certainly the cross section through the site shown in our Fig. 13 suggests that the center of occupation had been in the south end of the trench, shown in the upper part of the figure.


2021 ◽  
Author(s):  
Pilar Clariana ◽  
Ruth Soto ◽  
Conxi Ayala ◽  
Aina Margalef ◽  
Antonio Casas-Sainz ◽  
...  

<p>The characterization of the basement architecture of the Pyrenean Axial Zone, backbone of the chain, is crucial to understand its geodynamic evolution and the interplay between tectonism and magmatism. In this work, a new gravity-constrained cross section was built along the Central Pyrenees, between two of the largest Pyrenean Late Variscan granitic complexes, La Maladeta and Andorra-Mont Louis granites, to infer the geometry at depth of the basement host rocks. This cross section is ca. 65 km long and extends from the Mesozoic Bóixols basin in the South to the Late Variscan Bassiès granite to the North, close to the northern end of the Axial Zone. It is based on available geological maps, previous published works and new geological field data; together with newly acquired gravimetric stations (1141), to improve the existent spatial resolution of the gravity data from the databases of the Spanish and Catalan Geological Surveys, and density values from 65 rock samples covering all different lithologies in the cross section. Thus, its geometry at depth is constrained by means of an integrated 2.5D gravity/structural/petrophysical modelling.</p><p>The La Maladeta and Andorra-Mont Louis granites appear aligned in a WNW-ESE direction and both lie within the same Alpine basement unit, the Orri thrust sheet. They are separated about 40 km by the WNW-ESE-oriented Llavorsí syncline, formed by Devonian and Silurian rocks and limited to the north and south by south vergent thrusts. This syncline is located between two large Cambro-Ordovician anticlinorium structures, the La Pallaresa and Orri massifs to the north and south respectively, formed by a monotonous alternation of shales and sandstones with some intercalations of limestones and conglomerates affected by very low to medium grade of metamorphism. Most structures show southern vergence along the cross section, and its southern part is characterized by the occurrence of Triassic evaporites, a significant detachment level decoupling deformation between the Paleozoic basement and the Mesozoic-Cenozoic cover rocks.</p><p>The observed residual anomaly along the cross section shows a relative maximum, coinciding with the southern edge of the Axial Zone (Nogueras Zone) and southern half of the Orri massif, followed to the north by a relative large minimum. This gravity minimum in the core of the Axial Zone coincides with the northern half of the Orri massif, the Llavorsí syncline and southern half of the La Pallaresa massif and must be related at depth with rocks of lower density with respect to rocks located to the North and South. Two possible solutions have been postulated to explain the presence of lower density rocks: (i) the presence of Triassic evaporites at depth as a continuation to the North of the Triassic evaporites outcropping in the Rialp window located to the South and/or (ii) the presence of buried granitic bodies equivalent to the adjacent La Maladeta and Andorra-Mont Louis granites.</p>


2010 ◽  
Vol 56 (No. 6) ◽  
pp. 292-300 ◽  
Author(s):  
J. Husák

The paper is focused on the problems of the cross-border cooperation and the regional policy of the European Communities and the implementation of theoretical issues in the South Bohemia Region. The main aim of this paper is to compare the cross-border cooperation and its influence on the regional development of the South Bohemia Region between the 2004–2006 programming period (after the accession of the Czech Republic to the European Communities) and the 2007–2013 programming period. The paper also provides the typology of the realised cross-border projects from the perspectives of the number of projects and also their financial allocation. The results document the increasing importance of the cross-border cooperation and its highly positive impact on the social and economic development of the South Bohemia Region.


Author(s):  
Olaf Zenker

Political projects of belonging are concerned with sentiments of being ‘at home’ within specific collectivities, rooted in entanglements of people’s social locations, narratives of identification, and value regimes at varying intersections. Global history attests to the numerous ways in which modes of belonging have been juridified and legally restricted, and how legal categories have become populated and turned into markers of identity, thus revealing the politics of belonging as a normative project par excellence. In the shadows of accelerating globalization, recent decades have brought about an ever-diversifying and heavily contested multitude of identity politics, in light of which the time-honoured politics of belonging is bound to persist as a crucial concern for law and anthropology in the twenty-first century. Charting the contours of this complex terrain, this chapter engages with citizenship as an arguably still dominant, if not hegemonic, political identity as well as with alternative political projects of belonging. Zooming in on closely related territorial modes of belonging—ethnicity, nationhood/nationalism, diaspora, indigeneity, identities conventionally described as ‘autochthony’, and citizenship—it proposes an overarching framework of ‘contested autochthonies’ which allows the cross-cutting constructions of individual-territory-group triads, and their mutual interactions, to be studied at shifting scales. Against the backdrop of a case study of conflicting autochthonies in the South African postcolony, the chapter concludes by highlighting the close interdependencies between the (re)production of distributed senses of belonging and the attendant (re)distribution of belongings—and thus the need for an integrated analysis of recognition and (re)distribution in the politics of belonging.


1952 ◽  
Vol 15 (1) ◽  
pp. 34-36
Author(s):  
W. Everett Eakin

Sanitary conditions in farm buildings where milk is produced may be improved by replacing present multipaned windows with larger units of insulating glass which better transmit the light rays of the sun. The cross bars in present windows serve as chaff and dust collectors and also hold moisture that condenses on single glass. By using larger window areas in the south wall it is possible to use the heat rays of the winter sun for additional warmth. An overhang will shade out the hot summer sun, helping to keep interiors cooler.


2019 ◽  
pp. 171-194
Author(s):  
Adrian Favell ◽  
Janne Solgaard Jensen ◽  
David Reimer

The chapter introduces the cross-national comparative material offered by the qualitative interviews conducted in the EUMEAN survey. Building on Juan Díez Medrano’s study (2003) of how Europe is framed differently by Germans, Spanish and British, the chapter focuses on the discussions about mobility and cross-border experiences of residents of the five West European countries in EUCROSS (i.e., also adding Denmark and Italy in comparative terms). Taking the confident identities of Danes in Europe as its reference point, it contrasts the less experienced but sometimes more idealist points of view of Spanish and Italians, with the more doubtful voices of Germans and British. Tensions in their cross-border relations also surface, particularly between the privileged North-West of the continent and the South.


2013 ◽  
Vol 39 (3-4) ◽  
pp. 107 ◽  
Author(s):  
Isabelle Séguy ◽  
Nicolas Bernigaud ◽  
Arnaud Bringé ◽  
Michel Signoli ◽  
Stéfan Tzortzis

At the beginning of the 18th century, the Provence region was hit by several severe epidemics whose causes are still not clearly understood.To draw up epidemic profiles and to identify the pathogenic agents concerned, we constituted a large onomastic database and built ageographic information system for Martigues, a medium-sized community in the south of France. The cross-linking of epidemiological,spatial and demographical data allows us to propose a new diagnosis for the epidemic which reached Martigues in the autumn of 1705.


2010 ◽  
Vol 25 (5) ◽  
pp. 1317-1341 ◽  
Author(s):  
Tsing-Chang Chen ◽  
Jenq-Dar Tsay ◽  
Ming-Cheng Yen ◽  
Esperanza O. Cayanan

Abstract Stretched from Indochina, across the South China Sea, to the Philippine Sea, a monsoon cyclonic shear flow was formed by easterlies of the cold surge-like flow in the north and monsoon westerlies in the south before the onset of the tropical Southeast Asian monsoon on 12 May 2008. On this date, two named tropical cyclones (Halong and Matmo) evolved with a 12-h lag from a closed vortex adjacent to the coast of central Vietnam and another closed vortex near Palawan Island (Philippines) within this shear flow. These two cyclones, named the twin Philippine tropical cyclones, moved almost on the same track, along the anomalous shear line (departure from the climatological one) across the Philippines, and turned northeastward to the ocean south of Japan. It was revealed from synoptic analysis that the cold surge-like flow was coupled with the midlatitude eastward-propagating short wave in northeast Asia, and part of the monsoon westerlies were fed by the cross-equatorial flow, the downstream flow of easterlies around the northern rim of the Southern Hemisphere subtropical high. The environment favorable for the formation of the twin cyclones was developed from the tropics–midlatitude interaction between synoptic systems in these two latitudinal zones. Formations of these cyclones were a result of drastic spinups of the two closed vortices (within the monsoon shear flow) following the surge of monsoon westerlies, which coincided with those of easterlies of the cold surge-like flow, and the cross-equatorial flow originating from easterlies between the Southern Hemisphere subtropical high and the Southern Hemisphere shear flow.


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