Resolución N° 067 del 21 de abril de 2010 ¿Cuáles son los elementos objeto de verificación por parte de la cámara en las cesiones de cuotas sociales y nombramientos en Sociedades de Responsabilidad Limitada?

Servicios registrales

Resolución N° 071 del 27 de abril de 2010 ¿Cuáles son los elementos que las Cámaras de comercio verifican en el proceso de disolución y liquidación de sociedades? ¿Cuándo opera la disolución sin necesidad de declaración de la misma?

Servicios registrales

Resolución N° 34 del 8 de marzo de 2007 ¿Cuáles son los criterios que tiene en cuenta la Cámara de Comercio para llevar a cabo el cobro de impuesto de registro en los casos de una fusión por absorción de sociedades?

Servicios registrales

Resolución N° 47 del 26 de marzo de 2007 ¿Cuáles son los criterios que tiene en cuenta la Cámara de Comercio cuando evalúa los eventos de fallecimiento del socio gestor y la representación de las cuotas de este en las sociedades en comandita?

Servicios registrales

Resolución No. 024 del 26 de febrero de 2014 ¿En qué circunstancias y cómo debe hacerse la convocatoria para la asamblea de accionistas por parte de la Superintendencia de Sociedades?

La Cámara de Comercio de Bogotá inscribió el acta No. 152 AG de la asamblea de accionistas de la sociedad ORGANIZACIÓN SANITAS INTERNACIONAL S.A., en la cual se hizo nombramiento de la junta directiva en la sociedad mencionada. Contra este acto administrativo, presentó recurso de reposición el agente oficioso de algunos accionistas y uno de los miembros principales de la junta directiva de la sociedad.

Resolución No. 017 del 17 de febrero de 2014 ¿Cuál es el control que ejercen las Cámaras de Comercio sobre los actos de inscripción de las sociedades por acciones simplificadas?

La Cámara de Comercio de Bogotá inscribió el acta No. 003 de asamblea de accionistas del 15 de noviembre de 2013, mediante la cual se nombró representante legal de la sociedad ALCO ARQUITECTOS SAS.El representante legal "removido" de la sociedad mencionada solicitó la revocatoria del acto administrativo de registro.

Resolución N° 186 del 14 de agosto de 2007 ¿Bajo que criterios evalúa la Cámara de Comercio la toma de decisiones en las sociedades de responsabilidad limitada ?

Servicios registrales

Resolución N° 206 del 6 de septiembre 2007 ¿La remisión a las normas de las sociedades comerciales frente a las entidades del sector solidario, abarca todo su marco jurídico?¿ Es indispensable el consentimiento del titular del derechos particular reconocido en un acto?

Servicios registrales

Resolución N° 210 del 10 de septiembre de 2007 ¿Cuáles son los criterios que la Cámara de Comercio considera para evaluar el quórum y las máyorias en las sociedades anónimas?

Servicios registrales

Resolución N° 0220 del 24 de septiembre de 2007 ¿Cuáles son los presupuestos necesarios para la inscripción de modificación de situaciones de control? ¿Puede la Cámara de Comercio abstenerse de registrar un acto de modificación de tal situación cuando quien alega dicha modificación es una ESAL afirmando que solo procede tal registro cuando se trate sociedades comerciales?

Servicios registrales

Agrarian revolution in Central America : a comparison of Nicaragua and Honduras using Jeffery Paige's theory of Agrarian revolution

ABSTRACT In 1979 Nicaragua, under the Sandinistas, experienced a genuine, socialist, full scale, agrarian revolution. This thesis examines whether Jeffery Paige's theory of agrarian revolutions would have been successful in predicting this revolution and ln predicting non-revolution in the neighboring country of Honduras. The thesis begins by setting Paige's theory in the tradition of radical theories of revolution. It then derives four propositions from Paige's theory which suggest the patterns of export crops, land tenure changes and class configurations which are necessary for an agrarian and socialist revolution. These propositions are tested against evidence from the twentieth century histories of economic, social and political change in Nicaragua and Honduras. The thesis concludes that Paige's theory does help to explain the occurrence of agrarian revolution in Nicaragua and non-revolution in Honduras. A fifth proposition derived from Paige's theory proved less useful in explaining the specific areas within Nicaragua that were most receptive to Sandinista revolutionary activity.

Molluscan carbonate geochemistry and paleoceanography of the Late Cretaceous western interior seaway of North America

North Amerlc8 W8S inundated by fJ major eplcontlnental sea during ihe C:retaceo.us Period. The sOljihw6rd transgression of th.e northern Boreal See along the ~\festern Interior Seaway resulted in a meetlng with the northward edv6nclng waters from the GUlf of Mexico (Obradovich and Cobban, 1975). Th1s link was 1n eXlstence by late Albien time and 6llowed for the comm1ngl1ng of the prol1ferous Arctic and Gulf rnar1ne faunas (F1g. 1). By early Campanlan time, there was a widening of B6ffln Bay wlth a slrnult8neous subsidence 1n the Arct1c Archlpelago and Sverdrup 6as1n (W11liam and Stelck, 1975). Williams and Burk (1964) found 6 break 1n the marines sedlmentatlon in the f1anltoba area, suggesting Bland corlnectlon from the Dlstrlct of Keewatln through eastern M6fl1toba to the lake Sl~perlor reglon, lmplying that the only dlrect connection between the Interlor Sea with Baffln Bay, was yia the Arct1c. This hiatus was also documented by Meek and Hayden (1861) ln the United states between the Niobrara and Pierre Format1ons. Jeletzky (1971) suggested that the retreat of the sea towards the east was by a serles of strong pulses resultlng in the regression of the Campanlan and M66str1chtlan seas. During ttle Cretaceous1 the r1s1ng Corl1111era caused the western shoreline of the Interlor Sea to migrate eastwards and the Cordillera'l detritus produced deltaic cornplexes from the Mackenzie Valley to Ne\N Mexlcoo The foreland basin was continually subslding and thls down\",arplng aided in the eastward m1gration of the western shorel1ne. Thls also lndicates that trle water 'tIes becom1ng deeper in the central Plains sect10n of the Seaway (Fig. 2).

Sedimentology and micromorphology of drumlin sediments at Chimney Bluffs State Park, New York, United States of America

The drumlin sediments at Chimney Bluffs, New York appear to represent a block-inmatrix style glacial melange. This melange comprises sand stringers, lenses and intraclasts juxtaposed in an apparently massive diamicton. Thin section examination of these glacigenic deposits has revealed microstructures indicative of autokinetic subglacial defonnation which are consistent with a deformable bed origin for the diamicton. These features include banding and. necking of matrix grains, oriented plasma fabrics and the formation of pressure shadows at the long axis ends of elongate clasts. Preservation of primary stratification within the sand intraclasts appears to suggest that these features were pre-existing up-ice deposits that were frozen, entrained, then deposited as part of a defonning till layer beneath an advancing ice sheet. Multi-directional micro-shearing within the sand blocks is thought to reflect the frozen nature of the sand units in such a high strain environment. It is also contended that dewatering of the sediment pile leading to the eventual immobilisation of the defonning till layer was responsible for opening sub-horizontal fissures within the diamicton. These features were subsequently infilled with mass flow poorly sorted sands and silts which were subjected to ductile defonnation during the waning stages of an actively deforming till layer. Microstructures indicative of the dewatering processes in the sand units include patches of fine-grained particles within a coarser-grained matrix and the presence of concentrated zones of translocated clays. However, these units were probably confined within an impermeable diamicton casing that prevented massive pore water influxes from the deforming till layer~ Hence, these microstructures probably reflect localised dewatering of the sand intraclasts. A layered subglacial shear zone model is proposed for the various features exhibited by the drumlin sediments. The complexity of these structures is explained in terms of ii superposing deformation styles in response to changing pore water pressures. Constructional glaciotectonics, as implied by the occurrence of sub-horizontal fissuring, is suggested as the mechanism for the stacking of the sand intraclast units within the diamicton. The usefulness of micromorphology in complimenting the traditional sedimentology of glacigenic deposits is emphasised by the current study. An otherwise massive diamicton was shown to contain microstructures indicative of the very high strain rates expected in a complexly deforming till layer. . It is quite obvious from this investigation that the classification of diamictons needs to be re-examined for evidence of microstructures that could lead to the re-interpretation of diamicton forming processes. RESUME Le pacquet de sediments drumlinaire de Chimney Bluffs, New York, represent un "bloc-en-matrice" genre de melange glaciale. Des structures microscopique comprennent l'evidence pour la defonnation intrinseque attribuee a l'origine lit non resistant du drumlin. PreselVation des structures primaires au coeur des blocs arenaces suggere que ceux sont des depots preexistant qui furent geles, entraines et par la suite sedimentes au milieu d'une couche de debris sous-glaciaires en voie de deformation. Des failles microscopiques a l'interieur des blocs arenaces appuient aussi l'idee d'un bloc cohesif (c'est-a-dire gele) au centre d'un till non resistant. Des implications significatives s'emergent de cette etude pour les conditions sous-glaciaire et les processus de la formation des drumlin.

The wonders of Niagara : a visit to America's greatest cataract with a description of the points of interest in a region of scenic grandeur and beauty.

Cover title.