Ophiolite-related ultramafic rocks (Serpentinites) in the Caribbean region: a review of their occurrence, composition, origin, emplacements and Ni-Laterite soil formation

Ultramafic rocks, mainly serpentinized peridotites of mantle origin, are mostly associated with the ophiolites of Mesozoic age that occur in belts along three of the margins of the Caribbean plate. The most extensive exposures are in Cuba. The ultramafic-mafic association (ophiolites) were formed and emplaced in several different tectonic environments. Mineralogical studies of the ultramafic rocks and the chemistry of the associated mafic rocks indicate that most of the ultramafic-mafic associations in both the northern and southern margins of the plate were formed in arc-related environments. There is little mantle peridotite exposed in the ophiolitic associations of the west coast of Central America, in the south Caribbean in Curacao and in the Andean belts in Colombia. In these occurrences the chemistry and age of the mafic rocks indicates that this association is mainly part of the 89 Ma Caribbean plateau province. The age of the mantle peridotites and associated ophiolites is probably mainly late Jurassic or Early Cretaceous. Emplacement of the ophiolites possibly began in the Early Cretaceous in Hispaniola and Puerto Rico, but most emplacement took place in the Late Cretaceous to Eocene (e.g. Cuba). Along the northern South America plate margin, in the Caribbean mountain belt, emplacement was by major thrusting and probably was not completed until the Oligocene or even the early Miocene. Caribbean mantle peridotites, before serpentinization, were mainly harzburgites, but dunites and lherzolites are also present. In detail, the mineralogical and chemical composition varies even within one ultramafic body, reflecting melting processes and peridotite/melt interaction in the upper mantle. At least for the northern Caribbean, uplift (postemplacement tectonics) exposed the ultramafic massifs as a land surface to effective laterization in the beginning of the Miocene. Tectonic factors, determining the uplift, exposing the peridotites to weathering varied. In the northern Caribbean, in Guatemala, Jamaica, and Hispaniola, uplift occurred as a result of transpresional movement along pre-existing major faults. In Cuba, uplift occurred on a regional scale, determined by isostatic adjustment. In the south Caribbean, uplift of the Cordillera de la Costa and Serrania del Interior exposing the peridotites, also appears to be related to strike-slip movement along the El Pilar fault system. In the Caribbean, Ni-laterite deposits are currently being mined in the central Dominican Republic, eastern Cuba, northern Venezuela and northwest Colombia. Although apparently formed over ultramafic rocks of similar composition and under similar climatic conditions, the composition of the lateritic soils varies. Factors that probably determined these differences in laterite composition are geomorphology, topography, drainage and tectonics. According to the mineralogy of principal ore-bearing phases, Dominican Ni-laterite deposits are classified as the hydrous silicate-type. The main Ni-bearing minerals are hydrated Mg-Ni silicates (serpentine and ¿garnierite¿) occurring deeper in the profile (saprolite horizon). In contrast, in the deposits of eastern Cuba, the Ni and Cooccurs mainly in the limonite zone composed of Fe hydroxides and oxides as the dominant mineralogy in the upper part of the profile, and are classified as the oxide-type.

Indicadors de pressió ambiental a les platges de Menorca: prova pilot (IPAPM'pp)

L’augment del turisme experimentat des de principis dels anys 70 a l’illa de Menorca (Illes Balears, Espanya) ha provocat un impacte sobre les seves platges, el seu principal atractiu turístic. Molts d’aquests impactes s’incrementen durant la temporada alta, compresa entre els mesos de maig a octubre. L’objectiu principal d’aquest projecte és l’elaboració d’un sistema d’indicadors de pressió ambiental útils per a l’anàlisi de les platges. La zona objecte d’estudi de la prova-pilot, correspon a les platges del sud-oest de Menorca, aquestes cales són les que actualment es troben sotmeses a una major pressió. Es tracta de catorze platges tipificades en tres categories (A, B, C) segons les característiques del tipus d’espai on es troben situades. Són les platges de: Cala Degollador, Cala Blanca, Cala’n Bosch, Son Xoriguer, Son Saura-Es Banyul, Son Saura-Bellavista, Es Talaier, Cala Turqueta, Cala Macarelleta, Cala Macarella, Cala Galdana, Cala Mitjana, Cala Trebalúger i Cala Escorxada. Partint d’un treball bibliogràfic, s’ha realitzat una selecció de mig centenar d’indicadors potencials dels quals catorze han format part dels IPAPM’pp, mitjançant l’elaboració d’una anàlisi multicriteri. Per a cada un dels IPAPM’pp s’ha desenvolupat una metodologia amb les corresponents fitxes individuals descriptives per al seu seguiment temporal. En aquest primer estudi, l’indicador que presenta un nombre de valors no acceptables en una major proporció de platges, és l’indicador 3. Índex de valoració de les mesures de conservació del sistema natural, seguit de l’indicador 6. Superfície subsistema sorra per usuari. El 2006, les platges de tipologia A, presenten un major percentatge positiu de les variables dels indicadors. Les platges de tipologia B i C presenten un percentatge menor d’acceptabilitat dels valors dels indicadors.

Sant Llorenç del Montsec (La Noguera): un despoblat medieval

The medieval deserted village of St. Lloreng, a fortified place in the west lands of Catalonia, in Lleida, near Aragon, is studied from its origins in 11th. century unti1 14th.C. The growth and evolution of population during this time is shown by the houses, placed between the castle and the church, some so simply with only one room, some wider. The authors don't know why the village became deserted, but they indicate the possible move of the population into the limits of the Ager valley.