Persona: Lario Gómez, Javier
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Lario Gómez
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Publicación Episodios marinos del Último Interglacial (Estadio Isotópico 5) del litoral de Málaga (SE Peninsular)(Universidad de Málaga (UMA), 1999) Zazo Cardeña, Caridad; Hillaire Marcel, Claude; Goy Goy, José Luis; Hoyos Gómez, Manuel; Lario Gómez, JavierLa cronoestratigrafía del Cuaternario en el litoral bético mediterráneo ha sido construida fundamentalmente en base a la cartografía y correlación entre las distintas secuencias de episodios marinos y continentales desarrollados en cada una de las cuencas. La cronología entre las distintas unidades morfosedimentarias se ha hecho en base a su disposición relativa, distribución regional, datos paleomagnéticos y contenido faunístico. El gran desarrollo que presentan en este litoral los depósitos tirrenienses con abundancia de fauna, ha hecho posible la utilización de dataciones isotópicas que han permitido caracterizar cronológicamente los episodios cálidos registrados desde el final del Pleistoceno medio.Publicación Active landscapes of Iberia(Springer, 2020) Galve Arnedo , Jorge Pedro; Pérez Peña, José Vicente; Azañón, José Miguel; Insua Pereira, Diamantino M.; Cunha, Pedro P.; Pereira, Paulo; Viaplana Muzas, M.; Gracia Prieto, Francisco Javier; Remondo Tejerina, Juan; Jabaloy, Antonio; Bardají, Teresa; Silva, Pablo Gabriel; Zazo Cardeña, Caridad; Goy Goy, José Luis; Dabrio, Cristino José; Cabero, Ana; Ortuño Casanova, María del Rocío; Lario Gómez, Javier; https://orcid.org/0000-0003-2988-8077The recent geodynamic evolution of Iberia is recorded in its topography. Geomorphic markers and their dating; morphometric indices estimated through cutting-edge DEM analysis techniques; and the link of all this data with results of geophysical studies allow discussing why Iberia displays the highest average elevation in Europe and shows a particular topography with such diversity of landscapes. For example, the region of the Iberian (or Hesperian) Massif, the western sector of Iberia, shows an anomalous average elevation without a satisfactory explanation. On the other hand, different explanations about the recent evolution of the Alpine mountain ranges of the eastern sector of Iberia have come to light after macroscale landscape analyses. This is strengthening the debate on the driving force behind the actual topography of the Pyrenees, Cantabrian Mountains, Iberian Chain and Betics.Publicación Procesos cársticos en terrazas marinas del último interglaciar asociados a cambios climáticos y de nivel del mar (Golfo de Cádiz, España)(AEQUA, 2005) Cabero, Ana; Zazo Cardeña, Caridad; Goy Goy, José Luis; Dabrio, Cristino José; Borja, Francisco; Bardají, Teresa; Silva, Pablo Gabriel; Roquero García-Casal, Elvira; Lario Gómez, Javier; https://orcid.org/0000-0003-2988-8077The coastal strip between Trafalgar and Punta Paloma, is characterized by the development of a karstic complex that affects the Last Interglacial marine terraces (OIS 5c ~100 ka, Fig. 1), there composed of well cemented conglomerates and sandstones. Two different morphologies are recorded, both related to different genetic models: "solution pipes" controlled by climatic changes (switch from humidity to aridity), and "horizontal tubules" controlled by changes in base level. The origin and palaeoenvironmental meaning of these karstic forms are described for the first time in the littoral of Cadiz, within a chronological framework based on OSL (Optically Stimulated Luminescence) and U/Th (alpha and TIMS) dating.Publicación Geomorfología litoral y cárstica en la penibética malagueña(Universidad de Barcelona, 1998) Malvárez, G.; Zazo Cardeña, Caridad; Goy Goy, José Luis; Luque, L.; Lario Gómez, JavierPublicación Tectonic and morphosedimentary features of the 2010 Chile earthquake and tsunami in the Arauco Gulf and Mataquito River (Central Chile)(Elsevier, 2016-05-23) Zazo Cardeña, Caridad; Goy Goy, José Luis; Lario Gómez, JavierEffects of the 2010 Chilean earthquake and tsunami were evaluated at coastal sites between two zones of different coseismic deformations. Land deformation, run-up, inundation extent and deposit extent and thickness were measured in the field, providing insights into the processes and morphological changes associated with tsunami inundation and backwash. Three to five waves, of up to 10 m height, deposited several related layers along the coast, the thickness of these sandy deposits does not exceed 80 cm, and is generally less than 30 cm. Coseismic deformation measured by means of bio- and geomorphic markers agrees well both with model deformation and measured GPS. There is no relationship between the run-up height and the trend of coseismic deformation (uplift or subsidence), mainly because the effects of the tsunami were influenced locally by offshore bathymetry and coastal morphology.Publicación Sea level and climate changes in the Cabo De Gata Lagoon (Almeria) during the last 6500 YR BP(INQUA, International Union For Quaternary Research, 1998) Goy Goy, José Luis; Zazo Cardeña, Caridad; Dabrio, Cristino José; Baena Preysler, Javier; Harvey, A. M.; Silva, Pablo Gabriel; González, F.; Lario Gómez, JavierThe Holocene evolution of the lagoon of Cabo de Gata in the geodynamic framework of the south-eastem lberian Península is presented for the first time. The work is based on detail geomorphological mapping of the Quaternary deposits, and radiocarbon measurements of samples collected in the spit barrier systems. The genesis of the Cabo de Gata and Roquetas lagoons is connected to the joint action of three factors. ( l ) Neotectonics, that controlled the occurrence of lowlands. (2) The general glacio-eustatic, Holocene transgression, that brought the sea level to elevations 1.5-2 m above its present values and, eventually, flooded the lowlands during the Flandrian maximum ca. 6500 yr BP. (3) The climate (humidity/aridity) that influenced the sediment supply to the coast and also the small fluctuations of sea level after the Flandrian maximum. Four spit-barrier units have been distinguished. Deposition of the two older ones (H1 and H2 ) took place between ca. 6500 and ca. 2500 yr BP under longshore drift towards the NW. Both units enclosed a lagoon that ·is placed to the NE of its present position. The more recent units (H3 and H4) close the present lagoon and were deposited between ca. 2300 and present under longshore drift to the SE. A more hum id period has been identified during the Gap separating units H1 and H2 (ca. 4400- 4200 yr BP) when most holocene alluvial fans were deposited. Aridity increased after ca. 2500 yr BP when aeolianPublicación Changes in littoral dynamics and sea level in southern Iberia and Canary Istands during the Holocene.(Sociedad Geológica de España, 1996) Zazo Cardeña, Caridad; Dabrio, Cristino José; Goy Goy, José Luis; Bardají, Teresa; Ghaleb, B.; Lario Gómez, Javier; https://orcid.org/0000-0003-2988-8077The interaction between global factors tglobal" glacio-eustatic sea-leve/ rise) and regional factors (tectonic trend, oceanographic factor) is analyzed in different areas of the lberian and Canary lsland littora/. Sea-leve/ changes and climatic variations are stated for the Mediterranean and Atlantic littora/s, with different tidal ranges and tectonic trends. Different stages can be envisaged in the coastal evolution of a/most ali the analyzed areas from the beginning of Holocene (10.000 BP): at ca. 7.000 BP (Flandrian maximum) with a change from open estuaries to aggradational processes (Cádiz Gulf, subsiding area), basal peat (Valencia Gulf, subsiding area) and development of microcliffs (Mediterranean uplifting areas). From 7,000 to 2,700 BP a first progradation phase with development of spit bars took place in the mediterranean uplifting areas, whilst in the atlantic subsiding one starts the aggradation processes in the formerly open estuaries, an a/so from ca.4,000 BP development of spit-bar system. A second progradation phase ofthe spit bars systems occurs between 2,400 and 500 BP both in Almería and Cádiz Gulf, where a change from aggradation to progradation takes place in the estuary environments, and with a change in the direction of /ongshore drift (Mediterranean) and prevailing winds (both areas) at ca.2,400 BP. At ca. 1,200 BP a sudden paleogeographic change took place in estuary environments. From 500 BP up to now a marked increase of coastal progradation in ali littorals is observed. Climatic interpretations /ed to corre/ate anticyclonic conditions (as it happened during Little Ice Ages) with the growing of spit bar systems and progradation, while low pressure conditions (as during Medieval Warm Period) coincides with no progradation. In the Canary lslands, the development of storm ridges at ca. 3,500 BP can be corre/ated with an intensification of trade winds.Publicación Improving the coastal record of tsunamis in the ESI-07 scale: Tsunami Environmental Effects Scale (TEE-16 scale)(Universidad Politécnica de Barcelona, 2016-06) Bardají, Teresa; Silva, Pablo Gabriel; Zazo Cardeña, Caridad; Goy Goy, José Luis; Lario Gómez, Javier; https://orcid.org/0000-0003-2988-8077This paper discusses possibilities to improve the Environmental Seismic Intensity Scale (ESI-07 scale), a scale based on the effects of earthquakes in the environment. This scale comprises twelve intensity degrees and considers primary and secondary effects, one of them the occurrence of tsunamis. Terminology and physical tsunami parameters corresponding to different intensity levels are often misleading and confusing. The present work proposes: i) a revised and updated catalogue of environmental and geological effects of tsunamis, gathering all the available information on Tsunami Environmental Effects (TEEs) produced by recent earthquake-tsunamis; ii) a specific intensity scale (TEE-16) for the effects of tsunamis in the natural environment at coastal areas. The proposed scale could be used in future tsunami events and, in historic and paleo-tsunami studies. The new TEE- 16 scale incorporates the size specific parameters already considered in the ESI-07 scale, such as wave height, run-up and inland extension of inundation, and a comprehensive and more accurate terminology that covers all the different intensity levels identifiable in the geological record (intensities VI-XII). The TEE-16 scale integrates the description and quantification of the potential sedimentary and erosional features (beach scours, transported boulders and classical tsunamites) derived from different tsunami events at diverse coastal environments (e.g. beaches, estuaries, rocky cliffs,). This new approach represents an innovative advance in relation to the tsunami descriptions provided by the ESI-07 scale, and allows the full application of the proposed scale in paleoseismological studies. The analysis of the revised and updated tsunami environmental damage suggests that local intensities recorded in coastal areas do not correlate well with the TEE-16 intensity (normally higher), but shows a good correlation with the earthquake magnitude (Mw). Tsunamis generated by earthquakes can then be considered efficient processes in the direct transference of the “energy” released by offshore seismogenic sources to the nearest coastal areas, even over distances of hundreds of kilometres (>200km). This scale, as the previous ones, is independent of the earthquake type (i.e. style of faulting) and only focuses on the environmental effects triggered by tsunamis of seismic origin.Publicación The coastal record of tsunamis in the INQUA ESI-2007 scale(Instituto Geológico y Minero de España, 2014) Bardají, Teresa; Silva, Pablo Gabriel; Zazo Cardeña, Caridad; Goy Goy, José Luis; Cabero, Ana; Lario Gómez, Javier; https://orcid.org/0000-0003-2988-8077Seismic Intensity scales are based on the effects of earthquakes on man, man-made structures and on natural environment. However, the effects on the environment have been usually minimized because they were considered as inaccurate features. The growth of Palaeoseismology as an independent discipline led to the development of the ESI-2007 Intensity Scale, based on the effects of earthquakes on the environment and ratified by INQUA during its XVII Congress (Cairns, Australia-2007). This scale can be used alone or jointly with other intensity scales, but it becomes especially useful for seismic intensity higher than X, when damage-based scales get saturated and environmental effects are still diagnostic. Tsunamis are only considered in the ESI-scale by the height of the waves, and no by their geological or sedimentary record. Data from present day tsunamis (authors’ own work and other’s published data) are used as a first approach to the implementation of this record in the ESI-scale. However, the joint effort of an international working group is desirable in order to properly match effects and intensity degrees.Publicación Holocene incised-valley fills and coastal evolution in the Gulf of Cádiz (Southern Spain)(INQUA, International Union For Quaternary Research, 1998) Dabrio, Cristino José; Zazo Cardeña, Caridad; Goy Goy, José Luis; Sierro, F. J.; Borja, Francisco; González Delgado, José Ángel; Flores Villarejo, José Abel; Lario Gómez, Javier