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Hugo Moreno, José Bengochea-Guevara, Angela Ribeiro and Dionisio Andújar
In the field of computer vision, 3D reconstruction of crops plays a crucially important role in agriculture. On-ground assessment of geometrical features of vineyards is of vital importance to generate valuable information that enables producers to take ...
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Oscar Fabian Luengo Moreno, Hugo Perez Herrera
Pág. 90 - 105
La presente investigación propone construir una mirada patrimonial al paisaje rural de la provincia de Colchagua, Chile. Una mirada que pone en valor un capital creativo supeditado a una economía de recursos, que ha sido capaz de construir galpones, corr...
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Jon J. Major,Thomas C. Pierson,Richard P. Hoblitt,Hugo Moreno
Pág. 324 - 358
Explosive activity at Chaitén Volcano in May 2008 and subsequent dome collapses over the following nine months triggered multiple, small-volume pyroclastic density currents (PDCs). The explosive activity triggered PDCs to the north and northeast, which f...
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Hugo Moreno R.
Pág. 589 - 590
Obituario Leopoldo López.
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Hugo Alexander Rondon Quintana, Luis Angel Moreno Anselmi, Daniella Rodriguez Urrego, Jennifer Lee Marino
Pág. 19 - 33
AbstractDownloadsReferencesHow to Cite
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Hugo Moreno R.
Pág. 368 - 369
Lorenzo Casertano (1921-2004)
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Luis E. Lara,Jose A. Naranjo,Hugo Moreno
Pág. 241 - 258
Lanín volcano is a compound stratocone, mainly effusive, made up by four units defined through morphological criteria. The first unit represents an ancient volcano; the youngest three units form the present stratocone built since the Middle-Late Pleistoc...
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Fernando Catalá Moreno,Jorge Presa Matilla,Hugo Corres Peiretti,Julio Sánchez Delgado,Laura Granda San Segundo
Pág. 5 - 27
El túnel viario de María de Molina, que unirá el Paseo de la Castellana y la calle Velázquez con la N-II de Madrid a Barcelona, constituirá la mayor obra municipal de pasos subterráneos. El túnel de un total de 1.171 m de longitud va a absorber una salid...
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Luis Lara,Carolina Rodriguez,Hugo Moreno,Carlos Perez de Arce
Pág. 67 - 90
In the Andean Range, south of 39°S, there is a suite of eroded volcanic centres that includes remains of vents or proximal, intermediate or distal volcanic facies. New geochronological K-Ar data show that their ages are in the Late Pliocene-Middle Pleist...
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Ricardo Thiele,Hugo Moreno,Sara Elgueta,Alfredo Lahsen,Sofia Rebolledo,M. Eugenia Petit-Breuilh
Pág. 229 - 253
The Quaternary geological history of the uppermost the Río Laja valley shows a complex interrelation between volcanic, mass wasting, and alluvial and fluvial sedimentary processes. The valley was initialiy carved by Lower Pleistocene glacial action on a ...
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Ricardo Thiele,Hugo Moreno,Sara Elgueta,Alfredo Lahsen,Sofia Rebolledo,M. Eugenia Petit-Breuilh
Pág. 229 - 253
The Quaternary geological history of the uppermost the Río Laja valley shows a complex interrelation between volcanic, mass wasting, and alluvial and fluvial sedimentary processes. The valley was initialiy carved by Lower Pleistocene glacial action on a ...
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Leopoldo Lopez-Escobar,Jose Cembrano,Hugo Moreno
Pág. 219 - 234
ABSTRACT. Between latitudes 37° and 46°S of the Andes, the Nazca-South America Plate convergence is currently slightly oblique, Postglacial volcanism has been continuous and intense, being expressed as numerous composite stratovolcanoes (SV) and hundreds...
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Leopoldo Lopez-Escobar,Jose Cembrano,Hugo Moreno
Pág. 219 - 234
ABSTRACT. Between latitudes 37° and 46°S of the Andes, the Nazca-South America Plate convergence is currently slightly oblique, Postglacial volcanism has been continuous and intense, being expressed as numerous composite stratovolcanoes (SV) and hundreds...
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Hugo Moreno,Gustavo Fuentealba
Pág. 167 - 171
INTRODUCTION. On May 17, at about 6:00 a.m., the Llaima volcano began a strombolian eruption, 10 years since the last short phreatomagmatic eruption (April 1984). The Llaima volcano is a complex composite-shield volcano, with a buried caldera and 40 para...
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Hugo Moreno,Gustavo Fuentealba
Pág. 167 - 171
INTRODUCTION. On May 17, at about 6:00 a.m., the Llaima volcano began a strombolian eruption, 10 years since the last short phreatomagmatic eruption (April 1984). The Llaima volcano is a complex composite-shield volcano, with a buried caldera and 40 para...
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Jose A. Naranjo,Hugo Moreno,Carlos Emparan,Michael Murphy
Pág. 167 - 191
ABSTRACT. Recent explosive volcanism at Sollipulli volcano, southern Andes (39°S). The Solipulli volcano is a caldera that nests a ca. 2 km3 glacier. lts last eruption occurred over 700 years ago, through a parasitic cone. On the other hand, a paroxismal...
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Leopoldo Lopez-Escobar,Miguel A. Parada,Hugo Moreno,Fred A. Frey,Rosemary L. Hickey-Vargas
Pág. 211 - 226
RESUMEN. Contribucion a la petrogenesis de los volcanes Osorno y Calbuco, Andes del Sur (41°00'-41°30'S): estudio comparativo. Los volcanes Osorno y Calbuco, ubicados respectivamente en las latitudes 41°05'S y 41°20'S de la region sur de la Zona Volcani...
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Leopoldo Lopez-Escobar,Miguel A. Parada,Hugo Moreno,Fred A. Frey,Rosemary L. Hickey-Vargas
Pág. 211 - 226
RESUMEN. Contribucion a la petrogenesis de los volcanes Osorno y Calbuco, Andes del Sur (41°00'-41°30'S): estudio comparativo. Los volcanes Osorno y Calbuco, ubicados respectivamente en las latitudes 41°05'S y 41°20'S de la region sur de la Zona Volcani...
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Jose A. Naranjo,Hugo Moreno
Pág. 69 - 80
RESUMEN. El Llaima es uno de los mayores volcanes de los Andes del Sur (37°-46°S) con un area de ca. 500 km2 y un volumen de ca. 400 km3. Es un volcan compuesto, mixto y de escudo con una caldera cubierta y 40 conos adventicios de escoria. Se encuentra a...
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Jose A. Naranjo,Hugo Moreno
Pág. 69 - 80
RESUMEN. El Llaima es uno de los mayores volcanes de los Andes del Sur (37°-46°S) con un area de ca. 500 km2 y un volumen de ca. 400 km3. Es un volcan compuesto, mixto y de escudo con una caldera cubierta y 40 conos adventicios de escoria. Se encuentra a...
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