neovolcanic

[¦nē·ō·väl′kan·ik]

(petrology)

Referring to extrusive rocks that are of Tertiary or younger age.

References in periodicals archive ?

plexippus L.; Danaidae; Lepidoptera) in North America to the overwintering site in the Neovolcanic Plateau of Mexico.

POTENTIAL SIGNIFICANCE OF FALL BREEDING OF THE MONARCH BUTTERFLY (DANA US PLEXIPPUS) IN THE ROLLING PLAINS ECOREGION OF WEST TEXAS

Salansky, K.: 2009, Geophysical indication of unknown neovolcanic centre near Marianske Lazne.

The newly discovered neogene maar volcano near the Marianske Lazne, western Bohemia

The principal incidence of wildfires (red points) in forest (Figure 3(a)) occurs on the western side of Mexico, along the Western Sierra Madre, Southern Sierra Madre, Trans-Mexican Neovolcanic Belt, and Sierra Madre of Chiapas.

Estimation of total yearly C[O.sub.2] emissions by wildfires in Mexico during the period 1999-2010

Mammals and protected areas in the Trans-Mexican Neovolcanic Belt, pp 199-226.

Mastofauna del area de proteccion de flora y fauna La Primavera, Jalisco, Mexico

These sites form part of the province of the neovolcanic belt, which is formed by the subprovince of the plains and mountains of Queretaro and Hidalgo and the subprovince of the Anahuac lakes and volcanoes.

Comadia redtenbacheri (Lepidoptera: Cossidae) pupal development in the laboratory

Historical biogeography of lowland species of toads (Bufo) across the Trans-Mexican Neovolcanic Belt and the Isthmus of Tehuantepec.

Regionalizacion biogeografica de la mastofauna de los bosques tropicales perennifolios de Mesoamerica

Osgoodomys banderanus (Osgood's deermouse) is a nocturnal, solitary, medium-sized cricetid that is endemic to western Mexico, in particular the western portion of the Trans-Mexican Neovolcanic Belt (Fa and Morales, 1991).

Demographic features and habitat preferences of Osgoodomys banderanus (Osgood's deermouse) in Colima, Mexico

The station is in the Zoquiapan National Park, at the Neovolcanic Belt of Central Mexico, 3000-3500masl (Franco and Burquez, 1981).

Effects of Phyllophaga (Phytallus) hoegei larval density (coleoptera:melolonthidae) on plant and herbivore growth/ Efectos de la densidad de larvas de Phyllophaga (Phytallus) hoegei (coleoptera:melolonthidae) en el crecimiento de plantas y herbivoros/Efeitos da densidade de larvas de Phyllophaga (Phytallus) hoegei (coleoptera: melolontidae) no crescimento de plantas e herbivoros

The volcanic and tectonic activity is mostly confined to the neovolcanic zone that crosses the island from southwest to northeast and is the continuation of the ridge on land (Saemundsson 1979).

Porosity structure of Icelandic basalt/Islandi basaltide poorsus

Geographically, 70% of this group was found to the east of 100o W latitude and was concentrated at the eastern extreme of the neovolcanic axis in the states of Puebla, Hidalgo, and Veracruz, and extending down into Oaxaca (Fig.

Structure of Genetic Diversity among Common Bean Landraces of Middle American Origin Based on Correspondence Analysis of RAPD

Both molecular clock calibrations (based on Nei's D) and geological-age estimates of the Mexican Neovolcanic Axis are consistent with an initial divergence of no more than 10 million years for the Mexican taxa, and many species are apparently much more recently derived (Shaffer 1984a).

The polytypic species revisited: genetic differentiation and molecular phylogenetics of the tiger salamander Ambystoma tigrinum (Amphibia: caudata) complex

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