"Glendale Area History," as you might imagine, details the beginnings of our city, from Jose Maria Berdugo (later Verdugo) — a soldier of the Spanish king who received a land grant and established Rancho San Rafael, which includes the present-day areas of Glendale, Eagle Rock, La Cañada and Montrose — to the history of the inception of the Glendale News-Press and everything in between.
At the time, the newly created District of Columbia consisted of two counties, Washington (the present-day area of Washington, D.C.) and Alexandria (which is now Alexandria, Virginia).
At the time, the newly created District of Columbia consisted of two counties, Washington (the present-day area of Washington, D.C). and Alexandria (which is now Alexandria, Virginia).
Although, for some ancestral model reconstructions, no present-day area was within the suitable envelope, this does not invalidate the model, as past climates could exhibit climate types not seen in the present day [ 35].
Future areas of climatic suitability were compared with present-day suitable areas and present distribution by calculating the percentage of area lost under a scenario of unlimited dispersal.
Simulated present-day permafrost areas (grids) are marked in blue; permafrost areas (grids) from the Tibetan Plateau's frozen ground map are indicated by dots.
In some cases, original habitats were in present-day wintering areas, and animals developed a tendency to leave in spring in order to breed in other territories.
Rice was domesticated as early as 3500 bc, and by about 2,000 years ago it was grown in almost all of the present-day cultivation areas, predominantly deltas, floodplains and coastal plains, and some terraced valley slopes.
Other features of the Iberian topography, namely the longitudinal profile of the main rivers in the Iberian peninsula and the distribution of present-day endorheic areas, are consistent with the Tertiary tectonic evolution and the change from an endorheic to an exorheic regime during the Late Neogene and the Quaternary.
Area-averaged changes in soil temperature at a depth of 1 and 15 m in the present-day permafrost area in the QTEC are shown in Fig. 2a, b.
Petroleum migration patterns in the present-day shelf area of the Columbus basin reflect a complex interaction of structural evolution, stratigraphic architecture, and fault-seal behavior.
