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while enjoying the comforts of the fine field camp

publish 2022-07-27,browse 17
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  Another possibility to Lake Mead is presented by the following example. It is a hard choice to make. Let us think about MSFT from a different point of view. Jim Rohn once said, Either you run the day, or the day runs you。
while enjoying the comforts of the fine field camp at chinajá, we worked in the surrounding forest and availed ourselves of the opportunity to be on hand when the road crews were cutting the tall trees in the forest, thereby bringing to the ground many interesting specimens of the arboreal fauna.we stayed at chinajá until late march, with the exception of a week spent at toocog, another camp of the ohio oil company located 15 kilometers southeast of la libertad and on the edge of the savanna.thus, at toocog we were able to work both in the forest and on the savanna.in the summer of 1960, john wellman accompanied me to el petén for two weeks in june and july.most of our time was spent at chinajá, but a few days were spent at toocog and other localities in southcentral el petén.many areas in guatemala have been studied intensively by l.c.stuart, who has published on the herpetofauna of the forested area of northeastern el petén (1958), the savannas of central el petén (1935), and the humid mountainous region to the south of el petén in alta verapaz (1948 and 1950).the area studied by me and my companions is covered with rainforest and lies to the north of the highlands of alta verapaz and to the south of the savannas of central el petén.a few specimens of amphibians and reptiles were obtained in this area in 1935 by c.l.hubbs and henry van der schalie; this collection, reported on by stuart (1937), contained only one species, _cochranella fleischmanni_, not present in our collection of 77 species and 617 specimens.acknowledgments i am grateful to l.c.stuart of the university of michigan, who made the initial arrangements for our work in el petén, aided me in the identification of certain specimens, and helped in the preparation of this report.j.knox jones, jr.and john wellman were able field companions, who added greatly to the number of specimens in the collection.in guatemala, clark m.shimeall and harold hoopman of the ohio oil company of guatemala made available to us the facilities of the companys camps at chinajá and toocog.alberto alcain and luis escaler welcomed us at chinajá and gave us every possible assistance.juan monteras and antonio aldaña made our stay at toocog enjoyable and profitable.during our visits to southern el petén, julio bolón c.worked for us as a collector, and between march and june he collected and saved many valuable specimens; his knowledge of the forest and its inhabitants was a great asset to our work.jorge a.ibarra, director of the museo nacional de historia natural in guatemala assisted us in obtaining necessary permits and extended other kindnesses.to all of these people i am indebted for the essential parts that they played in the completion of this study.field work in the winter of 1960 was made possible by funds from the american heart association for the purposes of collecting mammalian hearts.my field work in the summer of 1960 was supported by a grant from the graduate research fund of the university of kansas.description of the area a vast lowland region stretches northward for approximately 700 kilometers from the highlands of guatemala to the gulf of mexico.the northern twothirds of this low plain is bordered on three sides by seas and forms the yucatán peninsula.the lowlands at the base of the yucatán peninsula make up the departamento el petén of guatemala.the area with which this report is concerned consists of the southcentral part of el petén.physiography immediately south of chinajá is a range of hills, the serrania de chinajá, having an almost due eastwest axis and a crest of about 600 meters above sea level.south of the serrania de chinajá are succeedingly higher ridges building up to the meseta de cobán and sierra de pocolha and eventually to the main guatemalan highlands.the northern face of the serrania de chinajá is a fault scarp dropping abruptly from about 650 meters at the crest to about 140 meters at the base.from the base of the serrania de chinajá northward to the río de la pasión at sayaxché the terrain is gently rolling and has a total relief of about 50 meters.north of the río de la pasión is a low dome reaching an elevation of 170 meters at la libertad; see stuart (1935:12) for further discussion of the physiography of central el petén.the rocks in southern el petén are predominately miocene marine limestones; there are occasional pockets of pliocene deposits.there is little evidence of subterranean solution at chinajá, but northward in central el petén karsting is common.the upper few inches of soil is humus rich in organic matter; below this is clay.climate the climate of el petén is tropical with equable temperatures throughout the year.temperatures at chinajá varied between a nighttime low of 65° f.and a daytime high of 91° f.during the time of our visits.in the köppen system of classification the climate at chinajá and toocog is af.rain falls throughout the year, but there is a noticeable dry season.to anyone who has traveled from south to north in el petén and the yucatán peninsula, it is obvious from the changes in vegetation that there is a decrease in rainfall from south to north.there is a noticeable difference between chinajá and toocog.although rainfall data are not available for chinajá and toocog, there are records for nearby stations (sapper, 1932)

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