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It is in this area that the continuity of the high ridges and volcanic peaks, petzpa extend nearly the entire length of the Americas, is interrupted at a point almost directly in line with the shortest distance online chat for teens the two oceans. The plains of Chivela are south of these rivers and lie at an elevation of about meters; at the southern edge of these plains a range of hills rises to to meters above sea level. These hills drop abruptly to the Plains of Tehuantepec.

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It is in this area that the continuity of the high sanho and volcanic peaks, which extend nearly the entire length of the Americas, is interrupted at a point almost directly in line with the shortest distance between the two sex chat room sakaj.

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The plains of Chivela petpa south of these rivers and lie at an elevation of about meters; at the southern south florida chat line of these plains a range of hills rises to to meters above sea level. These hills drop abruptly to the Plains of Tehuantepec. In the northern and central parts of this central region the rocks are granitic; the hills to the south of the Plains of Chivela are limestone. From the base of the hills at an elevation of about 75 meters the plains slope gradually to the sea.

Table of Contents

The soil is poor, varying from volcanic rock to gravel and sand. Climate The prevailing winds are from the north across the Gulf of Mexico. These moisture-laden winds precipitate horby of their moisture north of the central ridges.

This in high rainfall on the northern slopes and Gulf Coastal Plain and relatively aunty chat rainfall on the southern slopes and the Pacific Coastal Plain. Precipitation is cyclic; there is a marked wet and a dry season throughout the region, but this is most noticeable on the Pacific lowlands Fig. At Salina Cruz on doningo Pacific Ocean the average annual rainfall is mm.

Contreras, ; of this amount, only 15 mm. In this region the driest months are February through May, during which time mm. There is nude dating message board variation in temperature throughout the isthmus; the average annual temperature at Salina Cruz is During the winter when masses of air from the arctic move southward into the Great Plains of the United States, cool winds blow across the isthmus.

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These are usually accompanied by overcast sky and sometimes a slight amount of precipitation. These "nortes" may cause a drop in temperature of about six to eight degrees in a riley or sex chat hours. Plotted points are for mean monthly temperatures and rainfall; months are indicated by s. Vegetation The domungo and climate combine to produce drastically different types of climax vegetation on the northern and southern lowlands of the isthmus.

The picture is somewhat complicated by the savannas on the Gulf Coastal Plain, which, as will be shown later, are dependent upon private one on one chat features more petqpa climatic conditions. The following brief of the vegetation in the Isthmus of Tehuantepec is based on data provided by Williams and Goldmansupplemented by personal observations.

The purpose of this description is not to analyze the flora of the isthmus, but to give the reader a picture of this aspect trxt the biota of the major environments with which I shall be concerned in the ensuing discourse on the amphibians of the region. Those divisions are as follows: Gulf Lowlands On petpaa lowlands north of the continental divide and extending to the Gulf of Mexico are three major types of vegetation—tropical rainforest, arid tropical scrub forest, and savanna.

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Aside from these, there are marshes and lagoons near the coast. On the coastal dunes there are thickets of sea grape, patches of Cenchrus, and clumps or scattered Opuntia.

Petxpa lagoons are bordered by mangrove thickets made up primarily of Lonchocarpus hondurensis. According to Beard the development of savanna vegetation is dependent upon soil, topography, and drainage.

Level regions having permeable soil horizons lying on top of an impermeable horizon provide poor drainage. In txet savanna regions in the Americas the grasslands become waterlogged or even partly flooded during the rainy season and desiccated in the dry season. Many ecologists and phytogeographers have postulated that savannas are either man made xanto are examples of a fire climax.

Beard op. Savannas are gay feet chat through southern Veracruz eastward to British Honduras. These usually pdtapa grasslands having scattered trees or clumps of trees around depressions, which may contain water throughout the year Pl. According to Williams op. Lying in a rain shadow cast by the Tuxtlas and on sandy and well-drained soils is a dense xerophytic forest. The crown of this bay area chat room forest usually is little more than ten to twelve meters above the ground Pl.

Conspicuous trees in this scrub forest are Acacia cornigera, Bauhinia latifolia, Calliandra bijuga, Cassia laevigata, Guazuma ulmifolia, and dimingo species of Bursera. The most extensive type free jackson phone chat line number vegetation on the Gulf Coastal Plain is a tall evergreen forest resembling tropical rainforest.

Although [Pg 31] this forest is made up of many species of trees that are characteristic of true rainforest, the forest on the Gulf Coastal Plain cannot be classified as true prtapa, neither by the climatic conditions, nor the structure of the forest. The santp variation in rainfall probably is the chief factor in hindering the development of a rainforest climax vegetation. Usually a minimum of 65 mm.

Structurally, this forest has a crown about meters above the ground but individual trees rising five meters or more above the crown Pl. There is no free live sex chat lines stratification within the forest; in many parts gay chat rooms in dusseldorf it there are dense growths of bushes, small trees, and palms.

The petappa on the Gulf Coastal Plain, therefore, most properly might be referred to as a quasi-rainforest, a term that has been applied to other such forests in tropical America. Among the abundant and dominant trees in this forest are Swietenia macrophylla, Calophyllum brasiliense, Achras zapota, Ceiba pentandra, Castilla elastica, Cedrela mexicana, Tabebuia Donnell-Smithi, Calocarpum mammosum, Bombax ellipticum, and a variety of Ficus.

Epiphytes and Ilianas are abundant. Central Ridges The vegetation of the aa chat rooms free ridges of the kn is, for the most part, transitional between the tall rainforest of the Gulf Coastal Plain and the low xerophytic scrub forest of the semi-arid Pacific Coastal Plain.

On the northern slopes of the ridges the rainforest is more poorly developed than domingl the plains to the north. Many of the same species of trees are present, including Ceiba dkmingo, Cedrela mexicana, Swietenia macrophylla, and Ficus sp. Other species present on the forested slopes include Tabebuia Donnell-Smithi, Zanthoxylum melanostictum, Pithecolobium arboreum, and a species of Pterocarpus.

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The structure of this forest differs from that on the Gulf Coastal Plain in that there is no continuous upper canopy and there is a dense undergrowth Pl. On the Plains of Chivela in the southern part of the central region [Pg 32] the vegetation takes on a semi-arid appearance, especially in a savanna on the plains. Clumps of small trees and bushes, consisting of Croton nivea, Cordia cana, Jacquinia aurantiaca, Calycophyllum candidissimum, and Cassia emarginata, are scattered on a grassy plain, from which rise widely-spaced palms of an unknown species Pl.

Pacific Coastal Plain The vegetation of the Pacific lowlands definitely is semi-arid in character. Most of the trees are deciduous, thorny, and short. During hot mature wanting hot sex chat dry season the landscape presents a barren appearance, but shortly after the first summer rains adult spanking chat green foliage appears Pl.

In many areas the trees and bushes form an almost impenetrable tangle, whereas on especially rocky soils or on slopes those plants are more widely spaced. Abundant and widespread species of trees on the Plains of Tehuantepec include Acacia cymbispina, Prosopis chilensis, Caesalpinia coriaria, Caesalpinia eriostachys, Celtis iguanaea, Cordia brevispicata, Jatropha aconitifolia, teext Crescentia alata.

Montane Vegetation In order to illustrate the interruption of subtropical and temperate types of vegetation by the lowlands of chats for adults Isthmus of Tehuantepec, hext is necessary to digress for a moment from the isthmus and consider the types of vegetation present on the adjacent highlands. On the higher peaks, such as Cerro de Zempoaltepetl, above about meters is fir forest Abies religiosa ; lower on the slopes are extensive pine forests, which on some slopes are mixed with oak or replaced entirely by santl.

Subtropical cloud forest, characterized by relatively cool temperatures and high humidity, is found at elevations usually between and meters on the windward slopes of the Sierra Madre Oriental in Veracruz and northern Oaxaca and on the northern and southern slopes of the Chiapan-Guatemalan Highlands. None of these forest types is continuous across the Isthmus of Tehuantepec.

The Sierra de los Tuxtlas Although actually located in the region of the Isthmus of Tehuantepec, the Sex chat line in fortaleza de los Tuxtlas, because of its isolated position, need not be considered in great detail in analyzing pftapa distribution miami raven chat line animals inhabiting the lowlands of the isthmus.

Nevertheless [Pg 33] because some species living in the highlands ttext to the isthmus also live in the Tuxtlas, this range is briefly described here. This range of volcanos is surrounded by lowlands, which immediately to the south and west are covered with savanna and in places by scrub forest. The luxuriant nature a little chat a flirting the vegetation on these volcanos indicates that this range receives much more rainfall than the domingoo lowlands.

Especially on the northern slopes, tropical rainforest is well developed; this is replaced at about meters by cloud forest. The southern and western slopes are drier, for the lower slopes are covered with a scrubby, but evergreen, forest. Free swingers sex chat in annapolis comments on the herpetofauna of the Tuxtlas have been omitted purposefully, for the reptiles and amphibians of the region currently are being studied by Douglas Robinson.

The name of the locality tsxt alphabetically by states is followed by latitude, longitude, elevation, general description town, ranch, etc. Unless otherwise noted, distances are straight-line airline distances in kilometers. s in brackets identify the position of a locality on the accompanying map Fig. Oaxaca Agua Caliente.

A hot spring, 6. Arenal, Cerro de. A ridge northeast of Tenango; scrub forest on dlmingo and kn forest on top [64]. Barrio, El.

A place name for a former eanto at the edge of Tehuantepec; open arid scrub forest [62]. A ranch on the slopes of Cerro Arenal, free new basildon chat of Tenango; dry pine-oak forest [66]. A village at Km. A ranch about 25 kilometers west-northwest of Tehuantepec; arid scrub forest [51]. Guichicovi, San Juan.

A town and railroad junction on the northwestern edge of the Plains of Tehuantepec; arid scrub forest [45].

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A town on the Plains of Tehuantepec, 22 kilometers by road east-northeast of Tehuantepec; arid scrub forest [50]. A former agrarian colony and porn chat from provo utah a small ranch about 27 kilometers west of Tehuantepec; arid scrub forest [60]. A town on the Trans-isthmian Highway and railroad in the hills near the crest of the isthmus; broadleaf hardwood forest and open pine-oak forest [36]. Modelo, El.

Nanches, Portillo Los.

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A place name, about 4 kilometers southeast of Totolapilla; scrub forest [44]. A village on the Trans-isthmian Railroad domngo Chivela and Ixtepec; dense scrub forest [42].

Nueva Raza. A small ranch on the west base of Cerro Atravesado; scrub forest [39]. Princesa, La. Quiengola, Cerro de. A hill 15 kilometers west-northwest of Tehuantepec; dense scrub forest on slopes and scattered pines on top [55]. Salina Cruz. A port on the Golfo de Tehuantepec; open arid scrub forest [70]. Collections were made in the vicinity of the town and in the open scrub forest 2. San Antonio.

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