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Oriental Basin

Oriental Basin is a earth science topic covered in the lgStudy science library. This page brings together a partial reference excerpt, illustrations, worked examples, real-world applications and a short study plan, so you can understand Oriental Basin rather than just read about it. In short: The Oriental Basin, also known as the Libres-Oriental Basin, Oriental-Serdán Basin or San Juan Plains (in Spanish, Llanos de San Juan or Cuenca de Libres-Oriental), is an endorheic basin in east-central Mexico. It covers an area of 4,958.60 square kilometers, lying in the states of Puebla, Tlaxcala, and Veracruz.

Oriental Basin — main illustration
Oriental Basin — illustration

Key takeaways

  • Oriental Basin belongs to earth science; place it in that map before memorising details.
  • Learn the definition first, then one example that makes the definition concrete.
  • Connect Oriental Basin to a quantity you can measure, compute or draw — that is where exam questions come from.
  • Reproduce the core statement of Oriental Basin from memory before moving on to harder problems.

Reference excerpt

The Oriental Basin, also known as the Libres-Oriental Basin, Oriental-Serdán Basin or San Juan Plains (in Spanish, Llanos de San Juan or Cuenca de Libres-Oriental), is an endorheic basin in east-central Mexico. It covers an area of 4,958.60 square kilometers, lying in the states of Puebla, Tlaxcala, and Veracruz. The climate is temperate and subtropical, semi-arid to subhumid, with summer rains. Average annual temperature 12-16 °C, and annual total precipitation is 400–800 mm. The Trans-Mexican Volcanic Belt pine-oak forests ecoregion covers the mountains surrounding the basin to the west, north, and east. The mountains to the north and west, including the Cofre de Perote volcano, leave the valley in a rain shadow, and the xeric shrublands of the Tehuacán Valley matorral ecoregion occupies the center of the basin, and extend south into the Tehuacán and Cuicatlán valleys. Vegetation includes pine-oak forests and pine-fir forests at higher elevations, with dry scrub pine forests, oak forests, juniper scrub, yucca scrub, halophytic vegetation, and grassland. It includes the Llanos de San Juan and Llanos de San Andres. The basin contains several shallow, mostly alkaline lakes. Two ephemeral playa lakes, Totolcinco (El Carmen or Totolcingo) and Tepeyahualco (El Salado), lie in the lowest part of the basin (2300 meters elevation), and remain dry for most of the year. The basin includes six maar lakes, locally called axalpazcos, lying in shallow volcanic craters and sustained by underground water. A northern group of lakes – Alchichica, Quechulac, Atexcac, and La Preciosa – lie southeast of Lake Tepeyahualco, and the southern lakes, Aljojuca and San Miguel Tecuitlapa, lie southeast of Lake Totolcinco. The basin also has five dry maars, called xalapazcos. Chief towns in the basin include El Carmen Tequexquitla, Tlaxcala; Perote, Veracruz; and Oriental, Puebla. Groundwater levels in the basin have been dropping in recent years because of over-exploitation for irrigation and destruction of natural recharging areas. In addition, the government is considering pumping freshwater from the Oriental basin to Mexico City to the west and Puebla to the south.

Maar lakes The maar lakes, or axalpazcos, of the Oriental Basin are home to a closely knit set of endemic species, one at each crater lake. Some of these include the Atherinopsid fishes Alchichica silverside (Poblana alchichica), La Preciosa silverside (P. letholepis), Chignahuapan silverside (P. ferdebueni), and Quechulac silverside (P. squamata). Three species of dace (Evarra bustamantei, E. eigenmanni, and E. tlahuacensis) formerly native to the basin are presumed extinct since about 1970. The WWF-Nature Conservancy system of freshwater ecoregions includes the Oriental Basin with the Valley of Mexico, Lerma River, and Lake Chapala in their Lerma-Chapala freshwater ecoregion, based on faunal similarities, especially among the Atherinopsids.

Lake Alchichica

Lake Alchichica (19°25′N 97°24′W) in Tepeyahualco (municipality), Puebla, is the largest of the maar lakes of the Oriental Basin, and lies at an elevation of 2320 meters. It is Mexico's deepest natural lake, with a maximum depth of 64 meters, and a mean depth of 38.6 meters. The lake has an area of 1.81 square kilometers. It is both saline and alkaline (pH 8.7-9.2). Lake Alchichica is ecologically unique, with stromatolite deposits and a high degree of endemism. The biota has adapted to extreme conditions characterized by high ionic concentrations of water and poor nutrient content. The dominant stromatolite species are the spongy type Enthophysalis atrata, Enthophysalis sp. Calothrix cf. Parletina and Calothrix sp. and the columnar stromatolites Enthophysalis lithophyla and Nitzschia sp. In the deep parts of the lake, abundant cladophores develop on the spongy stromatolites, with many cyanobacterial epiphytes Chamaesiphon halophilus, Heteroleibleinia profunda, Mantellum rubrum and Xenococcus candelariae. 23 genera of phytoplankton have been found: fourteen genera of Chrysophyta, five of Cyanophyta and four of Chlorophyta. The dominant species throughout the year are Agmenellum sp., Amphora sp., Chaetoceros similis, Coscinodiscus sp., Cyclotella striata, Nodularia spumigena, Stephanodiscus niagarae and Synechocystis sp. The best represented species best of vascular plants in the axalpazcos are rooted emergent hydrophytes Eleocharis montevidensis, Juncus andicola, J. balticus subsp. mexicanus (syn. J. mexicanus), Phragmites australis, Scirpus californicus and Typha domingensis, the submerged rooted hydrophytes Cyperus laevigatus, Potamogeton pectinatus and Ruppia maritima, and the free-floating hydrophyte Lemna gibba. Animals endemic to Lake Alchichica include the Taylor's Salamander (Ambystoma taylori), the fish Poblana alchichica (Alchichica silverside, Charal de Alchichica), and the isopod Caecidotea williamsi.

References

Illustrations

Oriental Basin illustration
Oriental Basin: Atexcac Lake
Atexcac Lake

Worked examples

Example 1 — a first encounter with Oriental Basin

Start with the simplest possible case. Write down what Oriental Basin claims or describes in one sentence, then invent the smallest concrete situation in which that sentence is true. In earth science, the smallest case is usually a single object, a single equation or a single measurement. Check that every symbol or term in your sentence has a meaning in that case.

Example 2 — changing one variable

Take the situation from Example 1 and change exactly one quantity: double it, halve it, or set it to zero. Predict what should happen to Oriental Basin before you calculate. Comparing your prediction with the result is the fastest way to find out whether you understand the idea or only the words.

Example 3 — an exam-style question

Typical questions about Oriental Basin ask you to (a) state it precisely, (b) apply it to given data, and (c) explain a limitation. Practise writing all three answers in under five minutes; the third part is what separates a full-mark answer from an average one.

Applications of Oriental Basin

In research
Oriental Basin appears in earth science research whenever the underlying quantities have to be modelled precisely. Papers usually cite it as a starting assumption and then explore where it breaks down.
In technology and industry
Engineering practice reuses Oriental Basin in design rules, simulations and safety margins. Knowing the idea lets you read a specification sheet and understand why the numbers look the way they do.
In the classroom
Oriental Basin is common in secondary-school and first-year university syllabi. It links to neighbouring topics Drainage basins of Mexico, Endorheic basins of North America, Flora of Central Mexico, so understanding it makes those chapters shorter.
In everyday life
Look for Oriental Basin outside the textbook — in sport, cooking, traffic, electronics or the sky above you. An example you found yourself is remembered far longer than one you were given.
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How to study Oriental Basin in 20 minutes

  1. Read the reference excerpt below once, without taking notes.
  2. Close the page and write down what Oriental Basin means in your own words.
  3. Compare your version with the excerpt and mark what you missed.
  4. Work through the three examples above with pen and paper.
  5. Explain Oriental Basin out loud to somebody else — or to Teacher Smith in the lgStudy chat.

Frequently asked questions

What is Oriental Basin in simple terms?

The Oriental Basin, also known as the Libres-Oriental Basin, Oriental-Serdán Basin or San Juan Plains (in Spanish, Llanos de San Juan or Cuenca de Libres-Oriental), is an endorheic basin in east-central Mexico. It covers an area of 4,958.60 square kilometers, lying in the states of Puebla, Tlaxcala…

Why does Oriental Basin matter?

Because it connects several earth science ideas at once: it gives you a definition you can apply, a quantity you can calculate, and a way to check whether a result is plausible.

How should I study Oriental Basin?

Read the excerpt, restate it from memory, then work through the examples and applications listed on this page. The five-step study plan above takes about twenty minutes.

What does this page cover?

It gives you a compact reference excerpt plus original lgStudy explanations, examples, applications and study material on Oriental Basin.

Tags

  • Drainage basins of Mexico
  • Endorheic basins of North America
  • Flora of Central Mexico
  • Landforms of Puebla
  • Landforms of Tlaxcala
  • Landforms of Veracruz
  • Maars of Mexico
  • Oriental Basin
  • Tehuacán Valley matorral
  • Trans-Mexican Volcanic Belt

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