Sierra de las Quijadas National Park

Sierra de las Quijadas National Park

Location: 104 mi (167 km) Southeast of San Juan, San Luis Province   Map

Area: 150,000 hectares

Open: 8am- 9pm daily

Info: San Luis

Tel. (02652) 445 141

Official site

 

Sierra de las Quijadas National Park (Parque Nacional Sierra de las Quijadas) sits in northwestern San Luis Province, Argentina, roughly 116–125 km northwest of San Luis city via Ruta Nacional 147 near the paraje of Hualtarán (around km 922–923). The entrance is a further 7–8 km along a graded dirt/gravel road. Established in 1991, it covers about 73,785 hectares and protects the transition between the semi-arid Chaco and Monte of plains and plateaus ecoregions. It is also a Ramsar wetland site.
The landscape is dominated by striking reddish sandstone cliffs, canyons, and eroded formations carved over millions of years by wind and occasional rain. The signature feature is Potrero de la Aguada, a vast natural amphitheater of red and ochre rock walls and layered terraces. The area is paleontologically rich, with Cretaceous dinosaur footprints (including theropod and sauropod tracks) and fossils such as the pterosaur Pterodaustro. Archaeological evidence of pre-Hispanic occupation (including the Hornillos de Hualtarán ceramic-production site, roughly 1,000 years old) adds cultural depth.

 

Visiting tips

Best Time to Visit
Visit from April to October for milder temperatures (daytime highs often 15–22°C / 59–72°F), clearer skies, and lower humidity. Summer (especially January–February) brings extreme heat that can exceed 35–40°C (95–104°F), with trails sometimes restricted or closed for safety if temperatures at the start of a hike reach 33°C (Guanacos) or 35°C (guided trails). Rainfall is low overall (~300 mm annually) but concentrated from late spring into early autumn and can close trails or make the access road slippery. Weekdays outside Argentine school holidays are quieter.

Hours, Fees, and Access
The park is open every day, including holidays, from 8:00 to 19:00, with last entry at 17:00. Recent reports (including official social media and provincial sources) indicate free entry at present, though fees have been listed in the past and the Administración de Parques Nacionales (APN) site shows tariff categories. Always confirm current status before traveling, as policies change with inflation and regulations. Guided trails require a paid authorized guide (arrange in advance; costs vary but are typically modest).
There is no public bus service directly to the park. Rent a car or hire a taxi/tour from San Luis (or from Merlo, San Juan, or Mendoza). The closest commercial airport is Brigadier Mayor César Raúl Ojeda (LUQ) in San Luis, with flights from Buenos Aires. From the RN 147 turnoff, the final dirt section is generally passable in dry conditions but check road status after rain. Drive slowly for wildlife (guanacos, armadillos, etc.).

Trails and Activities
Several trails of varying difficulty start near the visitor/information area and parking. Some are self-guided; others require a guide or prior registration. Official details include:

Miradores (self-guided): ~2.2 km / 1.5 hours, low difficulty. Panoramic views of the Farallones cliffs and Potrero de la Aguada; the main accessible overlook experience.
Flora (self-guided): ~1.3 km / 45 minutes, low difficulty. Interpretive trail highlighting native plants adapted to arid conditions (signage with common and scientific names).
Huellas del Pasado (guided): ~3 km / ~2.5 hours, medium difficulty. Focuses on paleontology and geology; includes dinosaur footprints and endemic flora such as the chica bush.
Guanacos (self-guided with registration at the information office): ~5 km round-trip / ~3 hours, high difficulty. Rougher terrain with views of the farallones and southern Potrero; good chance to see guanacos.
Farallones (guided): ~9 km round-trip / ~4 hours, high difficulty. Descends toward the base of the red cliffs.

Guided departures have fixed windows (earlier in summer due to heat). Birdwatching is excellent (over 200 species, including Andean condors, yellow cardinals, and others); best early morning or late afternoon. Photography is outstanding, especially with the warm late-afternoon light on the red rock.

Practical Tips and Facilities
Bring at least 2 liters of water per person (more in heat); there is no potable water on the trails and limited or non-potable water at facilities. Pack a hat, sunscreen, sunglasses, closed comfortable shoes, light snacks, and insect repellent. Shade is scarce. Thermal amplitude is high, so layers help. No pets are allowed.
Facilities include a visitor/information area, bathrooms, picnic tables with grills, and a free basic campsite (limited sites, shared bathrooms with cold showers, tables, fire pits; suitable for tents or small RVs). A small store/restaurant is nearby on the RN 147 or about 500 m from the entrance for basics, empanadas, or regional food (hours may be limited, often Thursday–Sunday). Stock up in San Luis for longer stays. Wi-Fi is available in the information/parking zones.
Contact the park for trail status, guides, or questions: WhatsApp 266 473-2754 (daily during open hours), email sierradelasquijadas@apn.gob.ar, or phone 0266-473-2762 / 0266-444-5141. Follow the official Instagram (@pn.sierradelasquijadas) for updates.
Base yourself in San Luis city for more lodging, restaurants, and services (1.5–2.5 hours away), or look for simple options closer if available. The park pairs well with other San Luis attractions or a broader Cuyo circuit including places like Ischigualasto.
Respect the fragile environment, stay on marked trails, and check conditions the day of your visit. The combination of dramatic geology, fossils, and relatively light crowds makes it a rewarding, less-visited destination compared with better-known Argentine parks.

 

Geography

Topography and Landforms
Elevations range mainly from under 500 m above sea level in the Desaguadero River valley to 500–900 m across most of the sierra, with peaks approaching or exceeding 900–1,090 m. Notable heights include Cerro El Portillo and Cerro El Lindo (below ~1,090 m), Cerro Los Viejos (~920 m), and Cerros de la Aguada and Cerros de la Vidriera (~850 m). The landscape divides into six main physiographic units: the Desaguadero River flood plain, the circular/enclosed Arroyo de la Aguada valley, steppe, foothills, slopes, and summits.
The dominant visual character is dramatic arid badlands and eroded red sandstone sierras. Water and wind erosion have sculpted intense reddish (umber/ochre) cliffs (farallones), sheer walls, ravines, canyons, rock towers, terraces, and labyrinthine formations. The signature feature is the Potrero de la Aguada, a vast natural amphitheater or micro-basin in the heart of the sierra. It is enclosed by steep, stratified reddish sandstone and conglomerate walls, with erosion creating capricious shapes, balconies, and intricate terrain across thousands of hectares. Temporary watercourses drain this basin toward the Arroyo de la Aguada.
Eastern slopes tend to be gentler; western ones are more abrupt, with narrow quebradas. The overall relief emerges from surrounding arid plains.

Geology and Geological History
The park lies in the San Luis Basin, with sedimentary, metamorphic, and igneous outcrops of various ages. A major north–south fracture (subparallel to the Desaguadero River) lifted the Quijadas range. The basin is bounded eastward by the Sierra de San Luis and connects westward subsurface to Triassic basins in Mendoza and San Juan provinces; it extends northward toward Marayes.
Geological development involved three main stages:

Infill (~120–100 million years ago): A sedimentary basin flanked by highlands (including ancestral Sierras de San Luis and a range along the Desaguadero course) filled with fluvial, aeolian, and lacustrine sediments, accumulating more than 1,000 m of material.
Uplift and folding (beginning ~25 million years ago in the Tertiary, linked to Sierras Pampeanas and Andean processes): Layers were raised and folded. Uplift continues with the westward migration of the South American Plate.
Erosion: Concurrent with and after uplift, creating the modern valleys, ravines, and amphitheaters such as Potrero de la Aguada.

Key Lower Cretaceous formations exposed in the park (part of the broader Mesozoic red-bed sequences of central-western Argentina’s basins) include:

El Jume Formation (~120 mya, oldest): Outcrops prominently in Potrero de la Aguada; ~300 m thick alternating red sandstones and claystones from fluvial, aeolian, and lacustrine settings. It includes a notable paleolake mud column.
El Toscal and La Cruz Formations (~110 mya): Widespread, forming much of the reddish, whitish, and gray cliffs and gorges from high-energy fluvial environments. La Cruz includes basaltic lava layers (~109–107 mya).
Lagarcito Formation (~100 mya): Eastern slopes, dominated by claystones with some sandstones deposited in interconnected lakes; famous for exceptional fossil preservation.

A Tertiary San Roque Formation (~25 mya) of conglomerates, sandstones, claystones, and gypsum appears in low hills, along with Quaternary fluvial/aeolian deposits (sands, silts, loess-like materials) and younger alluvial/lacustrine/salt-flat sediments in flood plains and wetlands. The sequence documents continental arid-to-semiarid environments across much of the Mesozoic (Triassic through Cretaceous).
Paleontologically, the park is significant, especially the Lagarcito Formation’s Loma del Pterodaustro site (Konservat-Lagerstätte), which yielded abundant, well-preserved fossils of the filter-feeding pterosaur Pterodaustro guinazui (with its distinctive upward-curved jaws and fine teeth), fish, invertebrates, and early plant remains. Other vertebrate tracks and fossils occur in the formations.

Climate and Hydrology
The climate is semi-arid to arid serrano (continental arid), with pronounced daily and seasonal temperature swings. Annual precipitation averages roughly 250–300 mm, scarce and unevenly distributed—mainly late spring to early autumn (summer rains), with a dry winter. Relative humidity averages around 55%. Temperatures: average annual maximum ~24°C, minimum ~11°C; January monthly averages near 31°C (with highs often 35°C+ and occasionally exceeding 40°C); July minima near 3°C or below freezing. Extreme thermal amplitude is typical.
Hydrology is dominated by ephemeral streams fed by storm runoff; surface rocks erode readily. The Potrero de la Aguada acts as a closed catchment that concentrates rainwater and discharges it via the Arroyo de la Aguada into the Desaguadero River. The Desaguadero forms a western boundary (also an interprovincial limit with Mendoza) and creates a broad flood plain with saline influences. The park includes portions of the Lagunas de Guanacache wetland complex (a Ramsar site of international importance), historically a larger system linked to Andean river inflows, now reduced with salt flats and intermittent water bodies.

Broader Geographic Context
The park occupies a critical ecotone (transition zone) between Dry Chaco woodlands (with quebracho blanco and algarrobo) and the shrub-dominated Monte plains and plateaus (jarillas/Larrea, cacti, and other xerophytes). Vegetation is generally sparse and adapted to aridity; soils and land cover reflect the arid steppe and eroded sedimentary terrain. It preserves a unique sample of this transitional biogeography in west-central Argentina, alongside its geological and paleontological values (it is on UNESCO’s Tentative List for natural criteria related to outstanding landscapes, geology, and ecosystems).

 

Flora and fauna

Flora
The vascular flora is adapted to aridity, intense sun, poor soils, and erosion. Inventories record roughly 356–416 species (including infraspecific taxa; about 3.6% of Argentina’s flora in the more detailed count), in ~208 genera and 58 families. Dicots dominate (~74%), followed by monocots (~25%), with a few ferns and gymnosperms (Ephedra). The best-represented families are Poaceae, Asteraceae, Fabaceae, Solanaceae, Verbenaceae, and Bromeliaceae (together ~56% of species). Life forms emphasize drought adaptation: phanerophytes and hemicryptophytes (~24% each), chamaephytes (~22%), and therophytes (~16%).
Vegetation communities include:

Mixed open forests and groves with white quebracho (Aspidosperma quebracho-blanco) and algarrobo/mesquite (Prosopis spp., especially P. flexuosa), plus contributions of chañar and other Chaco elements.
Shrubby steppes dominated by jarillas (Larrea spp., Zygophyllaceae), typical of the Monte, along with garabato, brea, and other thorny shrubs.
Cacti (tunas, cardons, columnar and smaller forms) and bromeliads (chaguares, air plants/claveles del aire).
Gallery or riverine vegetation, halophyte rings on saline flats, pajonales (tussock grasslands), and rushes.
Rocky slopes with specialized slow-growing woody plants.

Endemics and notable species: Four taxa are exclusive (or nearly so) to the park and immediate surroundings—Atriplex quixadensis (Chenopodiaceae/Amaranthaceae), Senecio hualtaranensis (Asteraceae), Sclerophylax difulvioi (Solanaceae), and Gomphrena colosacana var. andersonii (Amaranthaceae). Many of these and other endemics face threats from restricted range, erosion, and human activity; several are critically endangered, endangered, or vulnerable. About 120 Argentine endemics occur in the park. The emblematic chica (Ramorinoa girolae) is a slow-growing, extremely hard-wooded shrub or small tree of rocky Monte slopes; it is nearly leafless, with green photosynthetic stems/branches, deep roots, and infrequent yellow-orange flowers.
Invasive/introduced plants include ~17 species, notably French tamarisk (Tamarix), which forms dense stands along streams. Overall, the flora shows strong adaptation to prolonged drought via reduced leaves, deep roots, water storage (succulents), and other xerophytic traits. Historical grazing and clearing have degraded some woodland patches, with restoration efforts underway after removal of unauthorized livestock.

Fauna
About 270 vertebrate species have been recorded (including a few introduced), reflecting the ecotonal mix of Chaco, Monte, Andean, and some Patagonian influences. Biodiversity is high for an arid zone, with important threatened taxa.
Mammals include:

Guanaco (Lama guanicoe), often in open areas.
Maras: Patagonian mara (Dolichotis patagonum) and Chacoan mara / conejo de los palos (D. salinicola).
Collared peccary (Pecari/Dicotyles tajacu) and gray brocket deer / corzuela parda (Mazama/Subulo gouazoubira).
Predators: puma (Puma concolor), gray fox / zorro gris pampeano (Lycalopex gymnocercus), Geoffroy’s cat, and others.
The endangered pink fairy armadillo / pichiciego menor (Chlamyphorus truncatus), a small fossorial specialist.
Other rodents (viscachas, cavies, tuco-tucos) and smaller carnivores.

Birds number in the 140–190 range in various counts. Highlights include the Andean condor (Vultur gryphus, using cliffs for roosting), black-chested buzzard-eagle / águila mora (Geranoaetus melanoleucus), the endangered crowned solitary eagle / águila coronada (Buteogallus coronatus), elegant crested tinamou / martineta (Eudromia elegans), various tinamous, raptors, and the Andean swift / vencejo blanco (Aeronautes andecolus), an aerial specialist that nests in crevices. Other notes include blue-crowned parakeet, yellow cardinal, and Monte endemics such as sandy gallito.
Reptiles and amphibians: Herpetofauna includes ~25 species (earlier lists; more in broader SIB data). Emblematic is the Argentine/Chaco tortoise (Chelonoidis chilensis), which digs burrows for summer heat refuge and winter hibernation, feeds on cacti, plants, insects, and snails, and is threatened by pet trade. Others include Argentine boa (Boa constrictor occidentalis), Darwin’s tree iguana and other Liolaemus, tegus (Salvator), various snakes (yarará, rattlesnake, colubrids), geckos, and amphibians such as the Mendoza four-eyed frog / escuercito (Pleurodema nebulosum) and common toad (Rhinella arenarum). Many are adapted to arid or rocky habitats.
Paleontological significance adds depth: Cretaceous formations (notably Lagarcito) have yielded abundant fossils, including the filter-feeding pterosaur Pterodaustro guinazui.

Conservation Context
The park is critical for endemic plants, the crowned eagle, pink fairy armadillo, tortoise, and connectivity of the Chaco–Monte transition. Challenges include invasive plants (tamarisk), historical grazing and clearing (partial recovery efforts noted), climate pressures, and limited water. Official emblems often highlight the tortoise, chica, and Andean swift. Trails allow observation of characteristic vegetation and wildlife such as guanacos and maras, with interpretive signage.