Location & Continent
Continent: Australia
Country: Australia (Northern Territory, South Australia, Queensland)
Coordinates: 24°34′S, 137°25′E
Simpson Desert – Map & Street View
Photos of the Simpson Desert

Physical Features
Area: ~170,000–180,000 km² (depending on boundary definition; often cited as ~176,500 km²)
Relief & Extent: A vast erg dominated by long, parallel sand ridges that can run for over 100 km; swales host claypans and ephemeral playa lakes.
Elevation: ~50–300 m across low plains and dune crests; prominent dune known as “Big Red” (Nappanerica) reaches ~40 m above surrounding flats.
Climate & Precipitation
Temperature: Summers are intensely hot; daytime maxima regularly exceed 40–45 °C in exposed basins. Winters are cooler with crisp nights and occasional frosts in swales.
Precipitation: ~125 mm median annual rainfall, highly variable and often delivered by summer thunderstorms; evaporation far exceeds rainfall, sustaining true desert conditions. After rare widespread rains, the desert “greens up” dramatically with wildflowers and ephemeral wetlands.
Ecological Features
Ecozone: Australasia Biome: Deserts & xeric shrublands (hot desert)
Ecoregion / IBRA: Simpson–Strzelecki Dunefields — hummock grasslands (spinifex) with acacia shrublands, scattered coolibah and river red gum along drainage lines.
Hydrology: Underlain by the Great Artesian Basin; discharge at mound springs (e.g., Dalhousie Springs) creates permanent oases.
Flora & Fauna
Flora: Dominant spinifex hummocks (Triodia spp.), sandhill canegrass (Zygochloa paradoxa) on dune crests, mulga (Acacia aneura), gidgee (Acacia cambagei), saltbush and ephemeral herbs following rain.
Fauna: Crest-tailed mulgara (Dasycercus cristicauda), southern marsupial mole (Notoryctes typhlops), plains mouse (Pseudomys australis), Eyrean grasswren (Amytornis goyderi) in canegrass, reptiles such as thorny devil and sand goannas, and wide-ranging dingoes. On the eastern margins and nearby grasslands, conservation programs for the greater bilby intersect with Simpson Desert habitats.
Geology & Notable Features
Geology: Quaternary aeolian sands over older basin sediments; dunes trend chiefly NW–SE under prevailing winds. Numerous claypans/playas (e.g., Lake Caroline) punctuate interdune corridors and influence dune erosion/reshaping along their margins.
Notable Features: Big Red (Nappanerica) near Birdsville; Poeppel Corner tri-state marker; historic 4WD routes (French Line, QAA Line, Rig Road, Madigan Line); Dalhousie Springs in adjacent Witjira NP; large protected estates including Munga-Thirri–Simpson Desert National Park (SA) and Munga-Thirri National Park (QLD).
Seasonal Access: Annual summer closure ~1 Dec – 15 Mar for safety across SA & QLD desert parks; always check current park alerts.
Introduction
The Simpson Desert (Wangkangurru Yarluyandi: Munga-Thirri) is Australia’s classic red-dune desert. Its sea of linear ridges, some stretching for hundreds of kilometres, forms one of the world’s most striking dune landscapes. Although rainfall is scant and erratic, pulses of moisture transform the dunefield—spinifex hummocks flush green, canegrass bends in the wind, and claypans briefly host waterbirds and invertebrate blooms. This page dives into what makes the Simpson unique, from its geology and climate to its living oases fed by ancient groundwater.
Geography
Spanning the NT–SA–QLD borderlands of central Australia, the Simpson is bounded by the Finke River and MacDonnell Ranges to the west/north, desert channels like the Diamantina to the east, and the Kati Thanda–Lake Eyre basin to the south. It is renowned for parallel dunes that maintain near-constant spacing and orientation across vast distances, separated by flat, often clay-rich swales and saltpan basins.
Climate
The Simpson sits within Australia’s core arid belt. Rain arrives mainly via summer convective storms, with strong year-to-year variability; median annual totals hover near ~125 mm. Potential evaporation dwarfs rainfall, so even “wet” years dry quickly. Heat extremes are common in late spring–summer; winter brings sunny days and cold, still nights.
Vegetation
Dune crests support canegrass and spinifex that anchor the sand ridges, while swales host acacia shrubs, forbs and annuals after rain. This patchwork creates micro-habitats for specialized fauna—from burrowing marsupials in loose sands to granivorous birds moving between seed flushes.
Wildlife
Despite harsh conditions, the Simpson harbours a resilient biota adapted to boom-and-bust cycles. Notable species include:
- Crest-tailed mulgara — a small carnivorous marsupial thriving on dune flanks and swales.
- Southern marsupial mole — a sand-swimming specialist rarely seen on the surface.
- Eyrean grasswren — a signature bird of canegrass dunes in the Simpson and Strzelecki deserts.
- Thorny devil — iconic lizard with capillary skin channels for water uptake.
- Greater bilby — conservation efforts on the Simpson’s eastern margins and nearby grasslands contribute to regional recovery.
Following major rains, irruptions of rodents and insects ripple through the food web, drawing raptors and other predators.
Comparison with Other Australian Deserts
| Feature | Simpson Desert | Great Sandy Desert | Great Victoria Desert |
|---|---|---|---|
| Location | NT–SA–QLD | WA (north) & NT | WA & SA |
| Dominant Landforms | Long parallel dunes; claypans | Linear dunes; sandplains | Dunes & gibber plains; salt lakes |
| Median Rainfall | ~125 mm | ~223 mm | ~162 mm |
| Iconic Features | Big Red; Poeppel Corner; Dalhousie Springs (adjacent) | Tanami edge, monsoonal influence north | Nuclear-test history sites; vast wilderness blocks |
Culture and Human Activity
The Simpson is the traditional Country of Aboriginal peoples including Wangkangurru Yarluyandi, with deep cultural ties to springs, dunes and songlines. Today, experienced visitors undertake remote 4WD crossings via historic seismic tracks. For safety and conservation reasons, cross-border desert parks enact a summer closure (typically 1 December – 15 March) and require proper vehicle preparation, recovery gear, visibility flags, and up-to-date park permits.
Conservation & Management
Large protected areas—Munga-Thirri–Simpson Desert National Park (SA) and Munga-Thirri National Park (QLD)—safeguard representative dunefields, playa systems and wildlife. Management focuses on visitor safety, invasive species control, fire regimes in spinifex grasslands, and partnerships with Traditional Owners. Long-term university research plots track biodiversity responses to rain pulses, fire, and predators, strengthening evidence-based management.
Conclusion
With its textbook parallel dunes, groundwater oases and pulse-driven ecology, the Simpson Desert is a living laboratory for arid-zone processes—and an unforgettable landscape for well-prepared travelers. Respect seasonal closures, plan conservatively, and you’ll witness how this desert oscillates between austere quiet and spectacular bursts of life after rain.
References
- National Parks SA — “Munga-Thirri–Simpson Desert National Park: access, summer closure & safety”
- Queensland Parks — “Munga-Thirri (Simpson Desert): park overview and visitor advice”
- Bureau of Meteorology — “Australian climate classification maps (arid interior)”
- Queensland Parks — “Simpson Desert (QAA Line) camping & alerts (seasonal closure & conditions)”
- University of Sydney — “Desert Ecology Research Group (long-term plots in the Simpson)”
- AGU Journal — “Temporal observations of a linear dune in the Simpson Desert”
- NASA Earth Observatory — “Simpson Desert, Australia (parallel dunes >100 km)”
- Wikipedia — “Simpson Desert (area, coordinates, features)”


