Australia's major cities—Sydney, Melbourne, Brisbane, Perth, Adelaide—all cling to the coast. The vast interior (the Outback) remains sparsely settled. Six interlocking factors explain why:
Arid/semi-arid zones dominate. Summer temperatures regularly exceed 45°C (113°F); rainfall is scarce and unpredictable.
Surface water is nearly absent. Groundwater (Great Artesian Basin) exists but is finite, often saline, and expensive to extract. Coastal cities tap reliable river and reservoir systems.
Colonization began at coastal ports (Sydney 1788, Hobart 1804, etc.). Inland exploration came later, revealing hostility to agriculture. Coastal capitals became administrative/commercial anchors; the interior never caught up.
Building inland cities requires massive infrastructure (water pipelines, power, transport) with limited economic return. Mining towns (e.g., Kalgoorlie, Mount Isa) exist but remain small, company-dependent, and cyclical.
Distance, terrain, and climate make roads/rail expensive to build and maintain. The Indian Pacific and Ghan railways cross the continent but serve freight/tourism—not daily commuting.
Isolation, extreme heat, limited services (health, education, retail), and few jobs deter permanent settlement. Fly-in-fly-out (FIFO) work dominates resource sectors.
Climate change may worsen interior habitability. For now, Australia remains a coastal nation by necessity.