Why Are Landforms Important to Life on Earth?

Landforms shape nearly every condition that life depends on, from where rain falls and rivers flow to which species evolve and where people settle. Mountains alone cover roughly a quarter of Earth’s land surface yet harbor more than 85% of the world’s amphibian, bird, and mammal species, a concentration of biodiversity that hints at how profoundly terrain influences living systems.¹ The story goes well beyond mountains, though: river valleys, floodplains, coastlines, caves, and even shallow depressions in the ground all create distinct conditions that steer ecology and evolution in ways most people never consider.

Mountains and the Outsized Concentration of Species

If you spread a map of global biodiversity across a table, the bright spots cluster along mountain ranges. The Andes, the Himalayas, the East African highlands, the mountains of Borneo: these regions host far more species per unit area than the flatlands around them. Topographically complex regions on both land and in the oceans consistently feature biodiversity hotspots, a pattern that reflects the deep geological influence terrain has on ecological and evolutionary processes.² The reasons are partly intuitive: as you climb a mountain, temperature drops, moisture changes, wind picks up, and soils shift. Each elevation band becomes a different world. But research on small mammals has shown that it is not just the presence of a mountain that matters. The magnitude and rate of tectonic uplift itself increases biodiversity, meaning that more dramatic and faster-rising landscapes generate more species over time.³

This makes sense when you think about what rising terrain does. As a landscape buckles upward, it fragments habitats, creates new climate zones, and throws up physical barriers between populations. Organisms that once moved freely across a region suddenly find themselves separated by ridges, deep valleys, or stretches of unsuitable climate. Over thousands of generations, those isolated populations diverge into distinct species. Mountains are not just places where species live; they are engines that manufacture new species.

How Landforms Drive Speciation

The relationship between physical barriers and new species is one of the most compelling stories in evolutionary biology. In the tropical Andes, researchers traced the evolutionary histories of 14 animal groups and identified 26 distinct events where populations were split apart and then diversified. The barriers responsible were not random. They corresponded to warm or dry river valleys, sudden changes in elevation, and high peaks separating populations on opposite slopes.⁴ In other words, the specific shape of the land determined exactly where lineages split.

Rivers work similarly, though with some nuance. In Madagascar, genomic work on Gerp’s mouse lemur showed that the barrier effect of a river depends on the river’s size and how far inland its headwaters reach. Populations separated by the largest river in the study area, one with headwaters extending deep into the highlands, showed especially high genetic divergence. Smaller rivers with lower-elevation headwaters were “leakier” barriers, allowing more mixing.⁵ A parallel finding comes from Amazonian forest birds, where rivers acted as barriers that promoted speciation, though with periods of gene flow breaking through. Some populations went hundreds of thousands of years without exchanging genes across a major river, long enough for substantial evolutionary divergence to accumulate.⁶

Islands, the ultimate geographic isolators, take this process even further. When a volcanic island chain rises from the sea, each island becomes a laboratory for independent evolution. Hawaiian spiders, for example, have repeatedly evolved the same body forms on different islands, a pattern called ecomorph radiation. Isolation combined with ecological opportunity produces species that converge on similar designs even though they evolved independently.⁷

Mountains as the World’s Water Towers

Beyond biodiversity, landforms determine where freshwater goes, and therefore where life can thrive. Mountains intercept moisture-laden air, force it upward, and wring out precipitation as rain or snow. The runoff feeds rivers that sustain billions of people and countless ecosystems downstream. This “water tower” function is especially critical in dry regions: in the world’s semiarid and arid zones, mountain contributions account for roughly 50 to 90% of total river discharge.⁸ Cities like Lima, Cairo, and much of Central Asia exist because mountains far upstream collect and release water that would otherwise never reach the lowlands.

Identifying exactly where this disproportionate contribution is greatest matters for water management. A global mapping effort found that the critical regions are those where mountain runoff vastly outpaces what surrounding lowlands produce on their own.⁹ When mountain snowpacks shrink due to warming temperatures, the consequences ripple hundreds or thousands of kilometers downstream. The landform itself is the infrastructure that makes entire agricultural systems and urban centers viable.

Landforms as Climate Refuges

One of the less obvious gifts that terrain offers life is protection from climate extremes. When global temperatures swing, as they have repeatedly over Earth’s history, organisms need places to ride out the change. Landforms provide these refuges.

In alpine landscapes, the uneven surface creates a patchwork of microclimates within very short distances. A single mountainside can show temperature differences of more than 7°C in mean soil temperature and over 10°C in surface temperature between its warmest and coolest micro-habitats, with growing seasons varying by more than 32 days. This means that even if regional temperatures rise by a couple of degrees, most alpine species can find a cooler spot within a short walk rather than needing to migrate to a higher latitude. Alpine landscapes, because of their topographic variability, are likely safer places for most species than lowland terrain in a warming world.¹⁰

Rock faces and crevices play a similar role at smaller scales. In the Pyrenees, researchers found that cliffs and rock crevices buffer extreme temperatures, protecting relict plant species that would otherwise be vulnerable to both historical and modern climate shifts. The high proportion of endemic and isolated plant populations found in rocky habitats across the range suggests that this buffering effect has been protecting species through repeated climate changes over long periods.¹¹ Even small topographic depressions matter. Sinkholes in karst landscapes, sometimes just a few dozen meters deep, maintain cooler and more humid conditions than surrounding terrain, providing refuge for climate-sensitive species that would struggle on the exposed surface above.¹²

Shaping Weather Patterns and Monsoons

Landforms do not just respond to climate. They actively create it. The most dramatic example is probably the Tibetan Plateau, a massive highland whose uplift over millions of years reshaped atmospheric circulation across Asia. Climate modeling experiments show that the evolution of the East Asian monsoon is closely tied to the rise of the plateau. The winter monsoon system in northern China, with its characteristic northerly winds, appears to have formed when the plateau reached roughly half its current height. The plateau’s influence on the East Asian winter monsoon is more pronounced than its effect on summer monsoon patterns, and more significant than its impact on the South Asian monsoon overall.¹³ Sediment records from basins near the plateau confirm this connection, with changes in vegetation and climate markers tracking both regional tectonic uplift and global cooling over the last several million years.¹⁴

On a smaller scale, mountain ranges create rain shadows. When moist air hits a mountain range, it rises, cools, and dumps its moisture on the windward side. The leeward side gets far less rain, sometimes dramatically less. In the Andes, drier regions receiving less than 1,500 mm of annual precipitation correspond to areas with unfavorable topographic orientation relative to prevailing winds, combined with reduced cloudiness from local breezes.¹⁵ In southern New Zealand, the uplift of the Southern Alps created a rain shadow that progressively dried out the eastern side of the island over the Pliocene and Quaternary periods. That aridification did not just change the climate. It drove fish speciation, as populations became isolated in increasingly different habitats on opposite sides of the mountain barrier.¹⁶

How Terrain Distributes Soil Nutrients

The shape of the land also governs where nutrients accumulate and where they wash away, which in turn determines what grows where. Water flows downhill, carrying dissolved minerals and organic matter with it, but the relationship is not as simple as “valleys are fertile and hilltops are barren.” Research in silvopasture systems found that nutrients like sulfur, calcium, zinc, iron, and total nitrogen increased in wetter, lower-lying areas, while sodium concentrated at higher slope positions.¹⁷ Slope aspect, the compass direction a hillside faces, independently influenced phosphorus and magnesium levels. The result is a mosaic of soil chemistry shaped almost entirely by the contours of the terrain.

In China’s dry-hot valleys, researchers found that total nitrogen and organic matter declined as slopes got steeper, while phosphorus accumulated in the gentler parts of the landscape. At the same time, organic matter and available potassium increased at higher slope positions, and total phosphorus decreased with elevation.¹⁸ In southern Ethiopia, a somewhat counterintuitive pattern emerged: organic carbon, total nitrogen, and several key cations were lower on lower slopes than on upper and middle slopes, likely because coarse sediments deposited by gully erosion diluted the nutrient concentrations.¹⁹ The takeaway is that landform does not just decide whether soil is fertile. It decides which nutrients end up where and in what concentrations, creating fine-grained habitat differences that shape plant communities and, ultimately, the animals that depend on them.

Floodplains, Rivers, and Freshwater Ecosystems

Where rivers spread out across wide gravel beds in mountain valleys, they create some of the most ecologically productive habitats on the planet. Gravel-bed river floodplains in mountain landscapes concentrate diverse habitats, nutrient cycling, and biological productivity far out of proportion to their area. These floodplains serve as the primary meeting ground for aquatic, avian, and terrestrial species and act as corridors that allow both water-dwelling and land-dwelling creatures to move through otherwise rugged terrain.²⁰

The physical shape of the river channel matters immensely. When researchers compared floodplain segments of rivers with confined, canyon-like segments, the floodplains retained organic material up to four times more effectively and supported roughly 58% greater richness of aquatic invertebrates. The two types of river stretches hosted distinctly different invertebrate communities.²¹ A canyon and a floodplain can be only a few kilometers apart on the same river, but ecologically they function as different worlds. The landform, not just the water flowing through it, dictates what lives there.

Even in arid regions, landform-created water bodies harbor surprising life. Spain’s Monegros Desert contains shallow saline lakes sitting in topographic depressions. Despite their extreme salinity and harsh conditions, these lakes host highly novel microbial communities spanning all three domains of life, including archaea, bacteria, and eukaryotes with no close known relatives. Some of the lineages found there are so genetically distant from cultured organisms that they represent entirely new branches on the tree of life.²²

Caves, Volcanoes, and Extreme Landform Habitats

Some of the most striking examples of landform-driven life come from extreme environments. Karst landscapes, where soluble rock dissolves to form caves and underground river systems, harbor species found nowhere else. In a well-studied cave system in northern Alabama, researchers recently described a completely new genus of cave-obligate fish, deeply divergent from all previously known cavefish genera. This new species lives alongside a distantly related cavefish in the same underground system, meaning that two lineages independently evolved the suite of cave adaptations, including loss of vision, within a single groundwater network.²³ The cave itself shaped convergent evolution: different ancestors, same environment, same result.

Volcanic islands illustrate a different dynamic. When a fresh lava flow cools, it presents a blank slate for life. The sequence of colonization follows a predictable pattern governed by the physical properties of the new substrate. Early colonizers tend to be fast-growing plants with wind-dispersed seeds and traits geared toward rapid resource acquisition. As the substrate ages and weathers, the community shifts toward slower-growing species with animal-dispersed seeds and more conservative resource strategies, gradually modifying the environment and expanding the range of ecological niches available.²⁴ Without the landform-creating process of volcanism, these ecosystems would not exist at all.

Coastal Landforms and Storm Protection

Along coastlines, specific landforms serve as buffers between the ocean and inland ecosystems and communities. Tidal marshes and mangrove forests occupy the low-lying terrain at the land-sea interface, and they are increasingly recognized for their ability to reduce flooding and shoreline erosion during storms.²⁵ These are not just passive features of the landscape. Their root systems stabilize sediment, their vegetation attenuates wave energy, and the terrain they occupy acts as a sponge that absorbs storm surge. Where these landforms have been destroyed by development, coastal flooding tends to worsen considerably.

The ecological productivity of these coastal landforms is also enormous. Mangrove forests serve as nurseries for fish and crustaceans, tidal marshes filter pollutants from runoff before it reaches open water, and the sediment they trap builds new land over time. Lose the landform and you lose not just storm protection but a whole web of ecological services.

Landslides, Disturbance, and Renewal

It is tempting to think of landforms as static backdrops to the drama of life, but they are constantly changing, and the changes themselves matter ecologically. Landslides, one of the most visible ways mountains reshape themselves, have a complicated relationship with ecosystems. Their immediate effects are destructive: they strip vegetation, bury stream habitats, and destabilize slopes. But they also create fresh surfaces for colonization, open forest canopy to light, and generate habitat heterogeneity that supports species unable to survive in uniform, mature forests.²⁶ The feedback between biological processes and geomorphic disturbance drives mountain ecosystem dynamics at multiple scales. A forest on a landslide-prone slope is not the same forest as one on stable ground, and the difference creates ecological diversity that a perfectly stable landscape would lack.

Wind-driven dust transport offers another example. In southern Africa, seasonal Berg winds are funneled and intensified by topographic features like river valleys. These winds carry nutrient-rich dust offshore, supplying an estimated 4.4 tons annually into the South Atlantic and feeding the highly productive Benguela upwelling system.²⁷ The shape of the land determines how dust gets channeled, where it ends up, and which marine ecosystems benefit from the nutrient input. Even ocean productivity, in this case, traces back to the contours of the continent.

Why Landforms Mattered for Human Civilizations

Humans are not exempt from landform influence. The earliest complex societies clustered along river floodplains, from the Nile to Mesopotamia to the Indus, precisely because alluvial landforms concentrate the fertile soils and reliable water supplies that agriculture demands. Archaeological analysis of the Indus River Basin reveals that settlement patterns shifted over time depending on the positions of floodplains, levees, and paleochannels, with proto-historic settlements concentrated on levee features at the edge of floodplains rather than within them.²⁸ People were reading the landform, settling where the terrain offered the best combination of water access and flood protection.

Even large animal movements track terrain. Historical ecology of bison in the Western Cordillera shows that bison movement from the Great Plains into the mountains followed specific corridors dictated by wide passes, valley openings, and the presence of open grassland versus dense forest. South Pass, with its exceptionally wide corridor and open grass-shrub vegetation, allowed herds to penetrate over 1,000 kilometers into the mountains, while narrower, forested routes limited penetration to much shorter distances.²⁹ The landform acted as a filter, determining which animals, and by extension which human hunters, could reach interior mountain habitats.

Permafrost Landforms and Climate Feedback

Some landforms do not just respond to climate but actively feed back into it. Thermokarst lakes, which form in topographic depressions created by thawing permafrost, are a growing concern in high-altitude and high-latitude regions. As surface temperatures warm, ice-rich permafrost degrades, creating marshy hollows and ponds that release stored greenhouse gases including methane and carbon dioxide.³⁰ These are landforms that literally amplify warming: higher temperatures create more thermokarst, which releases more greenhouse gas, which raises temperatures further. In the Indian Himalaya, the formation of new thermokarst lakes is being tracked as both a symptom of warming and a contributor to it. The terrain is not a passive victim of climate change. It is an active participant in the feedback loop.