Afghanistan

Afghanistan is a landlocked country in south-central Asia, positioned where Central Asia, South Asia, and the Middle East meet. Mountains dominate its interior. The Hindu Kush range cuts across the country from northeast to southwest, separating fertile river valleys from arid plains and high plateaus. Afghanistan’s climate is continental and generally dry, shaped by elevation, distance from the sea, and the rain-shadow effect of its mountains.

This geographic position has never been incidental. Trade routes, migration paths, and empires have all passed through Afghanistan’s valleys and mountain passes for thousands of years, and the country’s physical geography still shapes where people live, how they farm, and how goods move today.

This article examines Afghanistan’s mountain systems and geological setting, its rivers and drainage basins, its climate and ecosystems, and the human geography built on top of these physical foundations — population distribution, cities, agriculture, mineral wealth, transportation, and the environmental hazards that make daily life there demanding. Current political and administrative developments are noted where relevant, using neutral, factual language that keeps geographic description separate from political judgment.

Geographical Location and Regional Setting

Afghanistan sits at the hinge between Central and South Asia. It shares borders with Pakistan to the south and east, Iran to the west, Turkmenistan, Uzbekistan, and Tajikistan to the north, and a narrow strip of territory — the Wakhan Corridor — that reaches northeast to touch China. No coastline interrupts this ring of neighbors. Afghanistan is one of the world’s larger landlocked countries, and that single fact explains a great deal about its trade patterns, its infrastructure challenges, and its historical reliance on overland routes rather than ports.

Physically, Afghanistan connects several major regions. The Hindu Kush and Pamir ranges rise in the northeast, the Iranian Plateau extends into the west, and the plains of Central Asia stretch north across the Amu Darya. This makes Afghanistan a transition zone rather than a self-contained geographic unit — a place where mountain climates give way to desert basins within relatively short distances.

The country’s landlocked position has pushed trade and travel through a small number of mountain passes and border crossings for centuries. Settlement has concentrated in valleys and basins where water is available, while vast stretches of highland and desert remain sparsely populated. This pattern of concentrated valleys surrounded by difficult terrain recurs throughout Afghan geography and helps explain the layout of its cities, farmland, and roads.

Area, Shape, and Geographic Extent

Afghanistan covers approximately 652,860 square kilometers, according to United Nations statistical references, making it roughly the size of Texas or slightly larger than France. Its shape is irregular, widest across the north-central region and narrowing sharply into the Wakhan Corridor, a finger of land barely 20 to 60 kilometers wide that stretches toward the Chinese border.

Most of this territory is mountainous. The Hindu Kush and its associated ranges occupy the northeast and center of the country, while lowland basins and plains sit at the margins — in the north along the Amu Darya, in the west around Herat, and in the southwest around the Helmand and Sistan basins. This produces sharp east-west and north-south contrasts: high, cold, and rugged terrain in the interior and northeast, flatter and drier terrain toward the borders.

Habitable land is unevenly distributed. Valleys carved by rivers such as the Kabul, Helmand, and Hari support most agriculture and settlement, while the surrounding highlands and deserts remain thinly populated. The Wakhan Corridor, despite its narrow width, carries real geopolitical and geographic significance as Afghanistan’s only direct link to China.

Major Mountain Systems and Landforms

Hindu Kush Mountains

The Hindu Kush is Afghanistan’s defining mountain system, stretching roughly 800 kilometers from the Pamir Knot in the northeast to lower ranges near Herat in the west. It is part of the same mountain-building process that produced the Himalayas, and its highest sections carry permanent snow and glaciers.

The tallest peak in the range, and in the country, is Noshaq, at 7,492 meters. Noshaq sits in the Wakhan Corridor near the Pakistani border and ranks among the highest peaks outside the Himalaya-Karakoram system. Below the highest ridgelines, mountain passes such as the Salang and Khyber (the latter just across the Pakistani border) have served as critical corridors for trade, migration, and military movement for centuries.

The Hindu Kush shapes far more than the skyline. Its snowpack feeds the rivers that irrigate Afghan farmland, its elevation creates sharp temperature differences between valley floors and mountain slopes, and its ruggedness has historically limited road-building, leaving many communities relatively isolated for parts of the year.

Other Mountain and Highland Regions

Beyond the Hindu Kush itself, several related ranges add to Afghanistan’s mountainous character. In the northeast, spurs of the Pamir Mountains extend into Afghan territory near the Wakhan Corridor. The Safed Koh (also called Spin Ghar) rises along the eastern border with Pakistan, near the Khyber Pass. Koh-e Baba extends west from the central Hindu Kush, forming the backbone of the central highlands, and the Paropamisus range runs through the northwest toward Herat.

These ranges differ meaningfully from one another. The northeastern mountains are the highest and most heavily glaciated. The central highlands, home to the Hazarajat region, are lower but still rugged, with a harsh climate and limited arable land. Southeastern ranges along the Pakistani border are drier and lower still, while the northern foothills taper down toward the plains bordering Central Asia.

Plains, Plateaus, and Basins

Lower-elevation landscapes ring the mountainous core. The northern plains, drained toward the Amu Darya, contain some of Afghanistan’s most productive farmland. The Kabul Basin, home to the capital, sits at roughly 1,800 meters elevation, surrounded by mountains on most sides. The Herat Basin in the west and the Helmand Basin in the southwest support extensive irrigated agriculture along their namesake rivers.

Further southwest, the terrain turns markedly drier. The Sistan Basin straddles the Afghan-Iranian border, the Registan Desert covers a large area of sand and gravel plains in the south, and the Dasht-e Margo (“Desert of Death”) occupies part of the southwest with almost no permanent water. These desert and semi-desert plateaus contrast sharply with the cooler, wetter conditions of the mountainous interior, underscoring how much elevation and moisture availability vary within a relatively compact national territory.

Geological and Tectonic Setting

Afghanistan’s mountains exist because of plate tectonics. The country sits within the broader Alpine-Himalayan mountain belt, a zone formed by the ongoing collision of the Indian Plate with the Eurasian Plate. This collision, which also built the Himalayas, continues to push up the Hindu Kush and surrounding ranges today.

This tectonic activity produces frequent fault movement and earthquakes, particularly in the northeast, where the Hindu Kush region experiences some of the deepest and most frequent earthquakes in the world. Northern and northeastern Afghanistan are especially vulnerable because they sit closest to the compressional stress created by the plate boundary. Afghanistan’s geology is correspondingly diverse, ranging from ancient crystalline rock in the mountains to younger sedimentary basins in the north and southwest, shaped over millions of years by uplift, folding, and erosion.

This same tectonic and geological complexity underlies much of Afghanistan’s known mineral wealth. Ore-bearing rock formations associated with mountain-building processes are found throughout the country, a point discussed further in the section on natural resources.

Rivers, Drainage Basins, and Water Resources

Water in Afghanistan comes overwhelmingly from mountain snow and ice, not rainfall. The Amu Darya forms much of the northern border and drains toward the Aral Sea basin in Central Asia. The Helmand River, Afghanistan’s longest, flows from the Hindu Kush southwest into the Sistan Basin. The Kabul River drains the eastern highlands and eventually joins the Indus system in Pakistan. Other significant rivers include the Hari River in the west, the Murghab and Kunduz rivers in the north, and the Arghandab and Farah rivers, which support agriculture in the south and southwest.

These rivers fall into distinct drainage basins: some flow north toward Central Asia, some feed into the Indus system through Pakistan, and others empty into closed interior basins with no outlet to the sea, such as the Sistan Basin. Snowmelt from the Hindu Kush dominates river flow in spring and early summer, supplemented by seasonal rainfall, groundwater, and natural springs. Reservoirs and irrigation canals extend this water supply into the growing season.

Water availability varies enormously by season and by region, and many Afghan rivers swell in spring and shrink dramatically by late summer. The Helmand Basin and the Kabul River system carry particular geographic importance, since both cross international borders — the Helmand into Iran and the Kabul into Pakistan — making water sharing a recurring feature of Afghanistan’s regional relationships.

Climate and Weather Patterns

Afghanistan’s climate is predominantly continental and dry, but elevation creates enormous local variation. Winters are cold across the highlands, with heavy snowfall common in the Hindu Kush and central mountains, while lowland areas such as the Sistan Basin and the Registan Desert experience hot, dry summers with very little precipitation.

Precipitation generally falls in winter and early spring, largely as mountain snow, with summers across most of the country remaining dry. The Hindu Kush blocks much of the moisture that would otherwise reach the interior, creating rain-shadow conditions in parts of the south and southwest. Temperature extremes are common: Kabul, at high elevation, experiences cold winters and mild summers, while lower desert basins can reach very high summer temperatures.

Regional differences are pronounced. Northern Afghanistan sees a mix of steppe and semiarid conditions, the central highlands are cold and snow-bound for much of the year, eastern valleys receive some monsoon-influenced summer rainfall, and the south and southwest remain hot and arid year-round. Mountain snowpack functions as Afghanistan’s primary water storage system, since it releases meltwater gradually through spring and summer, directly supporting both irrigation and household water supply across the growing season.

Natural Environment and Biodiversity

Elevation drives ecological variation across Afghanistan just as it drives climate variation. High alpine and subalpine zones in the Hindu Kush support sparse vegetation adapted to cold and thin air. Mountain forests, most notably in the eastern province of Nuristan, contain conifers and broadleaf species and represent some of Afghanistan’s few substantial woodlands. Lower elevations transition through steppe, shrubland, and grassland before reaching the deserts and semi-deserts of the south and southwest. River valleys and scattered wetlands provide additional habitat amid this generally dry landscape.

This range of environments supports a notable array of wildlife. The snow leopard inhabits the high Hindu Kush and Pamir-adjacent mountains. Marco Polo sheep, one of the largest wild sheep species, graze the Wakhan Corridor’s high pastures. Siberian ibex and markhor occupy rugged mountain slopes, while the Afghan pika survives in alpine rock fields. Lower elevations support goitered gazelle, wolves, and, in forested eastern regions, brown bears.

Afghanistan’s mountains also serve as a migration corridor connecting wildlife populations across Central and South Asia. Forests in Nuristan and other eastern areas face pressure from logging and land conversion, and broader environmental stress — discussed later in this article — continues to affect habitat quality and wildlife populations across the country.

Population and Demographic Geography

Afghanistan’s population is estimated at roughly 41 to 42 million as of 2023, according to United Nations Department of Economic and Social Affairs projections, though estimates vary because no full national census has been completed in decades. The population remains predominantly rural, with a substantial share of Afghans living in agricultural valleys and irrigated plains rather than cities, though urbanization has increased in recent decades.

Population density follows water availability closely. Fertile valleys such as the Kabul Basin, the northern plains near Mazar-i-Sharif, and irrigated areas around Herat and Kandahar hold much higher population densities than the surrounding mountains and deserts. Mountain settlement tends to cluster in narrow valley floors and terraced slopes, wherever a reliable water source and cultivable land coincide.

Afghanistan has a young population with a high proportion of children and youth relative to older adults, a pattern typical of countries with historically high birth rates. Migration has also shaped the country’s demographic geography substantially: decades of conflict have produced large refugee movements, both outward to neighboring Pakistan and Iran and, more recently, waves of return migration. Regional demographic patterns vary considerably, with population concentrations shifting alongside these migration flows and the ongoing pull of urban centers.

Major Cities and Urban Geography

Kabul, the capital, is by far Afghanistan’s largest city, with an estimated population in the range of 4 to 5 million within its metropolitan area. It sits in a mountain-ringed basin at roughly 1,800 meters elevation, a location that historically offered defensive advantages and access to trade routes but now creates real challenges for water supply and infrastructure as the city has grown far beyond its original footprint.

Kandahar, in the south, has long functioned as a major trade and agricultural hub linked to routes toward Pakistan. Herat, near the Iranian border, occupies a fertile valley along the Hari River and has historically served as a crossroads between Iran and Central Asia. Mazar-i-Sharif, in the north, connects to trade routes toward Uzbekistan and sits amid productive agricultural plains. Smaller but geographically significant cities include Jalalabad, positioned along the route toward the Khyber Pass and Pakistan; Kunduz, in the northern agricultural plains; Ghazni, along the historic road between Kabul and Kandahar; Bamyan, in the central highlands; Lashkar Gah, in the irrigated Helmand Valley; and Khost, near the eastern border with Pakistan.

Each of these cities developed at a point where a river valley, a trade corridor, or a mountain pass created a natural gathering place for people and goods. As Kabul and other cities have expanded rapidly, water supply, housing, and transportation infrastructure have come under increasing strain, a geographic challenge shared by many rapidly growing cities in mountainous, water-scarce regions.

Languages, Cultural Geography, and Human Landscapes

Dari and Pashto serve as Afghanistan’s two official languages and are spoken across much of the country, while Uzbek and Turkmen are common in the north, Balochi is spoken in parts of the south and southwest, and Nuristani and other regional languages persist in the mountainous east. This linguistic diversity did not emerge randomly. Afghanistan’s mountainous terrain has historically limited contact between valleys, allowing distinct languages and dialects to persist in relative isolation, while major river valleys and trade routes have simultaneously connected the country to Central Asia, Iran, and South Asia, bringing in additional linguistic and cultural influences over centuries.

Rural landscapes dominate much of the country: terraced hillsides, irrigated valley farms, and mudbrick village architecture reflect centuries of adaptation to a dry, mountainous environment. Nomadic and semi-nomadic pastoralism, historically practiced by groups moving livestock between highland summer pastures and lowland winter grazing areas, remains part of the rural economy in parts of the country, alongside settled agricultural communities. Historic urban centers such as Herat and Balkh preserve traditional architecture tied to their long roles as trade and cultural hubs along Central Asian routes.

Rather than reflecting a simple checklist of separate groups, this cultural and linguistic diversity reflects the underlying geography — a country of isolated valleys, connecting trade corridors, and centuries of migration across a mountainous crossroads.

Administrative and Political Geography

Afghanistan is divided into 34 provinces, each subdivided into districts that handle local administration. Kabul functions as the country’s primary administrative center, concentrating national government functions, though provincial capitals such as Kandahar, Herat, and Mazar-i-Sharif serve as regional administrative hubs for their surrounding provinces.

Since 2021, Afghanistan has been governed by the Taliban, which refers to itself as the Islamic Emirate of Afghanistan; this represents a change from the previous internationally recognized government structure. This description reflects the current administrative reality on the ground rather than any political endorsement, and readers should note that the international status of the governing authority differs among countries and organizations. Geographically, the provincial and district framework has remained the basic unit of local administration across this transition.

Historical Geography

Afghanistan’s territory has functioned as a corridor for trade, migration, and empire for millennia, and its historical geography traces closely with its physical geography. Early agricultural societies settled river valleys such as those around Balkh, taking advantage of irrigation potential. The region fell under Achaemenid Persian influence before Alexander the Great’s campaigns introduced Hellenistic and Greco-Bactrian influence, visible in archaeological sites across the north. The Kushan Empire later developed the region as a hub of Buddhist culture, with major religious and artistic centers, including the Bamyan Valley.

Islamic expansion from the seventh century onward reshaped the region’s religious and cultural geography, and cities such as Herat, Ghazni, and Balkh grew into major centers of trade and scholarship along medieval routes connecting Persia, Central Asia, and India. Mongol invasions in the 13th century disrupted many of these urban centers, though Herat later flourished again as a center of Timurid art and architecture in the 15th century.

The modern Afghan state traces its origins to the Durrani state formed in the 18th century, centered on Kandahar and later Kabul. Nineteenth-century geopolitics, including competition between the British and Russian empires, shaped Afghanistan’s borders and its role as a buffer state. Through the twentieth and twenty-first centuries, population growth, road-building, and periods of conflict have continued to reshape settlement patterns and infrastructure, but the underlying geographic logic — cities anchored in valleys, trade routes threading through mountain passes — has remained remarkably consistent across two thousand years.

Agriculture and Rural Landscapes

Agriculture depends almost entirely on irrigation drawn from Afghanistan’s rivers and groundwater, since rainfall alone is insufficient across most of the country. Wheat is the dominant staple crop, supplemented by rice, maize, and barley. Orchard and horticultural products — including grapes, pomegranates, almonds, and apricots — thrive in valleys around Kandahar and Herat and represent an important source of rural income. Cotton and vegetables are grown in irrigated lowland areas, while livestock raising and pastoralism remain central to the rural economy, particularly in highland and semi-arid regions unsuitable for cropping.

Major agricultural regions include the northern plains, the Kabul area, the Herat basin, the Kandahar region, and the Helmand Valley, where a large-scale irrigation system built in the mid-20th century expanded cultivable land substantially. Agricultural productivity across these regions depends heavily on consistent water availability, and recurring drought, groundwater depletion, and aging or damaged irrigation infrastructure all constrain output in different areas at different times. The geographic importance of the Helmand Valley irrigation system remains significant for the surrounding region’s agricultural output, though its current operational performance varies with water availability and infrastructure conditions.

Natural Resources and Mineral Geography

Afghanistan’s geology, shaped by the tectonic forces described earlier, has produced a substantial range of known mineral deposits. These include copper, iron ore, lithium, rare earth elements, gold, and various gemstones, alongside marble, coal, natural gas, and petroleum. Some of the most extensively studied deposits include the Aynak copper deposit southeast of Kabul and iron ore reserves at Hajigak in the central highlands, both identified through geological surveys conducted over recent decades.

It is important to distinguish between different categories of resource information. Known geological formations and estimated deposits, identified through surveys by organizations including the United States Geological Survey, represent potential resources rather than proven, commercially extracted reserves. Many of Afghanistan’s mineral deposits remain unexplored in detail or undeveloped due to a combination of infrastructure limitations, security conditions, and lack of investment, meaning current production levels remain far below the country’s estimated geological potential.

Economy and Economic Geography

Afghanistan’s economy remains heavily tied to its geography. Agriculture, including crop farming and livestock raising, provides livelihoods for a large share of the population, particularly in irrigated valleys and northern plains. Mining, construction, small-scale manufacturing, trade, and services make up much of the remaining formal economic activity, alongside a substantial informal sector. Remittances from Afghans working abroad also represent an important income source for many households.

Landlocked status shapes economic geography directly, since all trade must cross neighboring countries, adding cost and complexity to imports and exports. Kabul, as the administrative and commercial center, differs economically from northern agricultural regions oriented toward trade with Central Asia, from western Afghanistan’s connections to Iran, from southern agricultural zones centered on Kandahar and Helmand, and from eastern border regions tied economically to Pakistan through the Khyber Pass corridor. According to World Bank estimates, Afghanistan’s economy has faced significant contraction since 2021, though precise current statistics vary among sources and should be treated as estimates tied to their specific reference year.

Transportation and Regional Connectivity

Afghanistan’s mountainous terrain and landlocked position make transportation a persistent geographic challenge. Highways connect major cities, but many routes cross high mountain passes that are vulnerable to snow closure in winter. The Salang Pass, cut through the Hindu Kush north of Kabul, remains one of the most important — and most difficult — routes in the country, connecting the capital to northern Afghanistan. The Ring Road, built in stages since the mid-20th century, links Kabul, Kandahar, Herat, and Mazar-i-Sharif in a loop intended to connect the country’s major population centers, though sections have suffered damage and disrepair over decades of conflict.

Border crossings connect Afghanistan to its neighbors: routes through the Khyber Pass and Torkham link to Pakistan, crossings near Herat connect to Iran, and northern crossings connect to Turkmenistan, Uzbekistan, and Tajikistan. Kabul’s international airport provides the country’s primary air link, supplemented by smaller regional airports. The Wakhan Corridor, though narrow and difficult to traverse, gives Afghanistan its only direct geographic connection to China, underscoring the country’s position as a hinge between Central and South Asian transportation networks.

Energy Geography

Afghanistan’s energy supply draws on a mix of hydropower, natural gas, coal, and imported electricity, supplemented by growing but still limited solar and wind capacity. The country’s mountainous terrain and substantial river flow give it meaningful hydropower potential, particularly along the Kabul and Helmand river systems, though much of this potential remains undeveloped.

Electricity access varies sharply between urban and rural areas, with many rural communities relying on limited local generation or remaining unconnected to any grid. Afghanistan has historically imported a significant share of its electricity from neighboring Uzbekistan, Tajikistan, and Turkmenistan, reflecting the gap between domestic generation capacity and demand. Seasonal water availability also affects hydropower output, since generation tied to river flow fluctuates between the high-water spring and summer months and the drier conditions of winter.

Tourism and Geographical Heritage

Afghanistan contains a range of landscapes and historical sites of significant geographical and cultural interest, even though conditions have limited tourism activity in recent decades. The Bamyan Valley, once home to monumental Buddhist statues carved into cliffside niches, remains an important cultural landscape in the central highlands. Nearby, Band-e Amir’s chain of deep blue lakes, formed by natural mineral dams, represents a distinctive geological feature and was designated Afghanistan’s first national park.

The Wakhan Corridor offers dramatic high-mountain scenery and some of the country’s most intact wildlife habitat. Herat and Balkh preserve historic architecture tied to their roles as Silk Road cities, while Kandahar and Kabul retain sites reflecting successive periods of Afghan political history. The Panjshir Valley, cut into the Hindu Kush north of Kabul, and the forested landscapes of Nuristan further illustrate the ecological and topographic range packed into a relatively compact national territory.

Natural Hazards and Environmental Challenges

Afghanistan faces a substantial range of natural hazards tied directly to its geology, terrain, and climate. Earthquakes pose a serious and recurring risk, particularly in the northeast, where the collision of the Indian and Eurasian plates generates frequent seismic activity. Drought recurs periodically across much of the country, straining both agriculture and drinking water supplies. Flooding, often triggered by rapid spring snowmelt or intense seasonal rainfall, affects river valleys and low-lying settlements. Steep terrain makes landslides and avalanches a persistent danger in mountainous regions, particularly during winter and early spring.

Extreme temperatures, dust storms, and desertification add further pressure, particularly in the arid south and southwest. These hazards stem from natural geological and climatic conditions, but their human impact depends heavily on factors such as building construction quality, early warning systems, and infrastructure — meaning the underlying natural hazard and the resulting human vulnerability, while related, are not the same thing.

Water Stress, Land Degradation, and Climate Change

Water scarcity ranks among Afghanistan’s most pressing long-term environmental challenges. Recurring drought, combined with groundwater depletion in areas of heavy agricultural pumping, has placed growing strain on irrigation systems already limited by aging infrastructure. Soil degradation and desertification affect parts of the south and southwest, while deforestation in areas such as Nuristan has contributed to habitat loss and declining biodiversity. Wetlands, always limited in extent, face additional pressure from both water diversion and drought.

Scientific assessments indicate that the wider Hindu Kush-Himalaya region has experienced measurable glacier and snowpack decline in recent decades, a trend documented by research institutions monitoring the broader mountain system. Projections suggest that continued warming could further reduce snowpack and glacier volume, altering the timing and volume of river flow that Afghan agriculture depends on. These are projections rather than certainties, and their precise local impact on Afghanistan’s specific river basins continues to be studied, but the general direction — reduced and less predictable water availability — is consistent with observed regional trends.

Afghanistan’s Regional Geographic Importance

Afghanistan’s location at the intersection of Central Asia, South Asia, and Southwest Asia gives it geographic significance well beyond its size. Its mountains feed river systems that cross into neighboring countries, making it relevant to regional water management in Central Asia, Iran, and Pakistan alike. Its historic trade routes, threading through the Khyber Pass, the Wakhan Corridor, and the plains bordering Central Asia, continue to shape regional connectivity and the potential for future transportation and energy corridors linking South and Central Asia.

The country’s biodiversity, concentrated in the Hindu Kush and Wakhan Corridor, connects wildlife populations across a wide swath of high-mountain Asia, while its patterns of migration and cross-border movement remain closely tied to conditions in neighboring countries. Viewed geographically rather than politically, Afghanistan functions as a hinge — a place where mountain systems, river basins, and transportation corridors from several major world regions converge.

Key Geographic Facts

Geographic Fact	Information
Official name	Islamic Emirate of Afghanistan (current de facto administration)
Region	South-Central Asia
Capital	Kabul
Total area	Approximately 652,860 square kilometers
Landlocked status	Landlocked; no coastline
Geographic coordinates	Approximately 33°00’N, 65°00’E
Highest point	Noshaq (7,492 meters)
Major mountain system	Hindu Kush
Major rivers	Amu Darya, Helmand, Kabul, Hari, Murghab, Kunduz, Arghandab, Farah
Major drainage basins	Amu Darya (Central Asian) basin, Helmand/Sistan interior basin, Kabul River (Indus) basin
Climate	Arid to semiarid continental, with cold mountain climates in highland areas
Major natural hazards	Earthquakes, drought, flooding, landslides, avalanches, dust storms
Population	Approximately 41–42 million (UN DESA estimate, 2023)
Largest urban center	Kabul
Major cities	Kabul, Kandahar, Herat, Mazar-i-Sharif, Jalalabad, Kunduz, Ghazni, Bamyan, Lashkar Gah, Khost
Major languages	Dari, Pashto (official); Uzbek, Turkmen, Balochi, Nuristani, and other regional languages
Major agricultural products	Wheat, rice, maize, barley, grapes, pomegranates, almonds, apricots, cotton
Major mineral resources	Copper, iron ore, lithium, rare earth elements, gold, gemstones, marble, coal, natural gas
Major energy sources	Hydropower, natural gas, coal, imported electricity, limited solar and wind
Major transportation corridors	Salang Pass, Ring Road, Khyber Pass route, Wakhan Corridor
Currency	Afghani (AFN)
Administrative divisions	34 provinces, subdivided into districts