Table Mountain: Elevation, Geology, Hiking & Fast Facts

Table Mountain (Huri ‡oaxa, Tafelberg)

Rising directly behind Cape Town on South Africa’s southwestern coast, Table Mountain is one of the most recognizable mountains in the world. Its immense flat-topped plateau, sheer sandstone cliffs, swirling “tablecloth” cloud, extraordinary fynbos vegetation, and dramatic position between city and ocean have made it a symbol not only of Cape Town but of South Africa itself.

The mountain’s highest point, Maclear’s Beacon, reaches approximately 1,085 meters (3,560 feet) above sea level. While modest compared with Africa’s great high mountains, Table Mountain has an impressive 1,068 meters (3,504 feet) of topographic prominence and more than 42 kilometers of isolation. It rises almost directly from the coast, producing a far greater visual impact than its elevation alone might suggest.

Table Mountain is also extraordinarily old. Its upper cliffs consist largely of resistant quartz-rich sandstone of the Table Mountain Group, deposited more than 500 million years ago. Beneath these layers lie even older Malmesbury rocks and Cape Granite. Erosion over hundreds of millions of years gradually removed softer surrounding material while leaving the resistant sandstone plateau standing above Cape Town.

The mountain is equally important biologically. It forms the heart of Table Mountain National Park and part of the Cape Floral Region Protected Areas UNESCO World Heritage Site. More than 2,000 plant species occur within the national park, many found nowhere else on Earth. Proteas, ericas, restios, geophytes, silver trees, rare orchids, and highly localized endemic species make the mountain one of the most botanically important urban natural areas on the planet.

Humans have interacted with the mountain for tens of thousands of years. SANParks records archaeological evidence of human activity in the region dating back approximately 30,000 years. Indigenous people knew the mountain long before European ships entered Table Bay, and Khoekhoe traditions preserved names including Hoerikwaggo, commonly interpreted as “Mountain in the Sea.”

Portuguese navigator António de Saldanha made the first recorded European ascent in 1503, probably using Platteklip Gorge. Today that same steep gorge remains the mountain’s most direct and popular hiking route.

Visitors can also reach the summit using the famous Table Mountain Aerial Cableway, operating since 1929. From the upper station, trails lead across the plateau toward Maclear’s Beacon, viewpoints over Cape Town, and longer routes connecting the mountain with Kirstenbosch, the Twelve Apostles, Devil’s Peak, and the Back Table.

⚡ Fast Facts

Fact	Details
Mountain	Table Mountain
Indigenous Name	Hoerikwaggo / Huriǂoaxa variants
Afrikaans Name	Tafelberg
Continent	Africa
Country	South Africa
Province	Western Cape
City	Cape Town
Mountain System	Cape Peninsula / Cape Fold Belt
Protected Area	Table Mountain National Park
Highest Point	Maclear’s Beacon
Elevation	Approximately 1,085 m / 3,560 ft
Prominence	Approximately 1,068 m / 3,504 ft
Isolation	Approximately 42.58 km / 26.46 mi
Nearest Higher Neighbor (NHN)	Helderberg Dome
Coordinates	Approximately 33.962° S, 18.425° E
Principal Rock	Peninsula Formation quartzitic sandstone
Major Lower Rocks	Malmesbury Group and Cape Granite
Volcano?	No
First Recorded European Ascent	1503
First Recorded European Ascender	António de Saldanha
Indigenous Use	Long predates European records
Easiest Major Route	Platteklip Gorge
Cableway Opening	October 4, 1929
National Park	Table Mountain National Park
UNESCO Status	Cape Floral Region Protected Areas
Signature Vegetation	Fynbos
Famous Weather Feature	Tablecloth cloud

📍 Where Is Table Mountain?

Table Mountain rises immediately south of central Cape Town in South Africa’s Western Cape Province.

The mountain occupies the northern portion of the Cape Peninsula, a narrow mountainous landmass extending southward between the Atlantic Ocean and False Bay.

Cape Town’s City Bowl lies directly beneath the mountain’s northern face.

Several famous neighboring landmarks define the surrounding skyline:

• Devil’s Peak to the east
• Lion’s Head to the northwest
• Signal Hill beyond Lion’s Head
• Twelve Apostles extending south along the Atlantic side
• Kirstenbosch National Botanical Garden on the eastern slopes
• Camps Bay beneath the western cliffs

Few major cities are so closely connected with a mountain.

Table Mountain is not simply visible from Cape Town.

It determines the city’s geography.

Roads, suburbs, weather patterns, neighborhoods, viewpoints, water systems, tourism, and even the shape of the urban landscape have developed around it.

🏔️ Why Is Table Mountain Flat?

The mountain’s defining feature is its broad, nearly level summit.

From Table Bay, the plateau appears almost like a giant tabletop approximately three kilometers wide.

This flat appearance developed through a combination of geology and erosion.

The upper mountain consists largely of exceptionally resistant sandstone.

Softer surrounding rocks weathered and eroded much more rapidly.

Over enormous spans of geological time, rivers, wind, rainfall, chemical weathering, and rockfall gradually stripped away surrounding material.

The resistant sandstone remained.

The result is not a perfectly horizontal slab but a broad plateau with cliffs around much of its edge.

📏 How High Is Table Mountain?

The highest natural point of Table Mountain lies near Maclear’s Beacon at approximately:

1,085 meters / 3,560 feet

Different sources give slightly different figures, commonly ranging from about 1,084.6 to 1,086 meters.

The difference reflects rounding and surveying conventions.

The upper cableway station is lower than the true summit.

This is important because many visitors ride the cableway, step onto the plateau, and assume they have reached Table Mountain’s highest point.

They have reached the top of the main tourist area—but not Maclear’s Beacon.

🗿 Maclear’s Beacon

Maclear’s Beacon marks Table Mountain’s true high point.

The stone beacon was constructed in 1844 as part of astronomical and geodetic surveying.

It was associated with Thomas Maclear, Astronomer Royal at the Cape.

Maclear was working to improve earlier measurements of the curvature of Earth made by French astronomer Nicolas-Louis de Lacaille.

His assistant William Mann built the beacon from stone.

The structure became an important triangulation point.

Today, hikers can reach Maclear’s Beacon by walking across the plateau from the upper cableway area or by climbing routes such as Skeleton Gorge and continuing across the Back Table.

📐 Topographic Prominence

Table Mountain has approximately:

1,068 meters / 3,504 feet

of topographic prominence.

That means the mountain rises more than one vertical kilometer above the highest saddle connecting it to higher terrain elsewhere.

For a mountain only 1,085 meters tall, that is enormous.

Nearly all of Table Mountain’s elevation counts toward its independent rise.

This explains why the mountain appears so dominant despite being comparatively low by global mountain standards.

Its steep northern and western faces rise very close to sea level.

🌏 Isolation

Table Mountain has approximately:

42.58 kilometers / 26.46 miles

of topographic isolation.

Higher terrain does not occur until the mountains east of Cape Town.

Modern topographic datasets identify higher ground around the Helderberg Dome region as the nearest terrain exceeding Table Mountain’s elevation.

This isolation helps make Table Mountain the dominant summit of the northern Cape Peninsula.

🧭 Nearest Higher Neighbor: Helderberg Dome

Table Mountain’s Nearest Higher Neighbor (NHN) is generally identified as Helderberg Dome, east of Cape Town.

Helderberg Dome rises to approximately 1,137 meters.

The higher terrain lies roughly 42.6 kilometers away.

This is a substantial distance for a mountain so close to a large urban center.

Although Devil’s Peak stands immediately beside Table Mountain, it reaches only about 1,001 meters and is therefore lower.

🪨 Geology of Table Mountain

Table Mountain contains an extraordinary geological record spanning more than half a billion years.

SANParks divides the principal rocks of the Cape Peninsula into three major groups:

1. Malmesbury Group
2. Cape Granite
3. Table Mountain Group

Each represents a different stage in the geological development of the region.

These rocks were formed long before anything resembling modern Cape Town—or even modern Africa—existed.

🪨 Malmesbury Group

The oldest widely exposed rocks around Table Mountain belong to the Malmesbury Group.

SANParks dates them to approximately 540 million years ago.

They include:

• Mudstone
• Shale
• Sandstone
• Metamorphosed sedimentary rocks

These sediments accumulated in ancient marine environments.

Later tectonic activity folded and altered them.

Malmesbury rocks occur on parts of:

• Signal Hill
• Devil’s Peak
• Lower mountain slopes

Because they generally weather more readily than the overlying sandstone, they form smoother and lower terrain.

🪨 Cape Granite

Approximately 540 million years ago, magma intruded into the Malmesbury rocks.

The magma cooled underground to form Cape Granite.

Granite contains minerals including:

• Feldspar
• Quartz
• Mica

Large granite outcrops occur throughout the Cape Peninsula.

They are particularly visible around locations such as:

• Lion’s Head
• Boulders
• Chapman’s Peak region
• Cape coastline

Granite forms part of the foundation beneath Table Mountain itself.

🪨 Table Mountain Group

Above these older rocks lies the Table Mountain Group, deposited approximately 520 million years ago.

SANParks divides it into several formations.

Graafwater Formation

The Graafwater Formation consists of reddish and purplish sandstone and mudstone.

It is generally around 25–65 meters thick.

Peninsula Formation

The Peninsula Formation forms the massive pale cliffs that define Table Mountain.

It consists largely of quartz-rich sandstone.

This formation can reach around 700 meters thick.

Pakhuis Formation

The Pakhuis Formation includes material deposited during ancient glaciation.

It contains pebbles transported by ice hundreds of millions of years ago.

Together, these layers preserve evidence of rivers, coastlines, changing climates, ancient continental ice, and tectonic movement.

🪨 Table Mountain Sandstone

The traditional term Table Mountain Sandstone is still widely used informally.

Modern geologists generally use more specific stratigraphic names such as Peninsula Formation.

The sandstone contains extremely high concentrations of quartz.

Quartz resists chemical weathering.

This durability explains why the upper mountain has survived while much surrounding terrain has been eroded away.

Its pale color also gives the cliffs their characteristic appearance.

🌋 Is Table Mountain a Volcano?

No.

Table Mountain is not volcanic.

This misconception occasionally arises because of its dramatic shape and isolated appearance.

The mountain is primarily an erosional remnant built from sedimentary rock.

No volcanic cone, lava chamber, or crater created its flat summit.

Its modern form resulted from:

• Ancient sedimentation
• Tectonic deformation
• Regional uplift
• Differential erosion
• Weathering
• Rockfall

The mountain is therefore fundamentally different from volcanic African peaks such as Kilimanjaro or Mount Cameroon.

🌍 The Cape Fold Belt

Table Mountain lies near the western end of the Cape Fold Belt.

The Cape Fold Belt formed during a major period of mountain building hundreds of millions of years ago as tectonic forces compressed sedimentary layers along the southern margin of Gondwana.

Many Cape Fold mountains farther east display dramatic folded rock layers.

Around Cape Town, the structure is somewhat different, but the Table Mountain Group forms part of the same broad geological province.

This ancient tectonic history helps explain why resistant sandstone extends far beyond the mountain itself into ranges across the Western Cape.

🧊 Ancient Glaciation

Evidence of ancient glaciation is preserved within the Table Mountain Group.

The Pakhuis Formation contains sediments associated with glacial conditions more than 400 million years ago.

At that time, the continents occupied dramatically different positions.

Southern Africa was part of Gondwana and lay much closer to the South Pole.

Ice transported and deposited rock fragments across the landscape.

These ancient glacial deposits should not be confused with recent alpine glaciers.

Table Mountain itself has no modern glacier and did not develop its flat top through recent Ice Age glaciation.

🌊 A Mountain Beside the Ocean

One of Table Mountain’s most spectacular characteristics is its immediate proximity to the sea.

The mountain rises only a few kilometers from both:

• Table Bay
• Atlantic Ocean

Its summit sits more than one kilometer above sea level.

This produces dramatic relief.

From ships approaching Cape Town, Table Mountain historically appeared as a huge natural landmark rising behind the bay.

Its shape became one of the most important navigation markers on southern Africa’s Atlantic coast.

🌬️ Climate

Table Mountain experiences a Mediterranean-type climate.

Most rainfall occurs during the cooler winter months.

Summers are generally warmer and drier.

However, conditions on the mountain differ substantially from those in Cape Town below.

Elevation and exposure create:

• Lower temperatures
• Stronger winds
• More frequent cloud
• Higher rainfall on some slopes
• Sudden weather changes

The wetter eastern and southern slopes support pockets of forest and rich vegetation.

The exposed northern and western faces are generally drier.

☁️ The Tablecloth Cloud

Table Mountain’s most famous weather phenomenon is the tablecloth.

During suitable conditions, cloud forms over the summit and spills across the plateau edge.

The process typically occurs when moist air is forced upward against the mountain.

As the air rises, it cools.

Moisture condenses into cloud.

As the air descends again, it warms and the cloud evaporates.

The result can look like a white cloth flowing continuously over the mountain.

🌫️ Why the Tablecloth Matters

The tablecloth is more than a beautiful weather effect.

SANParks notes that cloud and fog can provide important moisture to vegetation on the upper plateau.

Fog droplets collect on plant surfaces.

The water then reaches soil and wetlands.

This additional moisture supports specialized vegetation on the summit, including species adapted to wetter high-altitude conditions.

The cloud therefore influences both appearance and ecology.

🚬 Van Hunks and the Devil

Cape Town folklore offers a more colorful explanation for the tablecloth.

According to the famous story, pipe smoker Jan van Hunks challenged the Devil to a smoking contest on the mountain.

The two smoked so vigorously that huge clouds formed across Table Mountain.

Their contest supposedly continues whenever the tablecloth appears.

The story is folklore rather than meteorology, but it remains one of Cape Town’s best-known mountain legends.

🧑‍🤝‍🧑 Human History Before European Arrival

Table Mountain has a human history extending far beyond colonial Cape Town.

SANParks reports archaeological evidence of human presence in the region dating back approximately 30,000 years.

Stone Age communities used the broader Cape Peninsula for:

• Hunting
• Gathering
• Water
• Shelter
• Movement
• Seasonal resources

Khoekhoe communities later grazed livestock and moved throughout the region.

Oral history indicates that Indigenous people used routes such as Platteklip Gorge before Europeans ever attempted to climb the mountain.

🏷️ Hoerikwaggo

One important Indigenous name associated with Table Mountain is Hoerikwaggo.

SANParks translates the name approximately as:

“Mountain in the Sea.”

Other Khoekhoe spelling variants appear in historical and modern sources.

The name reflects the extraordinary appearance of the mountain when viewed from the surrounding coastline and ocean.

Long before Europeans called it Table Mountain, the mountain already occupied an important place within Indigenous geography.

⛵ António de Saldanha

The first recorded European ascent occurred in 1503.

Portuguese navigator António de Saldanha entered Table Bay while sailing along the African coast.

He reportedly climbed the mountain to obtain a better view of the region.

The ascent is traditionally associated with Platteklip Gorge.

Saldanha’s climb became one of the earliest recorded European mountain ascents in southern Africa.

However, calling him simply the “first person to climb Table Mountain” would be inaccurate because Indigenous people had already used the landscape.

The better wording is:

First recorded European ascent: António de Saldanha, 1503.

🥾 Platteklip Gorge: The Historic Route

Platteklip Gorge remains the most famous hiking route to Table Mountain’s summit.

It climbs directly through the huge cleft visible on the mountain’s northern face.

SANParks calls it the “highway to the top.”

The trail begins along Tafelberg Road.

From there, it climbs steeply through the gorge to the plateau.

The route is approximately:

3 kilometers one way

Although technically straightforward, it involves substantial elevation gain.

The climb is relentless.

🥾 Is Platteklip Gorge Easy?

Platteklip is often described as the easiest route.

That can be misleading.

It is the most straightforward route because it involves:

• No serious scrambling
• A clear path
• Stone steps
• No complicated route finding under normal conditions

But it is also very steep.

SANParks rates it from moderate to tough depending on fitness and conditions.

Summer heat can be intense.

Winter weather may be cold and wet.

The upper gorge can also become extremely windy.

🥾 Skeleton Gorge

Skeleton Gorge climbs the mountain from the Kirstenbosch side.

It begins within forest and offers a completely different experience from Platteklip.

The route climbs through Afromontane forest.

Steps, ladders, rocks, roots, and wet surfaces make it more varied.

Higher up, the route emerges onto the Back Table.

Hikers can continue across the plateau toward:

• Maclear’s Beacon
• Hely-Hutchinson Reservoir
• Upper Cableway area

SANParks notes that the route can be slippery even during summer.

🌳 Skeleton Gorge and Forest

The lower section of Skeleton Gorge passes through one of Table Mountain’s most beautiful surviving forest environments.

Dense vegetation provides shade.

Mosses, ferns, trees, streams, and wet rock create a cool atmosphere unlike the exposed northern face.

This habitat is also important for one of Table Mountain’s rarest animals:

the Table Mountain ghost frog.

🥾 India Venster

India Venster begins near the lower cableway area and climbs the mountain’s front side.

It is much more serious than Platteklip Gorge.

The route includes:

• Scrambling
• Exposure
• Rock steps
• Route-finding challenges

It should not be treated as a beginner trail simply because it begins near tourist infrastructure.

Inexperienced hikers are better served by Platteklip Gorge or by using a qualified local guide.

Wet weather, wind, and poor visibility can make India Venster significantly more hazardous.

🥾 Kasteelspoort

Kasteelspoort climbs from the Camps Bay side of the mountain.

The route ascends toward the Back Table and Twelve Apostles region.

It offers extensive views over:

• Camps Bay
• Atlantic Ocean
• Lion’s Head
• Western suburbs
• Twelve Apostles

Kasteelspoort is especially popular with hikers seeking a longer and less direct experience than Platteklip.

The route also passes close to remnants of historic cableway infrastructure associated with earlier development on the mountain.

🥾 Smuts Track

The Smuts Track connects Skeleton Gorge with Maclear’s Beacon.

It is one of the classic longer summit walks.

The route crosses upland terrain containing:

• Wetlands
• Fynbos
• Rocky sandstone
• Reservoir landscapes

SANParks specifically warns that hikers should avoid attempting the route to Maclear’s Beacon when heavy mist covers the mountain.

The plateau can become confusing in low visibility.

🚠 Table Mountain Aerial Cableway

The Table Mountain Aerial Cableway has transformed access to the mountain.

It officially opened on:

October 4, 1929

The original cable car carried only 19 passengers plus a conductor.

The journey took close to ten minutes.

Modern rotating cable cars can transport far more people while providing 360-degree views during the ascent.

By late 2025, the cableway had carried more than 33 million visitors since opening.

🚠 Cableway Upgrades

The cableway has undergone several major upgrades.

Important dates include:

• 1929 — original opening
• 1958 — larger cable cars
• 1974 — major modernization
• 1997 — introduction of modern Rotair cars

The rotating floor allows passengers to experience views in every direction.

The trip from lower station to upper station takes only a few minutes.

For many visitors, this provides their first experience of standing more than 1,000 meters above Cape Town.

⚠️ The Cableway Can Close

Cableway access should never be treated as guaranteed.

Strong wind, poor visibility, maintenance, or technical conditions may cause operations to stop.

SANParks specifically warns hikers climbing Platteklip Gorge not to assume they will be able to ride down.

If the cableway closes unexpectedly, hikers may need to descend on foot.

Anyone hiking up should therefore carry enough:

• Water
• Food
• Warm clothing
• Daylight
• Energy

for a full hiking descent if necessary.

🌿 Flora and Fauna

Table Mountain is one of the most botanically extraordinary mountains on Earth.

Table Mountain National Park contains more than 2,000 plant species.

Many have extremely small ranges.

Some occur only within a few square kilometers.

The mountain belongs to the Cape Floristic Region, the smallest of the world’s major floral kingdoms but one of the richest relative to its area.

🌿 Fynbos

The dominant vegetation is fynbos.

SANParks identifies four major plant groups that characterize fynbos:

• Proteas
• Ericas
• Restios
• Geophytes

Fynbos generally occurs on nutrient-poor soils.

Its diversity is extraordinary.

Individual valleys and slopes may contain plants absent from nearby mountains only a short distance away.

This intense local endemism makes Table Mountain globally important for conservation.

🌺 Proteas

Proteas are among the most recognizable fynbos plants.

The wider Cape Peninsula supports numerous Proteaceae species.

Their flowers are adapted to pollination by combinations of:

• Birds
• Insects
• Small mammals

Many proteas store seeds in woody flower heads.

Fire can trigger seed release and create conditions favorable for germination.

The mountain’s vegetation therefore cannot be understood without understanding fire.

🌸 Ericas

The Cape Floral Region contains an extraordinary diversity of Erica, or heath species.

Many occupy extremely limited ranges.

Some grow only on particular soil types, elevations, or slopes.

This specialization makes them highly vulnerable.

A poorly timed fire, invasive plant, trail disturbance, or climatic shift can threaten an entire species if its entire distribution covers only a few hectares.

🌾 Restios

Restios are reed-like plants characteristic of fynbos.

They occupy habitats ranging from dry slopes to moist summit wetlands.

Their appearance sometimes resembles grasses, but they belong to a different botanical group.

SANParks notes that restios occur across all major fynbos habitats.

They form an essential structural component of Table Mountain vegetation.

🌷 Geophytes

Geophytes include plants that survive difficult seasons through underground storage structures such as:

• Bulbs
• Corms
• Tubers

Famous examples include:

• Watsonias
• Disas
• Irises
• Numerous smaller flowering plants

Many produce spectacular blooms after fire.

The underground storage organs protect plants from heat and allow rapid regrowth when favorable conditions return.

🔥 Fire Ecology

Fire is essential to fynbos.

SANParks explains that healthy fynbos typically requires periodic burning.

Fire helps:

• Remove old vegetation
• Release nutrients
• Trigger seed germination
• Open habitat
• Stimulate flowering

But timing matters.

Fire that occurs too frequently can destroy immature plants before they produce seed.

Fire that is suppressed for too long can also alter ecosystem structure.

Managing fire is especially difficult because Table Mountain directly borders densely populated urban areas.

🌳 Afromontane Forest

Table Mountain also contains pockets of Afromontane forest.

These forests occur mainly in wetter ravines and sheltered slopes.

Important examples include:

• Skeleton Gorge
• Newlands
• Orange Kloof

The forest differs dramatically from open fynbos.

Tall evergreen trees create dense shade.

Mosses, algae, ferns, and other moisture-loving organisms thrive beneath the canopy.

Much larger areas of indigenous forest were historically harvested after European settlement.

Today, the remaining pockets are ecologically important.

🐸 Table Mountain Ghost Frog

One of Table Mountain’s rarest animals is the Table Mountain ghost frog.

The species is found nowhere else on Earth.

SANBI describes its entire natural range as only approximately 7–8 square kilometers.

It inhabits cold, fast-flowing perennial streams on the mountain’s eastern and southern slopes.

Adaptations include:

• Webbed feet
• Sucker-like toe pads
• Streamlined tadpoles
• Sucker-like tadpole mouthparts

These allow the frogs to cling to wet rock in rapidly flowing water.

The species is classified as Critically Endangered.

🐸 Why the Ghost Frog Is Vulnerable

Its tiny distribution makes the species exceptionally vulnerable.

Potential threats include:

• Water abstraction
• Erosion
• Invasive plants
• Stream modification
• Heavy recreational use
• Climate change

Even though its habitat lies largely within protected land, protection alone cannot eliminate every threat.

The ghost frog demonstrates how conservation on Table Mountain can have global significance.

If this species disappears here, it disappears everywhere.

🐾 Dassies

One of the animals visitors are most likely to encounter near developed summit areas is the rock hyrax, commonly called a dassie.

Dassies resemble large rodents.

Surprisingly, their evolutionary relatives include elephants and manatees.

They live among rocks and cliffs.

They often bask in sunlight.

Visitors should not feed them.

Feeding wildlife changes natural behavior and can create dependence or conflict.

🐈 Caracal

Caracals survive throughout portions of Table Mountain National Park.

These secretive wild cats are rarely seen by daytime visitors.

They hunt animals including:

• Rodents
• Birds
• Small mammals

Caracals have adapted surprisingly well to the fragmented urban landscape surrounding the park.

Research around Cape Town has shown that they move between mountain habitats despite roads, suburbs, recreation, and other human pressures.

🦌 Small Antelope

The national park supports several small antelope species.

These include:

• Klipspringer
• Cape grysbok
• Common duiker
• Grey rhebok
• Steenbok

Many are most active early or late in the day.

Their smaller body size suits fynbos vegetation and rocky terrain.

Klipspringers are particularly adapted to cliffs and boulder fields.

SANParks has undertaken reintroduction efforts for species that disappeared locally in the past.

🦔 Cape Porcupines

Cape porcupines also occur within the park.

These large nocturnal rodents feed primarily on plant material.

They dig for:

• Roots
• Bulbs
• Tubers

Their large black-and-white quills provide an effective defense against predators.

Most visitors never see them because they are active mainly after dark.

🐦 Birds

Table Mountain National Park has recorded approximately 250 bird species.

Habitats range from:

• Fynbos
• Forest
• Cliffs
• Wetlands
• Urban edge
• Coastline
• Marine environment

Characteristic fynbos species include:

• Cape sugarbird
• Orange-breasted sunbird
• Malachite sunbird
• Lesser double-collared sunbird
• Karoo prinia
• Grey-backed cisticola

Many play important roles in pollination.

🐦 Cape Sugarbirds

The Cape sugarbird is closely associated with flowering proteas.

Its long tail and long bill make it unmistakable.

The bird feeds on nectar and insects.

As it moves between flowers, pollen sticks to its head and feathers.

The bird then carries pollen to other plants.

This relationship makes sugarbirds important components of fynbos reproduction.

🦋 Table Mountain Beauty

One important insect pollinator is the Table Mountain Beauty, also called the Mountain Pride butterfly.

Its scientific name is Aeropetes tulbaghia.

SANParks describes it as an important pollinator of red-flowered mountain plants.

These include the famous:

red disa

The butterfly illustrates how some Cape plants depend upon very specific pollination relationships.

🌺 Red Disa

The red disa, Disa uniflora, is one of Table Mountain’s most famous flowers.

It thrives in moist mountain habitats.

Its vivid red flowers bloom during summer.

The species is closely associated with stream banks and wet areas.

Because many visitors seek out flowering disas, hikers should avoid leaving established paths or trampling fragile vegetation.

🌍 Cape Floral Region

Table Mountain lies within the Cape Floral Region, one of the greatest plant-diversity centers on Earth.

UNESCO recognizes the region for its:

• Exceptional plant diversity
• High endemism
• Evolutionary processes
• Specialized pollination
• Fire ecology

The Cape Floral Region contains thousands of plant species within an area much smaller than most global biodiversity hotspots.

Table Mountain represents one of its most visible and accessible sections.

🏛️ UNESCO World Heritage Status

Table Mountain National Park forms part of the Cape Floral Region Protected Areas UNESCO World Heritage Site.

The original World Heritage designation occurred in 2004.

The serial property was later expanded.

Its protected areas collectively conserve some of the most important surviving fynbos ecosystems.

Table Mountain’s UNESCO importance therefore comes primarily from biodiversity rather than simply from its famous scenery.

🏞️ Table Mountain National Park

Table Mountain itself lies within Table Mountain National Park.

The park extends far beyond the familiar flat summit.

It stretches through much of the Cape Peninsula.

Protected landscapes include areas around:

• Signal Hill
• Lion’s Head
• Table Mountain
• Devil’s Peak
• Twelve Apostles
• Silvermine
• Cape Point
• Cape of Good Hope

This creates an unusually long protected corridor through one of South Africa’s largest urban regions.

🏙️ An Urban National Park

Table Mountain National Park is remarkable because it borders dense urban development.

Hikers may walk from residential neighborhoods directly into wild mountain terrain.

This proximity creates major opportunities for recreation and conservation.

It also creates challenges involving:

• Wildfire
• Crime
• Invasive species
• Trail erosion
• Water use
• Development pressure
• Wildlife conflict
• Visitor numbers

Managing Table Mountain therefore requires balancing wilderness values with the realities of a major city.

🔐 Hiking Safety

Despite its tourist infrastructure, Table Mountain is a serious mountain environment.

SANParks advises hikers to:

• Avoid hiking alone
• Choose routes carefully
• Start early
• Tell someone the intended route
• Carry waterproof clothing
• Carry sufficient water
• Use appropriate footwear
• Stay together
• Carry navigation
• Monitor weather

Security also requires attention.

Because Table Mountain is an urban park, incidents of robbery have occurred on some routes.

Visitors should check current SANParks safety information before setting out.

🌬️ Wind Hazard

Strong wind is one of the mountain’s most common hazards.

The southeastern wind can become particularly powerful during summer.

Exposed edges and ridges can become difficult or dangerous.

Wind also increases heat loss.

A warm day at sea level may feel surprisingly cold near the summit.

Cableway operations may stop when wind becomes excessive.

🌫️ Mist and Navigation

The plateau can become confusing in thick mist.

Paths intersect.

Rock formations begin to look similar.

Visibility can fall dramatically.

Hikers should never assume that a flat summit means easy navigation.

Maclear’s Beacon lies several kilometers from the cableway.

Longer routes across the Back Table can involve much greater distances.

A map or reliable GPS route is important during extended hikes.

☀️ Summer Heat

Summer presents the opposite problem.

Platteklip Gorge and exposed western routes can become extremely hot.

Shade may be limited or nonexistent.

Rock surfaces radiate heat.

Hikers should carry:

• Plenty of water
• Sun protection
• Hat
• Food
• Electrolytes as appropriate

Early starts are generally preferable on hot days.

🌧️ Winter Weather

Cape Town winters are cooler and wetter.

Cold fronts can produce:

• Heavy rain
• Strong wind
• Low cloud
• Wet rock
• Rapid temperature drops

Forest routes such as Skeleton Gorge may become especially slippery.

Good waterproof clothing is important.

🔥 Wildfire

Wildfire is natural to the fynbos ecosystem.

However, fires can move very quickly in dry, windy weather.

Hikers should never enter closed areas or approach active fires.

Smoke can reduce visibility.

Wind direction may change rapidly.

In recent decades, several major fires have affected portions of Table Mountain National Park and nearby urban areas.

🧭 Why Table Mountain Is So Important

Table Mountain combines qualities rarely found together in one mountain.

It is:

• A major urban landmark
• More than 500 million years old
• Over 1,000 meters prominent
• One of Africa’s most recognizable mountains
• Home to thousands of plant species
• Habitat for globally unique animals
• A UNESCO-associated biodiversity site
• A sacred and historic Indigenous landscape
• One of southern Africa’s earliest recorded European ascents
• Accessible by both trail and cableway
• Surrounded by one of the world’s major cities

Its significance does not come from altitude.

Table Mountain demonstrates that a mountain only slightly above 1,000 meters can possess geological, ecological, cultural, and visual importance comparable with far taller peaks.

💡 Table Mountain Fun Facts

• Table Mountain reaches approximately 1,085 meters (3,560 feet).
• Its highest point is Maclear’s Beacon.
• The upper cableway station is lower than the actual summit.
• Table Mountain has approximately 1,068 meters of prominence.
• Its isolation is approximately 42.58 kilometers.
• Its Nearest Higher Neighbor is in the Helderberg region.
• The plateau is approximately three kilometers wide.
• Table Mountain is not a volcano.
• Its upper cliffs consist mainly of quartz-rich Peninsula Formation sandstone.
• Some of its rocks are more than 500 million years old.
• Cape Granite forms part of the mountain’s geological foundation.
• Ancient glacial deposits occur within the Table Mountain Group.
• The famous cloud over the summit is called the tablecloth.
• Indigenous people used the mountain long before European settlement.
• Hoerikwaggo is commonly translated as “Mountain in the Sea.”
• António de Saldanha made the first recorded European ascent in 1503.
• Platteklip Gorge is likely the historic ascent route.
• Platteklip remains the mountain’s most direct popular hiking route.
• Skeleton Gorge climbs through Afromontane forest.
• India Venster involves scrambling and exposure.
• Kasteelspoort approaches from the Atlantic side.
• Maclear’s Beacon was constructed in 1844 for geodetic surveying.
• The Table Mountain Aerial Cableway opened on October 4, 1929.
• The modern cable cars rotate during the journey.
• The cableway passed 33 million lifetime visitors in 2025.
• Table Mountain National Park contains more than 2,000 plant species.
• Fynbos includes proteas, ericas, restios, and geophytes.
• Fire is a natural and necessary ecological process.
• The Table Mountain ghost frog exists nowhere else on Earth.
• Its natural range is only about 7–8 square kilometers.
• Rock hyraxes, or dassies, are commonly seen around the upper mountain.
• Caracals live within the wider national park.
• About 250 bird species have been recorded within Table Mountain National Park.
• Cape sugarbirds help pollinate proteas.
• The Table Mountain Beauty butterfly is an important pollinator of red mountain flowers.
• Table Mountain National Park forms part of the Cape Floral Region UNESCO World Heritage property.

❓ Table Mountain FAQ

How high is Table Mountain?

Table Mountain reaches approximately 1,085 meters (3,560 feet) at Maclear’s Beacon.

Where is Table Mountain?

Table Mountain is located immediately south of central Cape Town in the Western Cape Province of South Africa.

What is the highest point on Table Mountain?

The highest point is Maclear’s Beacon.

Is the cableway station the summit?

No.

The upper cableway station is below Maclear’s Beacon.

Visitors must walk across the plateau to reach the mountain’s true high point.

How prominent is Table Mountain?

Table Mountain has approximately 1,068 meters (3,504 feet) of topographic prominence.

Is Table Mountain an ultra-prominent peak?

No.

An Ultra requires at least 1,500 meters of prominence.

How isolated is Table Mountain?

Its topographic isolation is approximately 42.58 kilometers (26.46 miles).

What is Table Mountain’s Nearest Higher Neighbor?

Higher terrain occurs around Helderberg Dome, east of Cape Town.

Is Table Mountain part of the Cape Fold Mountains?

Yes.

Its sandstone belongs to the geological formations associated with the wider Cape Fold Belt.

Is Table Mountain a volcano?

No.

Table Mountain is an erosional mountain built primarily from ancient sedimentary rocks over granite and older metamorphosed sediments.

What is Table Mountain made of?

Its upper cliffs consist mainly of hard quartz-rich sandstone of the Peninsula Formation within the Table Mountain Group.

Lower rocks include the Malmesbury Group and Cape Granite.

How old is Table Mountain?

The principal rocks forming the mountain are more than 500 million years old.

The modern shape developed much later through prolonged erosion.

Why is Table Mountain flat?

Its resistant sandstone plateau survived while softer surrounding rocks eroded more rapidly.

This differential erosion created the famous tabletop appearance.

What is the tablecloth cloud?

The tablecloth is a cloud that forms over Table Mountain when moist air is lifted, cools, and condenses near the summit.

Cloud can spill over the mountain edge like fabric draped across a table.

Who first climbed Table Mountain?

Indigenous people used the mountain long before written European records.

The first recorded European ascent was made by Portuguese navigator António de Saldanha in 1503.

What is Hoerikwaggo?

Hoerikwaggo is an Indigenous name associated with Table Mountain and is commonly translated as “Mountain in the Sea.”

What is the easiest route up Table Mountain?

Platteklip Gorge is generally the most straightforward summit hiking route.

It is technically simple but very steep and physically demanding.

How long does Platteklip Gorge take?

SANParks estimates roughly one to three hours uphill, depending on fitness, pace, and conditions.

Is Platteklip Gorge safe for beginners?

Fit beginners can use Platteklip under suitable conditions, but it should not be underestimated.

Heat, cold, wind, dehydration, and sudden weather changes can create serious problems.

Is India Venster harder than Platteklip?

Yes.

India Venster includes scrambling and exposed terrain and is better suited to hikers comfortable with that type of movement.

What is Skeleton Gorge?

Skeleton Gorge is a popular route from Kirstenbosch through Afromontane forest toward the Back Table and Maclear’s Beacon.

Can you take a cable car to Table Mountain?

Yes.

The Table Mountain Aerial Cableway connects Tafelberg Road with the upper plateau.

When did the Table Mountain Cableway open?

The cableway officially opened on October 4, 1929.

Does the cable car run every day?

Operations depend on weather, maintenance, and safety conditions.

Strong wind can close the cableway unexpectedly.

Visitors should check the official operating status before traveling.

Can you hike up and take the cable car down?

Yes, when the cableway is operating.

However, hikers should always be prepared to descend on foot in case the cableway closes because of weather or other conditions.

What plants grow on Table Mountain?

The mountain supports fynbos dominated by proteas, ericas, restios, and geophytes, along with wetlands and pockets of Afromontane forest.

How many plant species occur in Table Mountain National Park?

SANParks reports more than 2,000 plant species within the national park.

What is the Table Mountain ghost frog?

The Table Mountain ghost frog is a Critically Endangered frog found only in a tiny area of perennial streams on Table Mountain.

What animals live on Table Mountain?

Animals within the wider park include rock hyraxes, caracals, Cape porcupines, klipspringers, Cape grysbok, duiker, mongoose, numerous birds, reptiles, frogs, and insects.

Is Table Mountain a UNESCO World Heritage Site?

Table Mountain National Park forms part of the Cape Floral Region Protected Areas UNESCO World Heritage Site.

Is Table Mountain dangerous?

It can be.

Major risks include sudden weather changes, strong wind, heat, cold, fire, steep terrain, navigation errors, falls, dehydration, and crime on some trails.

Visitors should follow current SANParks safety guidance.

🔗 Related Articles

• Table Mountain, South Africa: Hiking Trails, Cableway & Visitor Guide
• Devil’s Peak
• The Devilish Origins of South Africa’s Iconic Devil’s Peak
• Mountains in South Africa: Highest Peaks, Major Ranges & Hiking Guide
• Types of Mountains: How the World’s Mountains Form

📚 Sources

• South African National Parks — Table Mountain National Park
• South African National Parks — Natural & Cultural History
• South African National Parks — Geology
• South African National Parks — Vegetation
• South African National Parks — Mammals
• South African National Parks — Birds
• South African National Parks — Insects
• South African National Parks — Hiking Trails
• South African National Parks — Safe Hiking
• UNESCO World Heritage Centre — Cape Floral Region Protected Areas
• South African National Biodiversity Institute — Table Mountain Ghost Frog
• Table Mountain Aerial Cableway — About Us & History
• Table Mountain Aerial Cableway — Cableway History
• Peakbagger — Table Mountain Topographic Data