Skip to content
VisitIsrael
Makhtesh HaGadol & HaKatan: The Two Other Negev Craters

Makhtesh HaGadol & HaKatan: The Two Other Negev Craters

By The Visit Israel Editorial Team · Last updated

Plan Your Negev Crater Visit

Rent a Car for the Negev Craters DiscoverCars

Rent a Car for the Negev Craters

Both Makhtesh HaGadol and HaKatan are car-only destinations — no public transport reaches either crater. Pick up a rental in Tel Aviv, Jerusalem, or Beer Sheva and drive south on Route 40 or Route 25. A single day car trip can link both craters with Sde Boker and Mitzpe Ramon.

Live prices & reviews on DiscoverCars

Affiliate link — we may earn a commission at no extra cost to you.

Compare car hire

via DiscoverCars

Negev Desert Tours from Tel Aviv Tour

Negev Desert Tours from Tel Aviv

Guided Negev day tours from Tel Aviv cover the desert craters, Sde Boker, and Mitzpe Ramon — a practical alternative to self-driving in unfamiliar desert terrain. Compare operators, departure times, and group sizes.

Live prices & reviews on GetYourGuide

Affiliate link — we may earn a commission at no extra cost to you.

Browse Negev tours

via GetYourGuide

Hotels near the Negev Craters Stay

Hotels near the Negev Craters

Yeruham (5 km from Makhtesh HaGadol) has a handful of guesthouses and B&Bs. Mitzpe Ramon (45 km from HaGadol, 55 km from HaKatan) is the best-equipped base with hotels at every level, from the iconic Beresheet on the crater rim to budget guesthouses in town.

Live prices & reviews on Booking.com

Affiliate link — we may earn a commission at no extra cost to you.

Find hotels nearby

via Booking.com

Israel has five makhteshim — erosion craters unique to the Negev and Sinai, found nowhere else on Earth. Most visitors know only one: Makhtesh Ramon, the world’s largest, overlooked by the town of Mitzpe Ramon. But two other craters lie within an hour of Beer Sheva, geologically as dramatic as Ramon and almost entirely free of tourist crowds: Makhtesh HaGadol (the Big Crater, near Yeruham) and Makhtesh HaKatan (the Small Crater, near Dimona).

This guide covers both.


What is a makhtesh?

Before you visit, it’s worth understanding what you’re looking at — because the Negev makhteshim are routinely misidentified in photos and travel writing as meteor craters or ancient volcanoes.

A makhtesh (מַכְתֵּשׁ in Hebrew; the plural is makhteshim) is a geological formation created by erosion, not by impact or eruption. The process: tectonic forces dome up a layer of hard limestone crust; rivers gradually cut drainage channels at the edges of the dome; over tens to hundreds of millions of years those rivers erode deeper and deeper through the softer sedimentary rock inside, leaving a steep-walled enclosed depression with a flat floor and a seasonal wadi (stream) exiting through a narrow gorge.

The floors of these craters expose sequences of Triassic and Jurassic marine sediment — rock formed when this desert was a shallow arm of the ancient Tethys Sea, 200–250 million years ago. That’s why you find ammonite and belemnite fossils on the crater floors of both HaGadol and HaKatan, and why the layered coloured sands of HaGadol display vivid reds, ochres, yellows, and greens from mineral variation in ancient seafloor sediments.


Makhtesh HaGadol — the Big Crater

The basics

Makhtesh HaGadol measures roughly 14 km long and 6 km wide, making it the second-largest makhtesh in Israel. Despite that scale, it receives perhaps 5–10% of Makhtesh Ramon’s visitor numbers. On a weekday morning in March you may have the northern rim viewpoint entirely to yourself.

The crater lies immediately south of Yeruham, a small development town about 50 km east of Beer Sheva. Yeruham itself is pleasant — it sits beside the artificial Yeruham Lake (built in the 1960s to collect floodwater; a good birdwatching spot) — but the crater is the reason to come.

The rim and the coloured sands

The northern rim viewpoint is 5 km south of Yeruham centre via a signposted dirt road (passable in a standard car in dry conditions; check local conditions after rain). From the car park, a short path leads to the rim edge: the view drops suddenly into a wide, flat-floored depression surrounded by steep walls of stripped sedimentary rock. The walls expose geological strata in almost horizontal bands — you can read the different formations like pages in a book.

The standout visual feature of HaGadol is the coloured sands on the crater floor. Iron-rich sandstone layers produce vivid red and orange exposures; clay-rich layers add yellow and green; white limestone layers provide contrast. From the rim the floor looks like a patchwork of mineral pigments spread across the desert. Walking trails on the crater floor bring you directly to the sand outcrops.

Nahal Tzafit and the crater floor trails

The most rewarding trail at HaGadol begins at the northern rim car park and descends into the Nahal Tzafit canyon — a dry riverbed carved through the crater wall. The lower section of the trail (approximately 4 km return, 2–3 hours) passes through white chalk cliffs, exposed coloured-sand formations, and sections of dry riverbed filled with smooth-worn boulders. After winter rains, seasonal pools form at the base of the canyon walls.

A longer crater crossing trail traverses the floor from north to south (approximately 12 km one-way; requires car shuttle or return). This route is best in spring when temperatures are manageable and the desert floor has patches of yellow and white flowers.

The INPA maintains the trails; carry the Amud Anan app for GPS navigation and current trail condition updates.

Ammonite fossils

The HaGadol crater floor is one of the more accessible fossil sites in Israel. Ammonite fossils (extinct spiral-shelled cephalopods related to nautiluses) appear in loose rock on the crater floor, identifiable by their coiled form. Belemnite fossils (cylindrical internal shells of an extinct squid-like animal) are also common. Do not remove fossils — INPA regulations prohibit taking geological or fossil material from nature reserves.


Makhtesh HaKatan — the Small Crater

The basics

Makhtesh HaKatan is the smallest of Israel’s five makhteshim: roughly 5 km east-west by 7 km north-south. Its location east of Dimona (about 65 km from Beer Sheva) makes it the most isolated and least-visited of the three main craters. That isolation is its greatest asset.

What distinguishes HaKatan visually is the near-perfect symmetry of its walls. The crater is almost oval in plan; from the rim viewpoints the opposing walls line up with geometric precision. Geologists attribute this to the unusually regular doming of the rock layer that was eroded away. The overall effect, particularly in the low-angle light of early morning or late afternoon, is of a vast natural amphitheatre.

The rim trail

A marked loop trail circles a section of the northern and eastern rim (approximately 5 km, 2 hours, relatively easy). The path follows the crater edge with near-constant views into the depression below. Several points along the rim offer descent routes to the crater floor — these involve some scrambling on loose rock and are best attempted with hiking poles and solid footwear.

The Nahal Shaharut wadi cuts through the southern wall of HaKatan and provides the main descent route for floor crossings. Hikers who want to do a crater-floor traverse rather than a rim loop should allow 4–5 hours for the round trip.

Practical access

The turnoff to Makhtesh HaKatan is signposted from Route 25 east of Dimona. A dirt track (7 km; passable in a standard car in dry conditions) leads to the northern rim car park. There are no facilities at the crater — no water, no toilets, no shade. Arrive with sufficient water and food for your planned activity.


Combining both craters

Makhtesh HaGadol and Makhtesh HaKatan are 35 km apart by road (via Route 25). A single day trip — starting at HaGadol in the morning and reaching HaKatan by early afternoon — is entirely feasible. A suggested circuit from Beer Sheva:

StopDistance from Beer ShevaTime on site
Makhtesh HaGadol (Yeruham)50 km2–3 hours
Drive to Makhtesh HaKatan+35 km
Makhtesh HaKatan (near Dimona)85 km from BS2 hours
Return to Beer Sheva~1 h drive

Allow 7–8 hours for the full circuit at a relaxed pace. Add Yeruham Lake (15 minutes, free) at the start for birdwatching, or extend south to Mitzpe Ramon (45 km from HaGadol) to complete all three major Negev craters in a long day.


Getting there

By car (the only practical option): Both craters require a car. There are no public transport routes to either crater rim.

The access tracks to both crater rims are unpaved but compact gravel, manageable in a standard saloon car in dry conditions. After heavy rain, verify conditions locally before driving the tracks.

Nearest fuel: Yeruham (for HaGadol); Dimona (for HaKatan). Fill up before leaving the towns — there are no fuel stations at the craters.


When to visit

SeasonConditionsNotes
Mar–Apr (Spring)18–27°C, occasional wildflowersPeak season; busy weekends
Oct–Nov (Autumn)18–26°C, clear skiesExcellent hiking; quiet
Dec–Feb (Winter)5–18°C, cold nightsBest photography light; check for rain
Jun–Aug (Summer)35–42°CStart before 7am; hike only to 10am

Avoid visiting in the immediate aftermath of winter rainstorms — the unpaved access tracks can become temporarily impassable and flash flood risk in the canyon sections is real. The Amud Anan trail app publishes current access alerts.


What to bring


Where to stay

Yeruham (adjacent to Makhtesh HaGadol) has a small selection of guesthouses and B&Bs — useful if you want to be at the rim at sunrise.

Dimona (nearest town to HaKatan) has budget hotels; it is a working-class industrial town without the heritage interest of Yeruham.

Mitzpe Ramon is the most comfortable and atmospheric base for exploring all three Negev craters. From there, HaGadol is 45 km north and HaKatan is 55 km north — both reachable as day outings from the same base. The town has a full range of accommodation from the crater-rim Beresheet Hotel to Selina Ramon glamping tents and budget guesthouses. See the Mitzpe Ramon guide for the full hotel and activity breakdown.


The three Negev craters at a glance

Makhtesh RamonMakhtesh HaGadolMakhtesh HaKatan
Size40 × 10 km14 × 6 km5 × 7 km
NearMitzpe RamonYeruhamDimona
Drive from Beer Sheva50 km south50 km east65 km east
Best forAll-round Negev experienceColoured sands + fossilsSymmetrical rim, solitude
Visitor numbersHighLowVery low
Town infrastructureFull (hotels, restaurants, tours)Basic (guesthouses)Minimal

For the full Negev picture:

Frequently asked questions

What is the difference between Makhtesh HaGadol, HaKatan, and Makhtesh Ramon? +

All three are makhteshim — a geological formation unique to Israel's Negev and Sinai deserts, formed by tectonic uplift followed by millions of years of water erosion. Makhtesh Ramon (covered in the Mitzpe Ramon guide) is the world's largest at 40 km long and is the most visited, with an established tourism infrastructure. Makhtesh HaGadol (the Big Crater) is 14 km long and 6 km wide, located near Yeruham, and is famous for its multi-coloured sandstone exposures and ammonite fossil beds. Makhtesh HaKatan (the Small Crater) is the smallest of the three — roughly 5 km × 7 km — near Dimona, with the most perfectly symmetrical walls of any makhtesh. HaGadol and HaKatan receive a fraction of Ramon's visitor numbers, making them the choice for travellers who want wild Negev landscapes without the crowds.

Are the craters volcanic or meteor impacts? +

Neither. All three Negev makhteshim are erosion craters — a geological type found only in Israel's Negev and in the Sinai. They form when tectonic forces dome up a cap of hard limestone; rivers cut drainage channels at the dome's edges; then millions of years of erosion hollow out the softer sedimentary rock inside. The Hebrew word makhtesh has no exact English equivalent — 'erosion cirque' is the closest geological term. The crater floors expose strata laid down when this desert was a Tethys Sea 200–250 million years ago.

How do I get to Makhtesh HaGadol from Tel Aviv? +

Drive south on Route 6 (toll motorway) to Beer Sheva, then east on Route 25 toward Yeruham. The crater viewpoint on the northern rim is signposted from the Yeruham junction. The total distance from Tel Aviv is approximately 175 km; driving time is around 1 hour 45 minutes. There is no direct public transport to either crater — the Egged bus to Yeruham or Dimona drops you in town, several kilometres from the rim access points. A rental car from Beer Sheva, Jerusalem, or Tel Aviv is the only practical option.

Can I combine both craters in one day trip? +

Yes — it's a full but manageable day. Makhtesh HaGadol (near Yeruham) and Makhtesh HaKatan (near Dimona) are about 35 km apart by road. Allow 2–3 hours at HaGadol (including the Nahal Tzafit lookout) and 1.5–2 hours at HaKatan, plus driving time. Starting by 7:30am from Beer Sheva or 6:30am from Tel Aviv lets you finish by early afternoon. Many drivers extend the loop south to Mitzpe Ramon (45 km from HaGadol) for a three-crater day trip.

What is the best season to visit? +

October to April. Spring (March–April) brings yellow and white Negev wildflowers along the crater rims and comfortable daytime temperatures of 18–27°C. Autumn (October–November) offers similar hiking conditions with fewer visitors than the spring school-holiday peak. Summer (June–August) is doable but brutal on the crater floors — temperatures exceed 38°C by 10am; any hiking must start before 7am. Winter (December–February) brings the clearest skies and dramatic low light for photography; nights are cold (2–8°C). Avoid visiting during and immediately after heavy rain (November–February) — desert flash floods can render rim access roads temporarily impassable.

Are there marked hiking trails at both craters? +

Yes. Makhtesh HaGadol has a network of INPA-marked trails including the popular Nahal Tzafit route that descends into the canyon from the rim, and a longer crossing trail that traverses the crater floor. Makhtesh HaKatan has a shorter but spectacular loop trail around the rim (approximately 5 km, 2 hours) and a descent route to the floor. Trailhead parking is free. Download the Amud Anan offline trail app before your visit — it covers both craters with GPS-tracked routes and difficulty ratings. Water is not available at the craters — carry at least 2 litres per person and 3 litres in summer.

Is an Israel National Parks Pass valid at the craters? +

Makhtesh HaGadol and HaKatan are managed by the Israel Nature and Parks Authority (INPA) and entry to the craters and their trails is free — no ticket or INPA pass is required at either site. If you are combining the craters with other INPA sites such as Ein Avdat, Avdat, Tel Be'er Sheva, or Masada on the same trip, the annual INPA pass (Kartis Teva, approximately ₪220/adult) will save money. See the Israel National Parks Pass guide for current prices.

What makes the coloured sands of Makhtesh HaGadol special? +

The crater floor of Makhtesh HaGadol exposes a cross-section of Triassic and Jurassic sedimentary strata — layers of sandstone, shale, and limestone laid down in different marine environments 200–250 million years ago. Different mineral compositions produce different colours: iron oxides create reds and ochres; clay minerals produce yellows and greens; white limestone layers contrast sharply. Walking across the floor you move through geological time in a way visible nowhere else in Israel. The same strata also preserves ammonite fossils (spiral-shelled cephalopods) and belemnite fossils in accessible locations — look carefully at loose rocks on the crater floor.

By The Visit Israel Editorial Team · Last updated