Climbing from the Lowest Point on Earth: The Dead Sea to Jerusalem, a Road Cycling Gauntlet Where Altitude Counts Backwards

Most of the world’s famous climbs start at a positive elevation and finish even higher. The roads around the Dead Sea completely invert that logic—your starting point is 439.78 meters below sea level, the lowest known point on the Earth’s land surface. From there, no matter which direction you ride, the first thing you always do is “climb from negative back to positive.” Simply returning to sea level already constitutes a small climb, and the real challenge is only just beginning.

This unique geography makes the roads around the Dead Sea a particularly special piece of the puzzle for road cycling enthusiasts. Whether climbing from the Dead Sea’s western shore toward Jerusalem, or heading north or south along the Jordanian side, riders experience something that is difficult to replicate anywhere else: you know with certainty that you are starting from “the lowest standable point on the Earth’s surface” and riding yourself back up to normal elevation.

Route Basic Information Table

Data Discipline Note: The Dead Sea’s water level has been steadily declining in recent years due to agricultural and industrial water extraction in the surrounding region—a widely reported environmental issue. The surface elevation figure will continue to be revised downward over time. This article uses figures from recent literature and marks them with “approximately”; actual values will vary slightly depending on the year of your visit. Publicly available sources for precise gradient breakdowns along the road are limited, so the following segment descriptions are presented in qualitative terms.

A Landmark That Is Disappearing

Before discussing the riding experience, one thing is worth making clear: the Dead Sea is not just a tourist landmark—it is shrinking at an alarming rate. Because neighboring countries have for decades diverted large volumes of water from the Jordan River and underground sources for agricultural irrigation and industrial use, the inflow into the Dead Sea has dropped sharply. Combined with the region’s already extremely high evaporation rate, the falling water level has been a publicly documented environmental phenomenon for decades. This means that the Dead Sea shoreline road you ride today may be even farther from the actual water’s edge ten years from now—riding this route is, in a sense, witnessing a landscape in transformation.

The Dead Sea’s status as the lowest point on the Earth’s land surface is inseparable from its unique geological structure. It sits within the Syrian-African Rift system, a vast geological rift that extends all the way from the East African Rift. The Dead Sea is an inland saltwater lake (strictly speaking, its high salinity makes “sea” a questionable term, but the name has persisted) formed along this rift zone through plate divergence and crustal subsidence. This also explains why the terrain around the Dead Sea is so dramatic—you are standing at one of the deepest depressions of a geological structure spanning thousands of kilometers.

Interestingly, this rift system is part of the same geological belt as the East African highlands route featured in another article on this site (the western escarpment of the Great Rift Valley, where Iten, Kenya is located)—the Syrian-African Rift system extends southward and becomes the East African Rift. In other words, if you have the opportunity to visit both places, you are in a sense experiencing two ends of the same crack in the Earth: one end is the Dead Sea, the lowest point on the Earth’s land surface, while the other is the East African highland escarpment at over two thousand meters of elevation. Geologically related, yet the surface landscapes they present could not be more different.

High-Salinity Water and Mineral Landforms

The Dead Sea’s salinity is extremely high, generally considered to far exceed that of ordinary seawater. This is why people famously barely sink and float effortlessly in the Dead Sea. This high-salinity environment has created a highly distinctive mineral landscape along the Dead Sea’s shores—salt crystal deposits frequently accumulate along the shoreline, appearing almost snow-white under the sunlight, creating a stark contrast with the surrounding ochre-yellow desert mountains. When riding through these sections, the mineral landscape itself is a stunning visual experience in its own right, and it is no wonder that many photography enthusiasts make special trips to document this unique scenery.

Two Distinctly Different Road Experiences

There are two main coastal road systems around the Dead Sea: Israel’s Route 90, which runs north-south along the Dead Sea’s western shore and the West Bank, with official data indicating it is one of “the world’s lowest roads,” reaching its lowest point at approximately 393 meters below sea level; and Jordan’s Route 65, which extends along the Dead Sea’s eastern shore and connects southward to the Red Sea port city of Aqaba.

These two roads are generally flat along the coastline itself. The real challenge lies in “leaving” the Dead Sea shore and climbing into the inland mountains—whether it’s the Judean Desert mountain roads heading toward Jerusalem on the Israeli side, or the roads climbing toward the Amman highlands on the Jordanian side, these are the core sections that turn the Dead Sea region into a road cycling mecca.

Segment Breakdown

Using the climb from the Dead Sea’s western shore toward Jerusalem as an example, the route is divided into three qualitatively described segments based on terrain characteristics.

Early Segment: Climbing from Negative Back to Sea Level

The starting point is on the Dead Sea shore, where the road hugs the saltwater coastline, surrounded by typical Judean Desert terrain—barren yellowish-brown hills with almost no vegetation, occasionally dotted with drought-tolerant plants. The most distinctive psychological experience of this section is watching the elevation reading on your bike computer or GPS device climb from negative three to four hundred meters back up to “zero”—a ceremonial moment that almost no other climb offers. Temperature is also a major test on this section. The Dead Sea shore sits at low elevation, and combined with the desert climate, daytime temperatures are frequently noticeably high even outside the peak summer season. Moreover, because of the low-lying terrain and poor air circulation, the mugginess feels more pronounced than at higher elevations on the same latitude.

Middle Segment: The Desolate Climb Through the Judean Desert

After leaving the Dead Sea shore, the road begins climbing along the mountainous edge of the Judean Desert, with the gradient gradually intensifying. The views on both sides are extremely open—due to sparse vegetation and almost no obstructions, visibility is excellent, but this also means there is absolutely no shade. In many travelogues written by riders who have completed this section, it is described as “moon-surface desolation,” echoing the Dead Sea’s mineral-deposit landscape and creating a unique visual impact: barren ochre-yellow mountains, paired with the strangely blue-white glimmer of the Dead Sea’s surface reflecting in the distant sunlight.

This desert terrain poses a severe challenge for resupply planning—settlements along the way are scarce, and water sources and shade are practically nonexistent. Any mechanical failure or complete exhaustion of energy on this section could escalate into a situation requiring external rescue; it is not something you can solve by simply finding a roadside shop.

The Judean Desert is also a significant historical and religious site, with the surrounding mountains dotted with ruins related to biblical narratives and the discovery site of the Dead Sea Scrolls, such as the famous Masada—an ancient fortress ruin built on a rocky plateau and a UNESCO World Heritage Site. Historically, the Roman military camps besieging Masada are believed to have relied on water supplies from nearby towns, which indirectly illustrates that this desert region has depended on external resupply to sustain human activity since ancient times—a historical fact that remains just as relevant in the context of a modern rider planning their resupply strategy.

If time permits, many riders choose to arrange a brief stop during this section to visit Masada or other historical sites, transforming a purely physical challenge into a riding journey with historical and cultural depth. This is also what gives the routes around the Dead Sea a unique layer of richness compared to purely natural-terrain climbs (such as many famous passes in the Alps)—you are not just riding terrain; you are riding through the site of thousands of years of human civilization.

Final Section: Climbing into the Jerusalem Highlands

As the route approaches Jerusalem, the terrain continues to rise steadily, and the landscape gradually shifts from pure desert地貌 to a Mediterranean-style hilly landscape with more vegetation and settlements. This transition is also a product of the vertical climate zones created by the Syrian-African Rift System—within a horizontal distance of just twenty to thirty kilometers, the climate zones undergo changes nearly equivalent to crossing multiple latitudes. Jerusalem itself sits on a plateau at an elevation of 700 to 800 meters, meaning the total elevation gain from start to finish exceeds 1,000 meters, with the vast majority concentrated within a relatively limited distance—the gradient intensity is not to be underestimated.

Upon reaching the outskirts of Jerusalem, riders will clearly feel a drop in temperature and an increase in air humidity. Combined with the city’s layered limestone architecture and millennia-old historic districts, this creates a finishing scene starkly contrasting with the desert landscape just traversed. Many travelers who have completed this route describe the journey from the ochre-yellow desolation of the Dead Sea climbing into Jerusalem’s limestone city walls as a condensed trip spanning thousands of years of human civilization, all within just a few dozen kilometers.

The Alternative on the Jordanian Side

For those choosing to tackle a similar elevation difference on the Jordanian side, the route logic is largely similar—climbing from the eastern shore of the Dead Sea along Highway 65 toward the highlands in the direction of Amman. Jordan’s road infrastructure and tourism amenities have developed steadily in recent years, and the eastern shore of the Dead Sea is itself a popular hot-spring resort destination. This route offers comparatively more complete tourism services, but the same desert climate and sparse resupply challenges remain, and the planning principles are largely the same as on the Israeli side.

Power and Pacing Estimates (Physical Model Calculation)

Using a standard climbing power model for estimation, the following are physical estimates, not representative of any real rider’s or event’s record data:

P = (Fg + Fr + Fa) × v / Drivetrain Efficiency
Fg = m × g × sin(arctan(Grade))       Gravitational Component
Fr = m × g × cos(arctan(Grade)) × Crr   Rolling Resistance
Fa = 0.5 × ρ × CdA × v²              Air Resistance

Calculation assumptions:

• Total mass m = 70 kg rider + 9 kg bike and gear = 79 kg
• g = 9.81 m/s²
• Crr ≈ 0.005 (road tires on asphalt)
• CdA ≈ 0.32 m² (climbing position)
• Air density ρ: The unique feature of this route is that the air density on the below-sea-level sections is actually higher than the standard sea-level value, not lower—calculated at an average elevation of approximately 200 meters (a mid-route estimate combining the below-sea-level start and above-sea-level finish), the air density differs little from the standard sea-level value of 1.225 kg/m³, being only slightly lower
• Drivetrain efficiency ≈ 0.975

Based on an estimated total distance of approximately 25 km and total climbing of approximately 1,200 meters, the average gradient is approximately 4.8%. Plugging this into the model yields the following:

The above are physical model estimates and do not account for the reduction in actual physical output caused by intense desert sun exposure, the elevated perceived temperature from lack of shade, or the dehydration risk from inconvenient resupply. It is worth noting specifically that because this route has a relatively steep average gradient (close to 5%) and almost no flat sections for recovery along the way, the actual perceived fatigue during riding is typically higher than what the average gradient number alone might suggest. Riders are advised to plan this challenge with more conservative target power, prioritizing body cooling and hydration over chasing speed.

Perspectives from Taiwanese Riders

For Taiwanese riders, the best comparison for the Dead Sea climbing route is the Beiyi Highway combined with an imagined vertical climate shift from the southern coast to the mountains, but with an additional variable that Taiwan completely lacks—a below-sea-level starting point. Taiwan has no road starting point below sea level, so the psychological and physiological transition of “climbing from a negative value back to positive” is a unique experience that must be felt firsthand to be understood.

In terms of gradient and intensity, the route’s average gradient (approximately 4.5–5%) is similar to the middle-to-later sections of the Beiyi Highway, but the desert environment with no shade and sparse resupply makes the actual challenge far more difficult than Beiyi. If you have ever tackled a long climb from the southern coast into the mountains at noon in summer, you should have some sense of déjà vu regarding the rate of energy depletion caused by the combination of “muggy heat, no shade, and sparse resupply”—the Dead Sea section is essentially an intensified version of that experience.

Another comparable experience for Taiwanese riders is the combination of sun and sea breeze encountered when riding along the eastern coastal highway (Provincial Highway 11)—coastal sections often lack tree cover for shade, and with sunlight reflecting off the sea surface combined with humid, hot air, the perceived temperature frequently exceeds weather forecast figures. Although the Dead Sea is an inland salt lake rather than an ocean, the combination of its low-lying basin and desert climate makes the mugginess and solar reflection even more intense. Moreover, eastern Taiwan at least has scattered villages and convenience stores along the way for resupply, whereas the desert sections along the Dead Sea coast have resupply density that is lower by an order of magnitude or more.

Another point worth mentioning is the temperature inversion phenomenon—most people intuitively assume “higher elevation means colder,” but the Dead Sea’s enclosed low-lying topography, combined with intense desert solar radiation and lack of air circulation, often results in perceived temperatures that are more muggy and hot than at normal elevations at the same latitude. This is exactly the opposite of the intuitive Taiwanese mountain experience of “the higher you climb, the cooler it gets.” Riders need to pay special attention to this counterintuitive climatic characteristic and prepare for cooling and hydration in advance, rather than applying the existing Taiwanese climbing experience of “the higher you climb, the cooler it gets.”

Practical Preparation

• Season: Summer temperatures in the Dead Sea region frequently exceed 40°C, and the low-lying terrain amplifies the muggy heat. It is recommended to avoid midday in the height of summer and prioritize starting in the early morning during spring or autumn.
• Resupply: Settlements and resupply points along the route are scarce. Be sure to carry significantly more water and electrolyte supplements than you normally would, and plan emergency contact and evacuation procedures in advance.
• Geopolitical Situation: The Dead Sea area involves Israel and the West Bank region, where political and security conditions change from time to time. Before planning your trip, be sure to check the latest official travel advisories and on-the-ground conditions, and do not rely solely on past experience.
• Visas and Border Crossings: Although border crossings exist between Israel and Jordan, actual customs regulations, opening hours, and visa requirements change frequently. Always defer to the latest official announcements and do not assume that past information remains applicable.

Safety Reminder

The extreme heat and intense sunlight of the desert climate are the most direct health threats on this route. The risk of heat exhaustion and heatstroke is amplified on sections without shade. If you experience dizziness, nausea, unusual fatigue, or cessation of sweating while riding, stop immediately, seek shade to cool down, and replenish fluids and electrolytes. Seek medical attention promptly if symptoms are severe. The safety reminders provided in this article are general guidelines only and do not replace professional medical evaluation. Those with cardiovascular disease or other chronic conditions should consult a physician before departure and carefully assess whether prolonged outdoor exercise under such harsh climatic conditions is appropriate.

Geopolitical conditions are also an unavoidable practical consideration when planning this trip. The security situation around the Dead Sea can change with the shifting political landscape. Before departure, check the latest travel advisories issued by your country’s ministry of foreign affairs or government agencies, and remain flexible—adjust or cancel your plans if necessary. Regarding road traffic, local highways are primarily used by cars and tourist buses, with some sections seeing higher speeds. Cyclists should wear high-visibility gear and pay attention to shoulder conditions.

The Dead Sea’s uniquely high-salinity water is irritating to the skin and eyes. If your itinerary includes going into the water, be careful to avoid getting saltwater in your eyes. If your riding gear accidentally comes into contact with splashes of Dead Sea water, rinse it with fresh water as soon as possible, as salt crystals left to accumulate over time can corrode metal components, zippers, and other hardware. Additionally, this area is a low-lying, enclosed basin, and air quality may be affected under certain weather conditions. If you have a history of respiratory conditions, consult a physician before the trip to assess whether prolonged high-intensity outdoor exercise in this terrain is suitable.

Finally, pay close attention to the battery life and signal coverage of your communication and navigation devices—parts of the Judean Desert have rugged terrain and sparse population, and mobile network signals may be unreliable. Download offline maps, carry a power bank, and inform your companions or accommodation of your planned route and expected return time so that assistance can be reached promptly in case of an emergency.

Conclusion: Key Takeaways and Action Checklist

The roads around the Dead Sea offer cyclists a geographic spectacle that cannot be replicated anywhere else—starting from the lowest point on Earth’s land surface, riding yourself back up to normal elevation, passing through a barren landscape that resembles the lunar surface along the way. This route tests not just your leg strength, but your overall command of extreme climate conditions and logistical planning.

Pre-departure checklist:

1. Avoid the midday heat of midsummer; prioritize early mornings in spring or autumn for departure
2. Carry far more water and electrolyte supplies than you would normally bring
3. Check the latest geopolitical and travel safety information before departure
4. Confirm the latest official regulations regarding visas and border crossings
5. Plan emergency contact and evacuation protocols; do not assume you can get help at any point along the way
6. Watch for signs of heat exhaustion and heatstroke; stop and cool down immediately if you feel unwell
7. Preserve the psychological ritual of starting at “negative elevation” and fully savor this unique climbing journey

Few places allow you to personally experience the moment your elevation reading flips from negative to positive while riding—the roads around the Dead Sea turn this geographic marvel into a real, attainable cycling challenge.

For road cycling enthusiasts who closely follow elevation numbers and power curves, the significance of the Dead Sea route may go beyond simply adding another climbing record. It is more like a three-dimensional geography lesson—when you watch your GPS altimeter climb from a negative value all the way back up to a three-digit positive number, the sense of accomplishment from that numerical reversal carries a completely different weight than simply setting a new personal record (PR) on a climb. This is also why, despite the harsh climate, scarce supplies, and shifting geopolitical situation along the way, the roads around the Dead Sea continue to attract long-distance riders from around the world who are willing to take on the challenge, coming back again and again to experience this one-of-a-kind journey of elevation inversion.

Related Reading

• Starting from 86 Meters Below Sea Level: Dante’s View in Death Valley, the World’s Most Unforgiving Road to Ride
• From Sea Level to Above the Clouds: Haleakalā on Maui, a 3,000-Meter Journey Through Three Climate Zones
• Riding to the Place Closest to Space: Ecuador’s Chimborazo, the Road at the Furthest Point from Earth’s Center
• A Road Where Elevation Counts Backwards: Jeju’s Route 1100, the Highest Paved Ascent on Korea’s Island Across the Flanks of Hallasan