This article covers international land boundaries that are undefined, undelimited, undemarcated or disputed, with particular attention to borders across icefields and glaciers such as the Chile–Argentina boundary on the Southern Patagonian Ice Field and the United States–Canada boundary in the Alask
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| Main topic | International land boundaries that are not fully agreed, mapped or marked |
|---|---|
| Key terms | Allocation, delimitation, demarcation, administration |
| Best-known undefined icefield section | Southern Patagonian Ice Field, Chile–Argentina, between Mount Fitz Roy and Cerro Murallón |
| Governing Chile–Argentina agreement | 1998 agreement on the Fitz Roy–Daudet sector (ratified 1999) |
| Approximate length of undefined Chile–Argentina section | About 50 km |
| Alaska boundary settled by | Alaska Boundary Tribunal, 1903 |
| Remaining US–Canada disputes | Maritime only (for example Dixon Entrance, Beaufort Sea, Machias Seal Island) |
| Glaciated border with active military presence | Siachen Glacier region, India–Pakistan |
| Recent example of glacier-driven border change | Italy–Switzerland redrawing near the Matterhorn, agreed 2023 |
A territorial dispute is a disagreement between two or more political entities over who possesses or controls a territory. The territory can be land, water or airspace. Not every border problem is a dispute, though. Many international land boundaries are accepted by both neighbouring countries but have never been fully described in a treaty, accurately mapped, or physically marked on the ground. This article covers both kinds of situation: borders that are actively disputed, and borders that are simply unfinished.
Borders across icefields, glaciers and high mountain ranges are a special case. Survey teams find them hard to reach. Physical markers cannot easily be placed on moving ice. Treaties written in the 19th century often described the line using geographic ideas, such as "the highest summits" or "the line dividing the waters", that turned out to be ambiguous once the land was properly explored. The best-known example is a section of roughly 50 kilometres on the Southern Patagonian Ice Field between Chile and Argentina. That section has no agreed boundary line at all, and maps in both countries still show it as undefined.
Other icy borders are legally settled but are defined mainly by coordinates rather than by markers on the ground. The boundary between the US state of Alaska and Canada in the coast mountains is the main example. Its land line was fixed by an arbitration tribunal in 1903, and the only active disagreements between the two countries in that region concern sea areas. Climate change has added a new problem: where a treaty ties a boundary to a glacier or a watershed, melting ice can move the line.
Terminology
Writers on boundaries use several terms with specific meanings. A widely used framework comes from the American geographer Stephen B. Jones, whose 1945 handbook Boundary-Making divided the creation of a border into four stages.
- Allocation: a political decision about which territory belongs to which state, often in broad terms.
- Delimitation: the precise description of the boundary line in a legal text, usually a treaty or arbitral award. The text may give coordinates, list named peaks, or state a principle such as following a river or watershed.
- Demarcation: the physical marking of the line on the ground. Methods include concrete or metal monuments, buoys, fences, or a cleared strip through forest.
- Administration: the ongoing management and maintenance of the boundary by the states involved.
Using these stages, several kinds of "unsettled" border can be distinguished.
- Undefined or undelimited border: no agreed legal description of the line exists for a section. The Chile–Argentina section on the Southern Patagonian Ice Field is in this category.
- Undemarcated border: the line is legally described, but it has not been marked on the ground. This is common in remote deserts, forests and mountains. It does not necessarily mean either side disputes the line.
- Disputed border: at least one state rejects the line claimed by the other, or rejects the legal basis of an existing treaty or award.
- De facto line: a line of actual control that separates areas administered by each side but has no agreed legal status as a boundary. Examples are the Line of Control in Kashmir and the Line of Actual Control between India and China.
A watershed (in British usage) or drainage divide is the line separating land that drains to one river system or ocean from land that drains to another. A nunatak is a rock peak or ridge that sticks up through an ice sheet or icefield. Both terms come up often in descriptions of icefield borders.
Why some borders remain unsettled
Borders stay unsettled for a combination of practical, legal and political reasons.
Vague or outdated treaties
Many boundary treaties were written before the land had been surveyed. Negotiators described the line using general principles, expecting later surveys to fill in the details. When the surveys were done, the principles sometimes pointed to different lines. In Patagonia, for example, the highest peaks of the Andes often do not lie on the continental drainage divide. A treaty that assumed the two coincided produced competing interpretations.
Difficult terrain
Icefields, glaciers, high ridges and dense forest make survey work slow, dangerous and expensive. Before satellite positioning, establishing exact coordinates in such places could take years of fieldwork. Some sections were left for "later" and were never completed.
Colonial legacies
Many boundaries in Africa, Asia and the Americas were drawn by colonial powers, sometimes with little local knowledge. Newly independent states have usually kept colonial boundaries under the legal principle of uti possidetis juris, which holds that new states inherit the administrative borders of the former colonial units. Where those colonial lines were vague or overlapping, disputes were inherited too.
Political sensitivity
Even small areas can carry national symbolism. Governments may prefer to leave a section undefined rather than risk being seen at home as giving up territory. Legislatures may refuse to ratify agreements that negotiators have already signed, as happened with an earlier Chile–Argentina proposal for the Southern Patagonian Ice Field.
Physical change
Rivers shift course, coastlines erode, and glaciers retreat. If a treaty ties the boundary to a natural feature, the legal line may move with it, or it may stay fixed while the feature moves away. Either outcome can create uncertainty.
Special problems of icefield and glacier borders
Borders on ice raise problems that rarely arise elsewhere.
- No permanent markers. Glaciers flow, typically by metres to hundreds of metres per year. A monument placed on the ice surface would be carried away. Markers can be placed only on bedrock, usually on nunataks or peaks.
- Hidden drainage divides. Where a treaty follows a watershed, the true divide may lie under hundreds of metres of ice. The divide on the ice surface can differ from the divide in the bedrock below, and the surface divide can shift as the ice changes.
- Changing landscape. Retreating glaciers expose new valleys and lakes. Features that negotiators relied on may change shape or disappear.
- Access and cost. Survey teams often need aircraft, mountaineering skills and favourable weather. Field seasons are short.
- Low practical pressure. Few people live on or use icefields. Governments may see little urgency in completing a line that affects no settlements, so work is postponed.
Because of these problems, many icefield boundaries are defined by straight lines between surveyed peaks rather than by continuous markers. Modern tools, including satellite positioning, aerial and satellite imagery, and digital elevation models, have made precise definition much easier. Political agreement remains the main obstacle.
Chile–Argentina: the Southern Patagonian Ice Field
The ice field
The Southern Patagonian Ice Field (Spanish: Campo de Hielo Patagónico Sur, often called Hielos Continentales) lies along the southern Andes. It is commonly described as the largest body of ice in the Southern Hemisphere outside Antarctica. Large outlet glaciers flow from it on both sides. On the Argentine side these include the Upsala, Viedma and Perito Moreno glaciers. Protected areas on both sides include Los Glaciares National Park in Argentina and Bernardo O'Higgins National Park in Chile.
Mount Fitz Roy (also called Cerro Chaltén), a granite peak about 3,400 metres high, stands at the north-eastern part of the disputed sector. It is a well-known climbing destination near the Argentine village of El Chaltén.
Treaty background
The modern Chile–Argentina boundary rests on the Boundary Treaty of 1881. In the Andes, this treaty placed the line along the highest summits that divide the waters. In northern and central sections the highest peaks and the drainage divide mostly coincide. In Patagonia they often do not. Argentina tended to stress the highest-peaks principle and Chile the drainage-divide principle.
In 1898 the two countries' boundary experts, Francisco Moreno for Argentina and Diego Barros Arana for Chile, agreed on parts of the line, including a description of the sector running across the ice field. Other disagreements were referred to arbitration by the British Crown. The 1902 award, issued under King Edward VII, divided the contested Patagonian areas between the two countries. The British surveyor Thomas Holdich carried out field work for the arbitration. In the ice field sector, however, the line described in 1898 relied on a very limited knowledge of the terrain. Later surveys showed that the description could be read in different ways.
Laguna del Desierto and the 1991 agreements
Disagreements continued in several places along the Patagonian border through the 20th century. In 1991 Presidents Patricio Aylwin of Chile and Carlos Menem of Argentina agreed on most of the remaining open points along the whole boundary. Two areas were left for separate treatment.
- Laguna del Desierto, a lake area just north of Mount Fitz Roy, was submitted to an arbitral tribunal of Latin American jurists. In 1994 the tribunal ruled in favour of Argentina's interpretation. Chile requested a revision, which was rejected in 1995.
- The Southern Patagonian Ice Field was to be divided along a compromise line known as the poligonal (polygonal line). This proposal met strong opposition in both countries, especially in their legislatures, and was eventually abandoned.
The 1998 agreement
On 16 December 1998, Presidents Eduardo Frei Ruiz-Tagle of Chile and Carlos Menem of Argentina signed a new agreement to define the boundary from Mount Fitz Roy to Cerro Daudet. Both national congresses ratified it in 1999. The agreement divided the sector into two parts.
- Section A, the southern part from Cerro Murallón to Cerro Daudet, was given an agreed line described in the treaty.
- Section B, the northern part from Mount Fitz Roy to Cerro Murallón, was handled differently. The agreement drew a rectangular area defined by coordinates and stated that the boundary inside it would be delimited later by the Chile–Argentina Mixed Boundary Commission (Comisión Mixta de Límites). The line was to be based on a detailed map at a scale of 1:50,000, which the commission was to prepare.
The section left for later is roughly 50 kilometres long. More than two decades after ratification, the commission has not completed the delimitation.
Current state
As a result, this part of the Chile–Argentina border is literally undefined. It is not a case of a line agreed in law but not yet marked. No agreed legal line exists inside the rectangle. Official maps in both countries usually show the area with a dotted line, a hatched or boxed area, or a note that the boundary is pending. Maps that appear to place the area on one side have caused diplomatic protests from the other.
The situation is generally described as calm. Both governments treat it as a technical matter for the joint commission rather than a source of conflict, and no military confrontation has taken place there. Still, the issue comes up regularly in national debate, especially in connection with tourism, mapping and national parks. Glacier retreat on the ice field adds a further complication, because the drainage pattern under and around the ice is changing.
United States–Canada: the Alaska boundary
Origins
The boundary between Alaska and Canada has two main parts. The northern part follows the 141st meridian west from Mount Saint Elias north to the Arctic Ocean. The southern part runs along the coast mountains of the Alaska Panhandle, separating Southeast Alaska from British Columbia and Yukon. The whole Alaska–Canada boundary is roughly 2,475 kilometres long.
The line originates in the Anglo-Russian Convention of 1825, which divided Russian America from British North America. For the panhandle, the convention said the boundary would follow the summits of the mountains parallel to the coast. Where those summits lay more than ten marine leagues (about 56 kilometres) inland, the line would follow a line parallel to the coast's windings at that distance. The convention did not say clearly how "the coast" should be measured where long, deep inlets cut into the land.
The United States bought Alaska from Russia in 1867 and inherited the boundary. The ambiguity became urgent during the Klondike Gold Rush of the late 1890s, when control of the ports at the heads of the inlets, such as Skagway and Dyea, gave access to the Yukon goldfields.
The 1903 tribunal
Under the Hay–Herbert Treaty of January 1903, the dispute went to the Alaska Boundary Tribunal. It had six members: three American (Elihu Root, Henry Cabot Lodge and George Turner), two Canadian (Louis-Amable Jetté and Allen Aylesworth) and one British (Lord Alverstone, the Lord Chief Justice of England). Britain was still responsible for Canada's foreign relations at the time.
In October 1903 the tribunal decided by four votes to two, with Lord Alverstone siding with the American members on the main questions. The decision measured the boundary around the heads of the inlets, keeping the panhandle's ports under US control. The two Canadian members refused to sign the award. The result caused widespread resentment in Canada and is often cited as one of the events that encouraged Canada to seek more independence in its foreign policy.
How the line is defined on the icefields
The award, and the survey work that followed, defined much of the panhandle boundary as a series of straight lines connecting specified mountain peaks. Joint survey parties determined the positions of these peaks over the following decades. Under treaties of 1908 and 1925, the International Boundary Commission, with one commissioner from each country, maintains the boundary.
Along most of the US–Canada border, the commission maintains survey monuments and a cleared strip called the "vista" through forested areas. On the Juneau Icefield, the Stikine Icefield and the ice-covered ranges around Mount Saint Elias, this is not possible. There the boundary exists mainly as a set of coordinates for summits and turning points, with straight lines between them. Some of the reference peaks are nunataks rising through the ice. Few or no physical markers stand along long stretches of ice.
This means the line is legally settled even where nothing on the ground shows it. Some published maps show short stretches, for example in the Juneau Icefield area near Devils Paw, as undefined or approximately located. Sources differ on whether such markings reflect a genuine gap in the legal definition or only incomplete surveying and cartographic convention. Neither government treats any part of the Alaska land boundary as an active territorial dispute.
Remaining disagreements in the region
The remaining disputes between the United States and Canada are maritime, not on land.
- Dixon Entrance, the strait between the southern tip of the Alaska Panhandle and Haida Gwaii in British Columbia. Canada treats a line drawn in the 1903 award, often called the "A–B line", as the maritime boundary. The United States regards that line as dividing only land territory and claims an equidistance-based line further south for maritime purposes.
- Beaufort Sea, north of the Alaska–Yukon land boundary. Canada argues that the 141st meridian continues out to sea. The United States argues for a line perpendicular to the coast, which produces a wedge of overlapping claims.
- Machias Seal Island and North Rock, in the Gulf of Maine on the Atlantic coast, both claimed by both countries.
In June 2022, Canada and Denmark (for Greenland) resolved their long-running dispute over Hans Island in the Nares Strait by dividing the island between them. This created a short land border between Canada and the Kingdom of Denmark.
Other glaciated and high-altitude borders
Siachen Glacier (India and Pakistan)
The ceasefire line in Kashmir agreed in 1949, and the Line of Control established after the 1972 Simla Agreement, were mapped only as far as a point known as NJ9842. Beyond it, the agreements described the line only vaguely as running "thence north to the glaciers". The Siachen Glacier, roughly 76 kilometres long, lies in this undelimited area in the Karakoram range.
In April 1984 India launched Operation Meghdoot and took control of the glacier and most of the Saltoro Ridge to its west. Pakistani forces hold positions on the western slopes. The line separating the two armies is called the Actual Ground Position Line. Siachen is often called the highest battlefield in the world. A ceasefire has generally held since 2003, but troops remain deployed. Far more soldiers have died from altitude, cold and avalanches than from combat.
India and China
The boundary between India and China has never been jointly delimited along most of its length. The two countries are separated by the Line of Actual Control, which neither side has fully defined on maps exchanged with the other. Major disputed areas include Aksai Chin, administered by China and claimed by India, and Arunachal Pradesh, administered by India and claimed by China as "South Tibet". Much of the line runs through high, glaciated terrain. A deadly clash in the Galwan Valley in June 2020 was the most serious incident in decades.
The Alps
Several Alpine borders follow watersheds across glaciers. As the glaciers shrink, the drainage divide can move. Italy reached agreements in the late 2000s with Austria and with Switzerland recognising that some sections of their glacier borders are "mobile", meaning that they move with the watershed. In 2023 Switzerland and Italy agreed to redraw part of their border near the Matterhorn, around the Theodul Glacier and the Plateau Rosa area, because melting ice had shifted the divide. Formal approval on the Italian side was reported as still pending after the Swiss approval.
The summit of Mont Blanc, the highest peak in western Europe, is subject to a long-standing disagreement between France and Italy. Italy holds that the border, under the arrangements that followed the 1860 transfer of Savoy to France, runs across the summit. French official maps place the border lower on the Italian side, so that the summit lies entirely in France. The two countries have not resolved the question. Local decisions by French authorities affecting areas that Italy considers Italian, such as the Col du Géant area, have prompted Italian protests.
Antarctica
Seven countries claim parts of Antarctica: Argentina, Australia, Chile, France, New Zealand, Norway and the United Kingdom. The claims of Argentina, Chile and the United Kingdom overlap on the Antarctic Peninsula. Part of the continent, Marie Byrd Land, is not claimed by any state. Under Article IV of the Antarctic Treaty (signed 1959, in force 1961), existing claims are neither recognised nor rejected, and no new claims may be made while the treaty is in force. These lines are therefore effectively frozen rather than settled.
Other high-mountain cases
- China and Bhutan have not concluded a boundary treaty. Disputed areas include the Doklam plateau, scene of a 2017 standoff involving Indian and Chinese troops. In 2021 the two countries signed a memorandum on a "three-step roadmap" for boundary talks.
- China and Tajikistan settled their dispute in the Pamir Mountains through an agreement under which Tajikistan transferred about 1,000 square kilometres of mountain land to China. Tajikistan ratified the transfer in 2011.
- China and Pakistan agreed a boundary in 1963 that includes the Shaksgam Valley in the Karakoram. India, which claims the whole former princely state of Jammu and Kashmir, does not recognise this agreement.
Selected unsettled land borders worldwide
The following table lists some well-known land boundary disputes and undefined sections. It is not complete, and the status of several cases changes over time.
| Area | States involved | Nature of the problem |
|---|---|---|
| Southern Patagonian Ice Field (Fitz Roy–Murallón) | Chile, Argentina | Section left undefined by the 1998 agreement; delimitation pending |
| Kashmir | India, Pakistan, China | Disputed sovereignty; de facto Line of Control and Actual Ground Position Line |
| Aksai Chin and Arunachal Pradesh | India, China | Undelimited; Line of Actual Control not jointly defined |
| Essequibo | Venezuela, Guyana | Venezuela rejects an 1899 arbitral award; case before the International Court of Justice |
| Belizean territory | Guatemala, Belize | Guatemalan claim; referred to the International Court of Justice after referendums in both countries (2018 and 2019) |
| Halaib Triangle and Bir Tawil | Egypt, Sudan | Different colonial-era lines; Halaib claimed by both; Bir Tawil claimed by neither |
| Abyei | Sudan, South Sudan | Disputed area awaiting a final status decision |
| Ilemi Triangle | Kenya, South Sudan (historically also Ethiopia) | Overlapping colonial-era lines; administered by Kenya |
| Badme and other sectors | Eritrea, Ethiopia | 2002 boundary commission decision only partly implemented |
| Kalapani, Lipulekh and Limpiyadhura | Nepal, India | Competing interpretations of an 1816 treaty; Nepal issued a new official map in 2020 |
| Preah Vihear area and other sectors | Cambodia, Thailand | International Court of Justice rulings of 1962 and 2013 on the temple area; other sectors disputed, with armed clashes in 2025 |
| Western Sahara | Morocco, Sahrawi Arab Democratic Republic | Disputed sovereignty over the whole territory |
| Lake Constance | Germany, Switzerland, Austria | No agreed boundary in much of the lake; the states hold differing legal views |
Some long-running cases have been settled in recent years. Examples include Hans Island (Canada and Denmark, 2022), a series of agreements on the Russia–China boundary completed in the 2000s, and a border treaty between Kyrgyzstan and Tajikistan signed in March 2025 after years of clashes in the Fergana Valley region.
How borders are settled
States use several methods to settle unsettled or disputed borders. Often they combine more than one.
- Direct negotiation between governments, producing a treaty. Most boundaries in the world were settled this way.
- Joint boundary commissions, made up of surveyors and officials from both states, which turn treaty language into mapped and marked lines. The Chile–Argentina Mixed Boundary Commission and the US–Canada International Boundary Commission are examples.
- Arbitration, in which the parties agree in advance to accept the decision of an arbitrator or tribunal. The 1902 Andes award, the 1903 Alaska award and the 1994 Laguna del Desierto award all used this method.
- International courts, especially the International Court of Justice in The Hague, which has decided many land boundary cases.
- Freezing or setting aside claims, as under the Antarctic Treaty, where states agree not to press claims while cooperating in other ways.
Settlement on paper is not always the end of the process. Awards may be rejected or only partly implemented, as in the Eritrea–Ethiopia case. Demarcation may take decades after delimitation, and in icefield areas it may never be practical in the usual sense.
Mapping and technology
Satellite positioning systems such as GPS, together with satellite imagery and digital elevation models, now allow peaks, ridges and drainage divides to be located with high precision. This has removed many of the purely technical obstacles that left icefield boundaries undefined in the past. The 1:50,000 map required for the Chile–Argentina Section B, for example, could be produced with modern methods. The delay is generally attributed to political and procedural factors rather than technical ones.
Mapping itself can be a source of tension. Several countries have laws governing how national borders must be shown on maps published within their territory. Commercial online map services sometimes show disputed borders differently depending on the country from which the map is viewed. Ice-covered areas are especially prone to inconsistent depiction, because there is often nothing visible on the ground for mapmakers to follow.
Debates and open questions
- Fixed versus mobile boundaries. If a treaty follows a watershed on a glacier, it is debated whether the line should stay where it was surveyed or move as the ice melts. The Alpine "mobile border" agreements choose movement. Other states may prefer fixed coordinates for legal certainty.
- Surface versus bedrock divides. On icefields, the drainage divide on the ice surface may differ from the divide in the rock beneath. Treaties written before this was understood rarely specify which one is meant.
- Whether to finish undefined sections. Some observers argue that leaving the Patagonian section undefined avoids political conflict at little practical cost. Others argue that the gap creates uncertainty for national park management, tourism, scientific research and search-and-rescue operations.
- Legal significance of maps. Courts have sometimes given weight to maps that one party accepted for a long time without protest, as in the 1962 Preah Vihear judgment. This makes governments cautious about how their own agencies depict unsettled areas.
- Climate change and resources. As glaciers retreat, newly exposed land and meltwater may gain economic value, for example for water supply, hydropower or tourism. This could increase interest in areas that previously seemed unimportant.
See also
- List of territorial disputes
- Southern Patagonian Ice Field
- Argentina–Chile border
- Laguna del Desierto incident
- Alaska boundary dispute
- Canada–United States border
- International Boundary Commission
- Juneau Icefield
- Dixon Entrance
- Hans Island
- Siachen conflict
- Line of Actual Control
- Mont Blanc
- Antarctic Treaty System
- Territorial claims in Antarctica
- Uti possidetis juris
- Drainage divide
- Terra nullius
Sources
Questions people asked
Are there international borders that remain undefined or unsettled on icefields, such as between the US and Canada or Chile and Argentina?
For CL-AR: A ~50 km section on the Southern Patagonian Icefield (between Mount Fitz Roy and Cerro Murallón) has literally remained undefined. The 1998 treaty left that specific section unsettled to be mapped and demarcated by a joint boundary commission later, and they never finished it. Maps on both sides still show a dotted or disputed box there.
For US-CA: The land boundary in Southeast Alaska is legally settled by the 1903 arbitration tribunal, but up on the icefields and jagged nunataks it's mostly defined by straight lines connecting surveyed peak coordinates rather than physical border monuments on the ground. The only actual active dispute there is maritime (the Dixon Entrance).