Tag: Archaeology

  • How Do We Measure the Age of Things on Earth?

    How Do We Measure the Age of Things on Earth?

    From where did we come, and how did we evolve? A variety of scientific fields are interested in these issues, and they have no way to find answers without reliable dating methods. This is why scientists use a wide range of geological and archaeological “clocks” to date objects. The adjectives “old” and “young” in Earth’s historical context refer to periods of thousands to millions of years rather than the average human lifespan. Geochronology, the study of the absolute ages of geological and archaeological objects such as rocks, minerals, wood, and human remains, has developed various techniques for that. It has greatly influenced our contemporary worldview by revolutionizing our knowledge of Earth’s past.

    Radiocarbon dating method

    Radiocarbon dating method

    The so-called radiocarbon method, sometimes termed C14 carbon dating, is perhaps the most well-known technique for estimating age. Because carbon has three naturally occurring isotopes (C12, C13, and C14). There is just one carbon nucleus (C14) with 14 nucleons (6 protons and 8 neutrons) for every trillion of the stable C12 with 12 nucleons in the nucleus. The decay of the C14 isotope to nitrogen has a half-life of approximately 5,730 years.

    The lower the amount of C14 isotope, the older the object.

    All living things maintain a consistent C12:C14 ratio because they continually breathe in newly generated C14 from the environment. But C14 is not replenished if the animal or plant dies. Since the ratio of the two carbon isotopes in its tissues gradually becomes more favorable to C12 over time, this process provides the foundation for the radiocarbon clock. Wood, fossilized plant material, and bone can all be dated by analyzing their isotope ratios to determine how long they have been out of contact with C14. Similar techniques can be used to date other carbon-based substances.

    A historical glance

    The C14 clock’s main benefit is that compounds containing carbon are prevalent in both living and nonliving materials. C14 dating can be used in archaeology and paleontology to determine dates ranging from 300 to 60,000 years. But carbon mostly only exists in organic material.

    It was in 1934 that Franz Kurie first proposed the possible existence of carbon-14. In 1940, at the University of California Radiation Laboratory, Martin Kamen and Sam Ruben made the discovery of carbon-14. In 1946, Willard Libby developed radiocarbon dating based on carbon-14 to determine the age of artifacts, rocks, and even water.

    There were only a few institutions in the 1950s and 1960s responsible for the development of the C14 detection technique, which employed counting tubes to measure the decay of the carbon isotope and made it available for use in archaeology for the purpose of dating. This was the first time that archaeologists had used a scientific technique of dating.

    Radiocarbon dating has allowed for a comprehensive study of the last 50,000 years of human history, shedding light on questions such as when Neanderthals went extinct in Europe and how the ancestors of modern humans spread in terms of their physical characteristics. However, this method of dating has also illuminated the end of the last ice age and the beginning of the present warm period, the change from nomadic to settled agriculture, and the first use of metals.

    Eruption of a volcano

    C14 dating has become standard practice in the field of archaeology. One of the many unexpected findings made possible by the C14 approach is the recalculation of the timing of a Late Bronze Age volcanic eruption on Santorini, which happened in the Aegean. Based on a combination of dynastic chronicle research and astronomical evidence, Egypt’s historical chronology places the eruption of the volcano in 1520 BC. Objects that survived the volcanic eruption and were buried in ash and rocks were analyzed using the C14 technique, which led researchers to infer that the eruption happened one hundred years earlier than previously thought.

    Groundwater radiocarbon dating is another use of the C14 method. Using it, researchers can distinguish between glacial reserves and recently developed bodies of water in North Africa, where people rely on underground water supplies for drinking and other uses. Everyday applications of the C14 approach include verifying the authenticity of artifacts, determining the age of wines and spirits, and finding synthetic ingredients in purportedly organic items.

    Zircon dating method

    Zircon dating method
    Credit: Queensland University of Technology

    When did the Earth form? Because it only accounts for events that occurred during the last few thousand years on Earth, the radiocarbon approach is insufficient to provide an answer. But then, how can you put a time stamp on something as basic as Earth’s creation? Amazingly, geoscientists have realized that looking at the microcosm and focusing on the microminerals inside rocks is the greatest way to get an answer to this issue. From this investigation, a picture can be constructed of the progression and chronology of Earth’s history on a global and continental scale.

    Zircon, known as the “star mineral” for its importance in reconstructing Earth’s past, is one of these little time capsules. The zirconium, silicon, and oxygen compound (zirconium silicate (ZrSiO4)) existed for nearly 4.4 billion years, making it the oldest mineral on Earth. Zircon can be found in abundance in the Earth’s crust. Typically measuring between 0.05 and 0.3 microns in size, it is found as minute grains in the rocks.

    Uranium atoms encased in a crystalline structure

    The presence of uranium in zircon’s crystal structure is an attractive trait for dating purposes. Since uranium decays into lead over time, scientists can use the decay rate to determine the age of an object by measuring the uranium/lead ratio. Uranium decay products are trapped in the crystal lattice of surrounding zircon to varying degrees depending on when the zircon formed.

    Zircon can be used as a “clock” that can measure up to 4.4 billion years into the past, making it more accurate than the radiocarbon approach. Consequently, this technique works very well for dating rocks. Due to the very lengthy half-lives of uranium’s decay to lead, it cannot be used for this purpose over timescales of less than around 1 million years.

    Zircon aids in the study of continental prehistory

    How the continents were first created and how they eventually developed is a fundamental subject for Earth historians. In modern times, we have learned that the continents on Earth’s surface move gently in a back-and-forth motion. They could run against one another or shatter into pieces. However, the age of the various parts of the continents varies widely. Each continent is really made up of several other, smaller continents called “terranes” that range in age from very young to very old. There is a unique signature of time for each terrane. But how can we figure out the age distribution of each one?

    Gondwana and Pangea

    In order to address this issue, geoscientists analyze zircon for the uranium and lead isotopes it contains. This technique of dating has been utilized to investigate several aspects of crustal rocks. Crusts have a complicated history. 550–500 million years ago, it started on the northern margin of Gondwana, a prehistoric continent in the southern hemisphere. A number of massive chunks separated off the primitive continent’s northern border. They moved up north as separate continents, eventually forming a complex mosaic.

    About 350–330 million years ago, the core region of the newly developing primeval continent Pangea was where the jigsaw pieces were ultimately fused together. However, 120 million years ago, Pangea, the supercontinent, started to split apart into different continents. The Atlantic Ocean opened, Africa was divided from South America, and North America and Europe were separated from one another.

    The zircon data show, for instance, that the European crust is made up of smaller continents that were still linked to modern-day North Africa 500 million years ago. Central Europe thus sits on a piece of the Earth’s crust that was once part of Africa many eons ago. For the record, Canada is home to the world’s oldest continental crust. Age estimates put it at upwards of 4 billion years. When compared, Europe is a very young continent.

    Uranium dating method

    How do we measure the age of things. Etched fission tracks in an apatite. Uranium dating method.
    Etched fission tracks in an apatite. (Credit: Researchgate.net)

    When it comes to dating the rock, the potential mechanisms of uranium in minerals are considerable as well. In addition to dating the rock, they also show how its temperature has evolved through time. You can use this to figure out when lava solidified or how slowly a rock cooled.

    Everything functions on a very basic principle: Fission marks are tiny destructions caused by fission products blasted into the mineral lattice when a uranium nucleus contained inside the material decays. These fission markings, which appear as thin lines and notches if the mineral grain is polished, prepared in a certain manner, and seen under a microscope, are readily apparent. Since the rate of uranium decay is well established, scientists can determine the age of a mineral by counting the number of fission traces inside it. The greater the number of traces, the longer the material was exposed to radiation, and hence, the greater the amount of damage it suffered.

    Intense heat causes a time reset

    But there’s more to think about: These fission marks can only occur if the mineral isn’t overheated. Fission markings in the lattice of apatite, for instance, shorten if the temperature is over 60 degrees Celsius. Above 110 degrees, the crystal lattice heals, and the atoms that were displaced by the fission products return to their original lattice positions, leaving no evidence behind. The timer on the fission track has been turned back to zero.

    The “clock,” which is dependent on the temperature of the rock, aids geologists in several ways: Fission traces cannot occur in the rock at these depths because the rock is too hot. If it is then hauled upward by plate tectonics, these traces will become visible. Geoscientists may calculate the time it took for a layer of rock to ascend from the depths of the Earth’s crust to the summit of a mountain range based on its present height, the known decay rate of uranium, and the quantity of fission traces it contains. For instance, scientists have calculated that the Val Bregaglia in Switzerland, is rising at a pace of 0.3 mm each year.

    Ancient glass and erupting volcanoes

    This approach can also be used in dating rocks: Lava often hardens within a short period of time after a volcanic explosion. Thus, the age of a volcanic mountain can be determined from the last eruption or formation of the corresponding volcanic rock by analyzing the fission residues in its minerals. This method can be used to date man-made objects as well. Glass was often dyed yellow using a uranium oxide compound from Roman times until well into the 19th century in Europe, North America, and China. Fission markings indicate the time the glass solidified, and can be used to date objects made of glass, such as drinking glasses or figurines.

    Potassium-argon dating

    Radioactive decay of Potassium-40.
    Radioactive decay of Potassium-40. (Credit: UC.edu)

    Also known as K–Ar dating, the potassium-argon dating is a technique for establishing the age of rocks by analyzing the abundances of radioactive argon and potassium inside them. Radioactive potassium-40 decays to argon-40 in minerals and rocks, providing the basis for this dating technique.

    But there is a similar decay process for potassium-40, which results in calcium-40. So, the age of a mineral or rock can be calculated from the proportion of these radioactive isotopes.

    However, the widespread availability of nonradiogenic calcium in minerals and rocks makes the calcium-potassium age technique seldom used. The escape of argon to the atmosphere during volcanism, on the other hand, results in a relatively low argon abundance on Earth.

    However, although radiocarbon dating can only identify an age up to around 60,000 years, potassium-argon dating can go back as far as about 100,000 years. As a result, a void between 60,000 and 100,000 years has been found, which must be bridged using other dating methods. Thermoluminescence dating covers this by going from 40,000 to 200,000 years ago.

    Nature as a dating method

    In addition to radiometric dating, geochronologists may use a variety of different techniques to determine when an object was formed. The foundation for this comes from the fact that many natural materials, like wood or sediments, document and archive temporal events and changes across time. The only thing we need to do is figure out how to read and accurately interpret nature’s time records.

    Annual rings in wood and sediment

    The seasons have an impact on the emergence of new geological structures or the deposition of new materials. For instance, during tree development, one can count the rings in the wood and, under ideal circumstances, estimate the tree’s age to within a year. Dendrochronology, the study of tree rings, has allowed researchers to construct chronologies for continents that go back some 14,000 years. Tree-ring dating, like carbon-14 dating, is an important tool in archaeology for establishing the age of structures like fortifications and habitations.

    However, Varve chronology, also known as soil dating, examines the layers of sediments to determine when they were deposited. Lake sediment, like tree rings, is produced in seasonal cycles, with summer producing a slightly different composition and, generally, a different colored layer than winter. Therefore, the age of a sediment layer can be determined, as can the biological and climatic conditions that existed during a certain time period, by analyzing the sequence and thickness of these layers.

    Depending on the specific circumstances, this method may provide an age estimate of between 40,000 and 70,000 years. The effects of historical climate change are typically inferred through varves.

    Thermoluminescence dating

    Room Temperature thermoluminescence. Thermoluminescence dating.
    Room Temperature thermoluminescence

    The term “thermoluminescence” is a combination of two ancient Greek and Latin words meaning thermos “hot” and lumen “light”. The term means “light from heat”.

    Natural radioactive elements found in rocks and ceramics are used in various techniques to determine the age of rocks. Quartz and feldspar, for example, have electrons that get essentially imprisoned at particular disruptions in the crystal lattice due to the radiation released by these materials.

    Electrons are affected by these disturbances in the same way that spheres are affected by depressions on a surface; they may roll into them but cannot roll out on their own. Therefore, the radioactive decay energy is still present in the materials. Light or heat releases the trapped electrons, which then rearrange themselves and release any extra energy as luminescence.

    How much energy the radioactive inclusions have stored in the material can be deduced from how bright the luminescence radiation is. In this way, it can be used to date items to at least 100,000 years ago. Thermoluminescence and optically stimulated luminescence are two terms used to describe these techniques for determining the age of the rocks.

    Thermoluminescence dating is advantageous because it can be used to date objects anywhere from 40,000 to 200,000 years ago, a time range that falls in between those of radiocarbon and potassium-argon dating.

  • Archaeometry: History as Shown Through Artifacts

    Archaeometry: History as Shown Through Artifacts

    Archaeometry is used to determine the nature, provenance, and function of archaeological artifacts, whether they be Stone Age artifacts, Roman frescoes, or puzzling remains in archaic containers. The scientific analysis of these artifacts yields frequently important new information about ancient societies and technologies.

    High-tech examinations of artifacts are progressively providing vital insights into their origin, age, and manufacturing methods and roles, making them indispensable tools for the interpretation and analysis of archaeological findings. Archaeometry is a crucial link connecting the social sciences and natural sciences within archaeology. So, what exactly does archaeometry accomplish? If so, how and where does it put such techniques to use? The work of these specialists is elucidated via the use of examples from the geomaterial sciences.

    What Is Archaeometry?

    The lekythos, a Greek vessel dating back about 2,500 years, was examined using X-ray diffraction. Archaeometry
    The lekythos, a Greek vessel dating back about 2,500 years, was examined using X-ray diffraction. (Credit: Researchgate.net)

    The investigation of artifacts and locations from the past using scientific methods is what’s known as archaeometry, or archaeological science. It has anything to do with archaeological methods.

    Rocks, valuable and decorative stones, building stones, binders and pigments, ceramics and glass, ores and metals—in theory, geoscientific or material-scientific archaeometry deals with (nearly) everything that is also material for inquiry in the geosciences, including applied mineralogy and crystallography.

    Biomineralization like bones, shells, corals, or organic compounds like amber might be added to the list at will. The so-called soil archive may also be considered a component of it, depending on the context, although this topic is currently predominantly addressed by geoarchaeology, which has emerged in recent years as a distinct discipline in several nations.

    Perspective on How Things Were Done in the Past

    There is a wide range of resources that may be cultivated by archaeometry. Materials that were created, used, and molded by humans and are therefore a representation of the deeds of our forefathers may be included as well as geological substances. The range of questions we pose to the material in the studies is distinct from those of our conventional geoscientific parent fields. Mineral pigments and rocks, for example, are examples of naturally occurring materials that have not been altered and still contain information that can be used in archaeology.

    Particularly in pre-literate societies, one must rely on cultural legacies to learn about the past in ways that a cultural science approach to archaeology cannot. For instance, we can learn about ancient trade routes, knowledge transfer, and socially formative contacts between different cultures if we can identify raw material resources and experimentally reconstruct production processes, some of which are unknown.

    In archaeometry, what constitutes “classical fieldwork” in geosciences entails the use of data gleaned from excavations and other fieldwork. However, at the outset of archaeometric investigations, the primary challenge is typically to identify the material. Objects that have been buried for thousands of years and subjected to the corrosive conditions of the soil environment fall into this category.

    A picture of a cross-section of a pottery from a chalcolithic-age furnace Archaeometry
    A picture of a cross-section of a pottery from a chalcolithic-age furnace, captured using backscatter electron (BSE) microscopy. The brightest spots are where the most dense substances are packed in (here copper). (Credit: Prof. Aaron Shugar, Buffalo State College SUNY)

    Archaeometry and Archaeology

    Today, archaeology projects almost never succeed without some sort of scientific input, and this goes well beyond the purview of the so-called “auxiliary science” that has traditionally been used in the field. Thus, archaeometry is no longer confined to the lab, where samples are politely handed over in plastic bags and where data tables are forgotten in the back of hefty excavation reports.

    Archaeometry experts often submit applications for or initiate large collaborative projects on their own, and their research interests are highly individualized, though they frequently pertain to issues of materials in the history of technology. Concerns of value and quality, human-environment linkages, and many others are included in the portfolio alongside questions about cultural interchange and information transmission.

    This makes it abundantly clear that we are interdisciplinary thinkers who move fluidly between the cultural and natural sciences, leaning more toward one or the other depending on our individual interests and institutional ties.

    How Does Archaeometry Work?

    Research data collected using archaeometric methods appear, at first glance, to be identical to their mineralogical-geoscientific analogs. What is measured and indicated after the fact is not drastically different for a slab of limestone used in a Roman wall decoration and one freshly extracted from a sedimentary rock sequence. In the case of archaeological artifacts, however, additional details must be provided to ensure the long-term viability of the data.

    Making the Most of Limited Resources

    Furthermore, archaeology often has a clear perspective on the objects it studies. If possible, data extraction shouldn’t involve sampling at all, and if it does, it should be done with extreme caution. This means that archaeometric analyses frequently need to squeeze as much information as possible out of small samples.

    What kind of sample size is required for even minimal confidence in conclusions? That really depends on the nature of the material being analyzed, particularly its microstructure and overall composition. Although spatially resolved methods like microprobe analysis or micro-X-ray fluorescence analysis may only need a few fragments of Roman glass to obtain a proper elemental analysis, an ancient Egyptian bust carved from coarse-grained stone would not benefit from such a tiny sample size.

    That’s why it’s crucial to have a good consultation. Archaeometry experts and their human counterparts should work together to collect samples or decide which parts of a larger object can be dissected and analyzed.

    Multiple Approaches to Analysis

    The composition of the picture may be deduced from an X-ray examination. Archaeometry
    The composition of the picture may be deduced from an X-ray examination. (Credit: Heritage Science)

    Once the sample is prepared for analysis, the material science techniques of archaeometry are very similar to those typically used in the analysis of geomaterials or chemicals. Methods such as polarization or scanning electron microscopy, X-ray fluorescence analysis in all its forms, microprobe analysis, and mass spectrometry are all examples of standard techniques. Additionally, cutting-edge X-ray analysis techniques and neutron activation analyses are employed to answer specialized inquiries.

    Non-destructive or minimally invasive techniques are typically required for examination, depending on the nature of the substance being studied. When there isn’t enough of a sample to do a standard X-ray diffraction examination, for instance, spectroscopic techniques like infrared or Raman microscopy are commonly employed to identify pigments and binders.

    Organic Materials and Mobile Techniques

    Now more than ever, archaeometric studies are concentrating on organic materials. There is typically a lengthy history of usage behind a ceramic, and in the pore patterns and fissures of the ceramic matrix are often kept material residues of foodstuffs or their breakdown products. Such chemicals and biological components may be identified using gas or liquid chromatography, as well as proteomics techniques.

    The advent of portable chemical analysis tools is a huge advantage for archaeological digs and the investigation of museum artifacts that are either too fragile to leave their secure environments or are situated in another country. The usage and improvement of mobile sampling techniques, such as laser ablation for later laboratory mass spectrometry, are also on the rise and becoming more effective.

    Substances Show Usage

    Archaeometry seeks, in part, to answer questions about the purpose of artifacts by examining their composition and construction methods. This may be useful for determining what kind of product was stored in a certain container in the past.

    Small ceramic vials up to around ten centimeters in size have been discovered among the artifacts of several tribes that lived throughout the Late Neolithic and Iron Ages. This kind of small vessel dates back to the 5th millennium BC and has been discovered throughout the Balkans, as well as in the southeastern Prealps (France) and southern Transdanubia (Hungary).

    But what were these ancient vials even used for? Even in the case of perfectly preserved ceramic vials, the original contents and, by extension, the function are still unknown. Because of the soil’s lengthy storage time, adhesions may include subsequent forms as well as remnants of the original contents. Because of their size and elaborate ornamentation, it is believed that these artifacts formerly contained expensive cosmetic or medicinal substances, maybe for cultic reasons.

    Here’s where archaeometry comes in: it takes not only chemical but also structural and material science analytical techniques – preferably non-destructive or at least minimally intrusive – to get close to the absolutely unknown nature of the leftovers in the vial.

    Researchers use analytical techniques from organic chemistry like gas chromatography (GC) and mass spectrometry (MS), as well as techniques like electron microscopy and X-ray fluorescence analysis.

    Anywhere From Crucibles to Makeup Jars

    Different applications are being discovered for these ceramic vials in the present day. Lead-containing slag deposits, for instance, were identified in 2019, suggesting that they served as small crucibles for lead ore. Multiple types of lead were found on content residues in a subsequent study of a similar set of items from the same location and time period.

    Cerussite (PbCO3), an inorganic component, was detected in the still-preserved contents of another vial in 2021 using spatially resolved X-ray analysis and gas chromatography-mass spectrometry, along with beeswax and probably other organic components such as vegetable oils or animal fats. Whether or not the antibacterial activity of lead-containing chemicals was understood for medicinal uses, and whether or not the ingredients served aesthetic reasons, is unknown.

    Finding Out the Origin and Age

    Clarifying a find’s provenance or production history is another major use of archaeometry. This is because, with the right kind of analysis, it is sometimes possible to recreate the material’s composition and the signs of different processing processes even after thousands of years have passed.

    Basalt Rocks

    While basalt was used for many things in the past, its most notable usage was as a grinding stone, which was crucial to the preparation of many dishes. Because of its porosity structure and fine-grained mineralogical phase composition, it is ideal for grinding. Due to its often quite sharp-edged macro- and micropores, basalt maintains its grinding ability over extended periods of time.

    In addition, the grain ground with basalt rock causes significantly less damage to teeth when consumed as bread or porridge due to the absence of quartz and low abrasion. Because of these qualities, millstones and grindstones fashioned from basalt were highly sought after and regularly traded across great distances and time periods.

    Therefore, suitable basalt deposits were a resource in high demand across the region. Archaeometric-geoscientific approaches are necessary for tracing these paths and the consequent cultural connections since they provide a characterization of raw material and end product, allowing for a provenance study.

    For example, during the Roman era, the basalt quarries in Mayen, Eifel Mountains in Germany, were a major producer of millstones. A large number of basaltic millstones discovered on excavations in many European countries were assumed to have originated in the Eifel based on macroscopic similarities.

    Actually, this was demonstrated by scientists using cluster and discriminant analyses. There are even instances where they were able to attribute millstone basalt to specific lava flows.

    Carolingian Chalice

    The Tassilo Chalice, dating from the 8th century AD. Archaeometry
    The Tassilo Chalice, dating from the 8th century AD.

    It is possible to learn even more about the inner workings and background of an artifact by combining the results of a chemical analysis with a microscopic examination of its structure. The Tassilo Chalice, for instance, has been protected for centuries thanks to the monks of the Kremsmünster Abbey in Austria. The Bavarian Duke Tassilo III, who passed away after the year 780, and his Lombard wife Liutperga are memorialized on this chalice alongside images of Christ and the Evangelists, among other figures.

    This copper goblet with silver studs is a masterpiece of Carolingian goldsmithing. Parts of the figural medallions could have been added or changed at a later date, although scholars were divided on the subject. This is a crucial point that needs answering, since it raises room for varying interpretations of the data.

    In this case, too, archaeometry was necessary. The silver overlay was revealed to be a mosaic of many tiny silver sections that had been mechanically applied, some of which were riveted on with pins. Recently repaired areas were identified by a combination of microscopic dissection of the sheets and their overlaps and detailed chemical mapping of the sheet metal sections and rivets with hundreds of analytical sites.

    Also, the analyses showed that the evangelist medallions on the chalice were all manufactured simultaneously. Despite being restored at a later time, the majority of the motifs and how they were implemented date back to the Carolingian era.

    History of Archaeometry

    To the best of our knowledge, the term “archaeometry” was first used in the early 1950s in Oxford. At the close of the 18th century, the chemistry pioneer Martin Heinrich Klaproth (1743–1817), who based his career in Berlin, first came to prominence in discussions about the scientific research of antiquities.

    Material interest in what has been handed down from the “ancients” rose in tandem with the 19th-century European fervor for antiquities and the establishment of organized archaeological collections in museums. The conservation and restoration of artifacts also played a crucial role in this context, since artifacts composed of non-ferrous metals and alloys, for example, were sometimes altered beyond recognition by thousands of years of ground storage. Here, one had to use scientific procedures to figure out what substance was in question.

    During the 19th century, scholars grew more interested in jewelry and valuable stones, such as those used for Roman finger rings or early medieval garment clasps. Specialized mineralogical expertise was sought to determine if glass or red minerals like zircon, ruby, spinel, or garnet were employed in the vast arrangement of burgundy clear discs.

    As early as 1890, Otto Tischler conducted scientific investigations on artifacts in what was then East Prussia, and he successfully identified the red platelets as garnet using physical and optical inspection techniques. Tischler was destined for this since he possessed a doctorate in prehistory and a degree in natural sciences and mathematics with a crystallographic-mineralogical emphasis. This makes him a prototypical archaeometric researcher—someone who studies two areas simultaneously.

    Modern archaeometry owes a great deal to a number of influential figures who were working in their area throughout the 19th century.

    Today, archaeometry is often studied as an elective for a bachelor’s degree and less rarely as a standalone master’s program. There is a high need for this since natural sciences are essential to almost all archaeological projects.

    References

    • Marcos Martinón-Torres and David Killick. “The Oxford Handbook of Archaeological Theory”. Oxford University Press
    • Killick, D; & Young, S. M. M. (1997). Archaeology and Archaeometry: From Casual Dating to a Meaningful Relationship? University of Arizona
    • Michael E. Smith, 2017. “Social science and archaeological enquiry”.
  • 3,500-Year-Old Hittite Graffiti With 250 Characters

    3,500-Year-Old Hittite Graffiti With 250 Characters

    Archaeologists excavating the remains of the Hittite city of Hattusa have uncovered graffiti dating back 3,500 years: red paint figures on the tunnel walls. To our knowledge, these roughly 250 characters are the only colored Anatolian hieroglyphs that have been discovered so far. The majority of Anatolian hieroglyphs discovered to date have been carved into rock or sculpted in relief. The discovery suggests that literacy in Hittite was not limited to the ruling class.

    It is generally agreed that the Hittites, behind Egypt and Assyria, were the third most powerful civilization in the Eastern Bronze Age.

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    Large portions of Asia Minor and the Near East were under their rule. Hittite Hattusa, which served as the capital from 1600 to 1200 B.C.E., was located about 93 miles (150 kilometers) east of Ankara, Turkey. In its prime, the city area was up to 445 acres (180 hectares), and it was surrounded by walls that stretched over 5.5 miles (9 kilometers). The city served as the seat of the great kings and had huge gates and temples.

    Found in the underground passageway

    Archeologists have previously seen inside a tunnel that led under a colossal fortress. The Yerkapi rampart was up to 130 feet (40 meters) high and over 820 feet (250 meters) long, and it was shaped almost like a pyramid. At the very top of the ramparts of Yerkapi stood a gate adorned with four sphinxes.

    3,500-Year-Old Hittite Graffiti With 250 Characters

    It has long been hypothesized by archaeologists that this impressive edifice was built not for defense but rather as part of a religious ceremony. In August 2022, an excavator was exploring the tunnel under the Yerkapi and saw some crimson markings on the tunnel’s only coarsely hewn walls. They were graffiti styles colored with a reddish-brown root paint on the walls.

    Walls covered with colored hieroglyphs

    This hieroglyph might represent Kurunta, the name of a Hittite deity.
    This hieroglyph might represent Kurunta, the name of a Hittite deity. (Image: German Archaeological Institute)

    The investigation of the 249 characters discovered in the Yerkapi tunnel confirmed that they are Bronze Age Anatolian hieroglyphs, a pictorial script more often seen on rock monuments or seals in the Hittite Empire. Unlike other known hieroglyphs, however, they are not carved into a rock or fashioned into a relief. On the other hand, the Yerkapi’s signs were not only carved into stone, they were also colored. Archaeologists say that just two sites in the former Hittite Empire have yielded any examples of such colored inscriptions.

    3,500-Year-Old Hittite Graffiti With 250 Characters

    The discoveries at Yerkapi show that the use of Anatolian hieroglyphic writing was far more pervasive in Hittite culture than was previously thought. Initial investigations reveal that the Yerkapi monument in Hattusa is covered with graffiti featuring at least eight distinct sets of repetitive characters. Many of the inscriptions have been well maintained and may be read with just a little effort, while a few have been degraded beyond readability.

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    The research indicates that many of the graffiti from the Bronze Age are names of persons or gods, while others serve as a kind of signal along the way.

    The discoveries provide light on the Late Bronze Age in a way that was not anticipated. Archaeologists have digitized the whole building, including the hieroglyphs, and created a three-dimensional model of it to record this rare find.