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Melka Kunture is a cluster of prehistoric sites located in the Ethiopian highlands, at 2000-2200 m above sea level, in the Upper Awash basin. The climate is rather cool (annual mean temperature 17°) and rainy. Palynological results prove that the original vegetation was of Afromontane type, i.e. distinct from the savanna one which develops at lower elevations. After 60 years of excavations at 20 sites and in 60 archaeological levels, the sequence includes the Oldowan, the Acheulean, the Middle Stone Age and the Late Stone Age. Hominin fossils were discovered in direct association with the lithic technocomplexes. Ichnological levels provide information on the life and behaviour of hominins and fauna which printed their tracks. Research on the hominin adaptation to the climate and environment of the highlands is relevant to understand how and when the earliest peopling of Europe happened., Melka Kunture es un clúster de yacimientos prehistóricos situados en el altiplano etíope, a 2.000-2.200 m sobre el nivel del mar, en la cuenca alta del río Awash. El clima es más bien fresco (temperatura media anual de 17° C) y lluvioso. Los resultados palinológicos demuestran que la vegetación durante el Pleistoceno era de tipo afromontano y, por lo tanto, diferente a la de sabana que se desarrolla en cotas más bajas. Tras casi 60 años de excavaciones en 20 yacimientos y en unos 60 niveles arqueológicos distintos, la secuencia arqueológica identificada incluye el Olduvayense, Achelense, Middle Stone Age y Late Stone Age. También se han descubierto fósiles de homininos en asociación directa con industrias líticas de diferentes tecnocomplejos. Además, se conocen niveles icnológicos, que proporcionan información sobre la vida y el comportamiento de homininos y fauna. La investigación sobre la adaptación de los homininos al clima y al entorno de las tierras altas es relevante para entender cómo y cuándo se produjo el primer poblamiento de Europa.

[EN] The Castle of Marmilla, located near the village of Las Plassas (central-Sardinia), represented a strategic military stronghold of great importance in the war between the kingdom of Arborea and the Aragonese Kingdom of Sardinia in the fourteenth century. Archaeological documents highlight the use, albeit partial, of some environments even in the modern age, during the times of feudal Sardinia (XV-XVI century), when the castle was an integral part of the possessions of the Barony of Las Plassas. It was used as a district prison until the nineteenth century. Built on top of a conical hill at 270 meters above sea level the castle has an irregular hexagonal shape, elongated along the north-west and south-east. Its foundations are excavated in a layer of Miocene sandstones and currently occupy the entire hilltop. What remains of the castle of Marmilla denotes a series of construction phases. A wide circle of walls delimiting the fortification of 550 square meters: inside there are the remains of a cistern and two towers, to the N and S sides, near the entrance. At present, the main tower and the walls, perimeter and internal, are preserved, albeit affected by a profound degradation, and they allow us to observe the construction techniques and choices made in the ongoing renovations, restorations and strengthening interventions. The structure is made of cantons sandstone cut with precision; at the base of the north tower was used ashlar stones. The cistern, located below ground level, is carved into the rock and covered with sandstone cantons; a second tank is located outside the masonry, near the northern side of the fortification. By minero-petrographic and physical-mechanical analysis of geomaterials (i.e., stones, mortars) used in the castle construction, the alteration degree of the materials, in order to identify a correct restoration for conservation purposes, has been defined.