Archeological in the context of "Archaeological excavation"

The Hattians (/ˈhætiənz/) were an ancient Bronze Age people that inhabited the land of Hatti, in central Anatolia (modern Turkey). They spoke a distinctive Hattian language, which was neither Semitic nor Indo-European. Hattians are attested by archeological records from the Early Bronze Age and by historical references in later Hittite and other sources. Their main centre was the city of Hattush. Faced with Hittite expansion (since c. 2000 BC), Hattians were gradually absorbed (by c. 1700 BC) into the new political and social order, imposed by the Hittites, who were one of the Indo-European-speaking Anatolian peoples. The Hittites kept the country name ("land of Hatti") unchanged, which also became the main designation for the Hittite state.

The religious beliefs and practices of Mycenaean Greece (c. 1600–1100 BC) are difficult to discern due to limited archeological, iconographical, and material records. Existing evidence suggests that the Mycenaean religion was the mother of the Greek religion, sharing many divinities later found in classical Greece (510–323 BC), including Zeus, Poseidon, and Dionysus. Several Mycenaean religious customs, such as animal sacrifices and votive offerings, survived into the Greek period, as did terms and concepts such as theos (deity), hieros (holy man), nawos (temple), and temenos (land cut off and assigned for communal purposes).

John Chadwick noted that at least six centuries lie between the earliest presence of Proto-Greek speakers in Hellas and the earliest inscriptions in the Mycenaean script known as Linear B, during which concepts and practices will have fused with indigenous pre-Greek beliefs, and—if cultural influences in material culture reflect influences in religious beliefs—with Minoan religion. As for these texts, the few lists of offerings that give names of gods as recipients of goods reveal little about religious practices, and there is no other surviving literature.

The Chillón River is a river located in western Peru. It originates in the glaciers of the Andes, and its mouth is located in the Pacific Ocean coast of the Callao Region. Its volume gets higher during the summer months (December to March). The river's valley is very fertile. It has been inhabited by varying indigenous cultures (including the Chancay culture) for more than ten thousand years, as shown by archeological evidence.

The Pan-American Highway follows the valley to the north of Lima, Peru's capital city.

Deogarh is a village in Lalitpur district of the Indian state of Uttar Pradesh. It is located on the right bank of Betwa River and to the west of Lalitpur hills. It is known for Gupta monuments and for many ancient monuments of Jain origins inside and outside the walls of the fort.

The fort on the hill is dominated by a cluster of Jain temples on its eastern part, the oldest of these dating to the 8th or 9th century. Apart from Jain temples, the wall frescoes of Jain images of "iconographic and the stylistic variety", are special features of the fort. The three ghats (ghat means "flight of stone steps leading to the river"), which provide approach to the Betwa river edge from the fort – the Nahar Ghat, the Rajghat and the ghat with the Siddh ki Ghufa (saints cave) – are also of archeological significance.

Palaeozoology or paleozoology (Greek: παλαιόν, palaeon "old" and ζῷον, zoon "animal") is the branch of paleontology and evolutionary biology that specifically deal with the study of prehistoric organisms from the kingdom Animalia and the recovery and identification of their fossil remains from geological (or even archeological) contexts. The field also extends to the use of these fossil records for reconstructive phylogeny (via comparative anatomy and phylogenetics) and paleoecology, i.e. the study of ancient natural environments and ecosystems.

While speculative fossils of earliest animals (in the form of primitive sponges such as Otavia) can trace back to the late Tonian period of the mid-Neoproterozoic era, definitive macroscopic metazoan remains are mainly found in the fossil record from the Ediacaran period onwards, although they do not become common until after the Cambrian Explosion, and vertebrate fossils do not become common until the Late Devonian period in the latter half of the Paleozoic era. Perhaps the best known macrofossils group is the dinosaurs. Other popularly known animal-derived macrofossils include trilobites, crustaceans, echinoderms, brachiopods, mollusks, bony fishes, sharks, Vertebrate teeth, and shells of numerous invertebrate groups. This is because hard organic parts, such as bones, teeth, and shells resist decay, and are the most commonly preserved and found animal fossils. Exclusively soft-bodied animals — such as jellyfish, flatworms, nematodes, and annelids — are consequently rarely fossilized, as these groups have few mineralized tissues that can survive geological processes, although trace fossils of their existence and activities can be preserved.