Distinguishing features between man made tools and naturally fragmented alleged tools

Size: px
Start display at page:

Download "Distinguishing features between man made tools and naturally fragmented alleged tools"

Transcription

1 Distinguishing features between man made tools and naturally fragmented alleged tools Introduction: There are certain degrees of differences between the man made tools what we frequently called artifacts and the naturally fragmented or made alleged tools. On the other hand there are also some naturally fragmented rocks which possess certain similar characters like those of the man made tools with some specific purposes. Such similar characters sometimes make confusion which mislead the archaeologists while identifying and classifying the Artifacts specimens. The archaeologists sorted out the basic attributes which are possessed by each man made or modified tool with a purpose and apply while identifying and classifying the tools. Hence archaeologists try to find out the sign of intentional knapping, because the purpose of intentional knapping is to make tools, in the broader sense of the term (as it will always leave similar scars on man Alleged tools made tools). The technological interpretation of any worked stone artifact will therefore be specific to that artifact, and based on the precise observation and recognition of those scars. A (man made) stone artifact can only be defined as such by removal scars, both positive and negative. Resulting from either the pressure flaking or percussion technique, such scars obey physical laws and are identical whether the knapping is intentional (man-made) or not (natural). The diagnosis of intentional knapping is best indicated when the artifacts are discovered in a well defined archaeological context. In the case of chance discoveries or surveys, the main criteria for recognizing intentional knapping is the organization of removals. Caution is required when flakes or even pebble tools are found on a beach, for they may well result from natural phenomena (so called naturally made alleged tools); to the contrary, the discovery of a single handaxe or a single Levallois core can prove intentional knapping (man-made): the organization of removals follows so specific a sequence that the 1

2 possibility of chance knapping due to random impacts can be dismissed. The number of pieces found and their geological position provide additional information concerning the context and further help to established the possible presence of a site. However one must bear in mind that it is not always easy to distinguish (man-made) intentional from naturally made (unintentional knapping), and the often arises as to whether the modifications reflect intent or accident. The present topic aims at discussing the points of difference between the man-made and naturally made or fragmented alleged tools. The concept of man made tools : Man first conceptualizes the would be shape, size, working edge and butt of the tool beforehand, and accordingly he selects the suitable raw material, then chose the flaking techniques to make it. Therefore, man made tools have generally a regular pattern. Regularly patterned tools are therefore considered as the signs of culture. Stone is the most imperishable of all the materials which were used by our prehistoric man for the manufacturing of his tools. He made stone tools by Bulb of percussion percussion flaking technique (striking a stone with another stone). There is evidence of gradual technological evolution in the man-made tools. The resultant character of the blow may be understood first, that a sharp blow directed vertically at a point on the surface of the block of rock, say flint, knocks out a solid cone called conchoidal fracture. However, when the blow is directed obliquely near the edge of a slab, a flake is detached with half of the cone of percussion. This halfformed cone of percussion at the point Conchoidal fracture of impact on the flake is called the positive bulb of percussion, and the corresponding hollowed flake scar on the parent lump or core is called the negative bulb of percussion. There are also Direction of the blow 2

3 low concentric ripples around the bulb of percussion corresponding to the force of the blow and the amount of the resistance in the block. This is, according to L.S.B. Leakey, because of the fact that the force from a blow does not travel in the direction of the blow but at an angle to it, and not in one straight line, but along a curve representing the ever-widening circles. He further stated that if the direction of the blow is at an angle to the surface of the flint only a small part of the cone affects the flint, and the rest is absorbed outside the flint. Manufacturing techniques of man-made tools : Researches on the techniques of making stone tools by prehistoric man have now established various ways of flaking. These can be grouped under three categories - (a) Direct percussion flaking, (b) Indirect percussion flaking and (c) Pressure flaking. In the direct percussion flaking, the hammer strikes directly on the surface of the block of stone for detaching a desired flake. The flakes detached by using different hammers will exhibit different characters. For example, the flake struck off the core by using large heavy hammer stone will exhibit very prominent bulb of percussion on the main flake surface, while light stone hammer produces flakes with small and flatter bulb of percussion. At times some of the massive flakes are also Prominent bulb of percussion used in making tools like cleavers and hand axes. This will be hard to believe in case of the nature. The prehistoric man in making the stone tools also employs step flaking and bi-polar techniques. These two techniques are the evidence of preconceived ideas of man for making the stone tools. The naturally fragmented alleged tools do not exhibit such preconceived ideas. Flakes produced by the levallois or discoid core technique will always have a regular pattern, and the levallois flakes could be used as tool without further modification. But nature cannot produce such flakes with regular patterns. Another convincing character of the man made tools is the presence of the alternate secondary flaking that nature cannot produce. The purpose of the alternate and secondary flaking is for 3

4 producing sharp working edge and blunt suitable handholding or hafting place. Pressure flaking is a highly specialized technique adopted by the prehistoric man in making tools like leaf-shaped points. This technique produces very thin flake scars resembling the fish scales arranging in a regular systematic pattern. However, such regular set of meaning full fish scale-like scars are not present on the naturally made alleged tools. Prehistoric man had also adopted the techniques of pecking, sawing, grinding and polishing in making Neolithic stone tools; and these techniques were applied purposefully. There is no evidence of such purposeful techniques in the naturally produced tools. Types of man made tools and naturally fragmented alleged tools : Man made tools are best represented by the types such as Chopper, Chopping tool, various types of Hand-axes and Cleavers, Pick, Handazes, Scraper, Point, Borer, Blade, Burins, Micro-blades, Denticulates, various types of celts, Ringstones or Mace-heads and naturally made alleged tools are called Eoliths. Even the oldest Hand-axes from the earliest Pleistocene deposits have standardized forms, whereas the eoliths though used as tools by the immediate forerunners of man lack such character. K.P.Oakley (1965) stated, The possibility of discovering evidence of man in the Pliocene was being considered towards the end of the last century, and in 1891 Prestwich published an account of some crudely shaped flints, looking like simple tools which had been found in patches of the Pre-glacial plateau drift on the North Downs of Kent by an amateur archaeologist, Benjamin Harrison, of Ightham. They came to be known as Eoliths, since it was suggested that they were the earliest recognizable implements, and represented the dawn of tool making. However, detailed studies have shown that all the Kent and Sussex Eoliths can be matched exactly by stones chipped by natural agencies. Thus, any among them which have been chipped by man would not be distinguishable from the probably far greater number which has been shaped through the accidents of nature. 4

5 Knapping Accident A knapping accident, which may occur during flaking, shaping or retouching, is an unforeseen and unintentional accident generating products with a specific morphology. Archaeologically observed and experimentally produced knapping accidents are identical, thus strengthening the credibility of the analogy-based experimental approach. They come as a certain number of types and are due either to flow flaws in the raw material (such as joints, vesicles, saccharoid, nodules etc.) or to some mismanagement on the knapper s part. Knapping accidents have varying repercussions on the continuation of the knapping sequence to which they belong. They can be irreversible (for instance, the fracture of a large leaf-shaped bifacial piece, pluging Levallois point etc.) put right (hinged blade removed from a core with two striking platforms : in the case, a single removal struck off from the opposite platform is sufficient for debitage to proceed unimpaired), or of no consequence (bulb scars, fracture of a burin spall when the later is a waste product, etc.) Although unintentionally obtained, the products resulting from knapping accidents can also be used as blanks. Knapping accidents can broadly be divided into four groups. They are : (1) Breaks, (2) Plunging flakes, (3) Hinged flakes, and (4) Miscellaneous. 1. Breaks : Breaks are accidental snapping of a flake upon removal, or of any artifact in the process of being knapped. The occurance of breaks is irrespective of technique employed (percussion, pressure etc.). The main type of breaks are : i) Clean breaks, ii) Siret accidental breaks, iii) Languatte breaks and iv) Nacelle breaks. i) Clean break : It is the type of the break whose surface is perpendicular to the dibitage axis and the lower face. ii) Siret accidental break : It refers to the snapping of a flake into two aligning the debitage axis. Such accidents were long mistaken for burins; they leave but a partial arris on the core (when it is at all visible), on the distal part of the removal negative. iii) Languette breaks : They usually occurs on the upper or lower face. They can be simple or double, in which (the latter case) they sometimes generate characteristic waste products. iv) Nacelle breaks : It is initiated by bulb scars which arch suddenly 5

6 towards the upper face, removing parts of the two edges, and then intersected suddenly at the lower face. The small waste product corresponding to the Nacelle has a very specific shape. Such incidents are very common when pressure rather than percussion is applied. 2. Pluging flakes : They result from phenomenon causing the fracture plane, whose proximal part is normal, to plunge suddenly away from the exterior surface and remove a whole section of the blank, be it a core, a debitage product or a tool. 3. Hinged flakes : They are the opposite of plunging flakes, although they probably share the same physical causes (variation in the propagation speed of the fracture front). A hinged flake is a removal whose fracture plane, normal in its proximal part, arches suddenly and intersects prematurely with the upper face of the blank, resulting in a rounded fistal end (hinge-fracture) or an abrupt clean break (stepfracture). The blank is therefore shorter than what was expected. Hinge pieces and their removal negatives are very prominient. It is the most common accident that befalls the beginners when they try their hand at knapping. 4. Miscellaneous : These includes incipient fractures, lipped flakes, parasitical flakes, and spontaneous removals. 6

7 Agencies for producing naturally made alleged tools : We need to know the various agencies in nature that cause flaking of stone to distinguish these characters from those of the man made tools. Flaking could also be done by the natural agencies. Thermal change termed as thermal fracture is one of the chief accidental agencies by which stones are flaked. K.P.Oakley (1965:9 10) stated that Rapid changes of temperature cause unequal expansion or contraction of the surface of the stone or rock relative to its interior. In Blade-core like fracture due to Thermal changes deserts, for example, the exposed surfaces of some types of rock are continually flaking as a result of the difference between the day and night temperature. In the cold regions, flakes are commonly split off by frost the outer layer of the stone expanding through the freezing of absorbed water. A flake or flake-scar due to frost or other thermal fracture is easily recognized for the surface of fracture has either a roughish, blank appearance, or shows ripples concentric about a central A residual frost-pitted lump point.. Flakes with round in outline are produced by the frost action, and the residual frost-pitted lump of appropriate shape is easily mistaken as implement. Thermal changes are sometimes cause flint to break into prisms resembling blade-cores; and stones 7

8 splintered by fire or facetted by sandstorms are occasionally mistaken as blades. However, in closure examination it could be noticed that such splintered blades break through the joint-plane or the strains setup by slow internal shrinkages. When heavy stones carried by the waves of sea or heavy torrential water or the glacier strike against the fixed stone in the beach or gravel bed the detached flakes will flatter and more diffused bulb of percussion will be formed. After Friction sometime the flaked stone is eroded and redeposited at another location, and again strikes by another heavy stone in the same process as above resulting to the detaching of another flake either unidirectionally or bidirectionally to the previous flake scar. Such repeated course of action may produce the stone resembling the shape of an implement. Since the flakings are not done simultaneously, the flake scars exhibit different rate of weathering or patination and are also not purposeful. Another evidence of man-made tool is the presence of purposeful secondary flakings. But thin pieces of stone can be chipped through friction against another stone as occurs in soil-creep (solifluxion), in torrent action, or in glacier. Such naturally chipped flakes lack logical design, the flakescars occur in uneconomical profusion, the edges have brushed appearance, and the flake-surfaces are usually scratched. 8

9 Difference between the man made and naturally flaked alleged tools : In short, there are many differences between the man made and naturally fragmented or made alleged tools. Six points of differences are discussed here. In the case of man made tools the cone of percussion is prominent. In contrast to it, the naturally made alleged tools, the cone of percussion is either flatten or almost absent. Similar, in the man made Point of impact tool the flaking ripples are concentrated to the point of impact whereas in the naturally flaked or made alleged tools the flaking ripples are concentrated around a central point. Regarding the primary and secondary flakings, these are purposefully present in case of man made tools but irregular and uneconomical in those naturally made alleged tools. In addition to these characters, alternate flaking is present in the case of man made tools but absent in the case of naturally made alleged tools. Moreover, the patination of the flaking scars are uniform in the case of man made tools but different patinations are found in Naturally chipped flake the naturally made alleged tools. Above all, there is a regular set pattern in the case of man made tools but it is irregular in the naturally made alleged tools. Thus, we may summarise the differences between the man made tools and naturally made alleged tools in a tabular form as below: 9

Archaeologia Cantiana Vol

Archaeologia Cantiana Vol Archaeologia Cantiana Vol. 65 1952 SURFACE PAL^OLITHS FROM STANDARDHILL FARM, NEAR ELHAM By P. J. TESTER THE seven Palaeolithic implements shown in the accompanying illustrations were collected by the

More information

The Upper Palaeolithic of North China Chaisi Locality 7701

The Upper Palaeolithic of North China Chaisi Locality 7701 The Upper Palaeolithic of North China Chaisi Locality 7701 Tang Chung Centre for Chinese Archaeology and Art The Chinese University of Hong Kong 1 LOCATION The site of Chaisi is located at the bank of

More information

What are the different ways rocks can be weathered?

What are the different ways rocks can be weathered? Romano - 223 What are the different ways rocks can be weathered? Weathering - the breakdown of rocks and minerals at the Earth s surface 1. 2. PHYSICAL WEATHERING Rock is broken into smaller pieces with

More information

Comparing Bipolar Artefacts with Pseudo-Artefacts and Industrial Waste An overview based on experimentation

Comparing Bipolar Artefacts with Pseudo-Artefacts and Industrial Waste An overview based on experimentation Comparing Notae Praehistoricae, Bipolar Artifacts 30-2010 with : 95-100 Pseudo-Artifacts and Industrial Waste 95 Comparing Bipolar Artefacts with Pseudo-Artefacts and Industrial Waste An overview based

More information

Lithic artefacts, miscellaneous collections from outside the main sequence: Phases T-1, 9, 9-10 and 11

Lithic artefacts, miscellaneous collections from outside the main sequence: Phases T-1, 9, 9-10 and 11 439 Chapter 21 Lithic artefacts, miscellaneous collections from outside the main sequence: Phases T-1, 9, 9-10 and 11 by Francis Wenban-Smith INTRODUCTION The lithic remains presented in this chapter represent

More information

The Upper Paleolithic Longwangcan Site at Yichuan in Shaanxi

The Upper Paleolithic Longwangcan Site at Yichuan in Shaanxi The Upper Paleolithic Longwangcan Site at Yichuan in Shaanxi The Institute of Archaeology, Chinese Academy of Social Sciences Shaanxi Provincial Institute of Archaeology Key words: Longwangcan site; microliths;

More information

Deposited on: 15 October 2014 NMS Repository Research publications by staff of the National Museums Scotland

Deposited on: 15 October 2014 NMS Repository Research publications by staff of the National Museums Scotland Saville, Alan and Ballin, Torben Bjarke. (2009) Upper Palaeolithic evidence from Kilmelfort Cave, Argyll: a re-evaluation of the lithic assemblage. Proceedings of the Society of Antiquaries of Scotland,

More information

CHAPTER FIVE THE LITHIC ASSEMBLAGES

CHAPTER FIVE THE LITHIC ASSEMBLAGES CHAPTER FIVE THE LITHIC ASSEMBLAGES The lithic assemblages of Tshisiku Shelter, Balerno Main Shelter and Balerno Shelter 2 provide most of the data for this study of hunter-gatherers and interaction since

More information

Cover Page. The handle holds various files of this Leiden University dissertation.

Cover Page. The handle   holds various files of this Leiden University dissertation. Cover Page The handle http://hdl.handle.net/1887/19054 holds various files of this Leiden University dissertation. Author: Zwyns, Nicolas Title: Laminar technology and the onset of the Upper Paleolithic

More information

Archaeologia Cantiana Vol

Archaeologia Cantiana Vol Archaeologia Cantiana Vol. 63 1950 PALAEOLITHIC FLINT IMPLEMENTS FROM THE BOWMAN'S LODGE GRAVEL PIT, DARTFORD HEATH By P. J. TESTER THE Bowman's Lodge pit is the most recent of several extensive excavations

More information

GLENTAGGART, SOUTH LANARKSHIRE DISCUSSION OF A SCOTTISH CHERT ASSEMBLAGE AND ITS ASSOCIATED TECHNOLOGY

GLENTAGGART, SOUTH LANARKSHIRE DISCUSSION OF A SCOTTISH CHERT ASSEMBLAGE AND ITS ASSOCIATED TECHNOLOGY GLENTAGGART, SOUTH LANARKSHIRE DISCUSSION OF A SCOTTISH CHERT ASSEMBLAGE AND ITS ASSOCIATED TECHNOLOGY T.B. Ballin 4 and M. Johnson 5 ABSTRACT In 2001, CFA Archaeology Ltd. recovered a substantial chert

More information

COLLECTION OF STONE ARTEFACTS FROM THE MOO FOOT TERRACE1 AT ABBOTS LEIGH, AVON

COLLECTION OF STONE ARTEFACTS FROM THE MOO FOOT TERRACE1 AT ABBOTS LEIGH, AVON Proc. Univ. Bristol Spflfawol. Sue.. 1991, 19 (I), 33-41 PRELIMINARY REPORT ON A RECENT COLLECTION OF STONE ARTEFACTS FROM THE MOO FOOT TERRACE1 AT ABBOTS LEIGH, AVON by B. HACK and A.P. CORNISH ABSTRACT

More information

Weathering, Erosion, Deposition, and Landscape Development

Weathering, Erosion, Deposition, and Landscape Development Weathering, Erosion, Deposition, and Landscape Development I. Weathering - the breakdown of rocks into smaller particles, also called sediments, by natural processes. Weathering is further divided into

More information

Chipped Stone Tool Use in the Maya Coastal Economies of Marco Gonzalez and San Pedro, Ambergris Caye, Belize

Chipped Stone Tool Use in the Maya Coastal Economies of Marco Gonzalez and San Pedro, Ambergris Caye, Belize 3 AQ < Qe Chipped Stone Tool Use in the Maya Coastal Economies of Marco Gonzalez and San Pedro, Ambergris Caye, Belize William James Stemp BAR International Series 935 2001 TABLE OF CONTENTS CHAPTER 1

More information

MORE STONE TOOLS FROM RAINBOW BAR, HILLHEAD

MORE STONE TOOLS FROM RAINBOW BAR, HILLHEAD Proc. Hampshire Field ClubArchaeol. Soc. 54,1999,163-171 (Hampshire Studies 1999) MORE STONE TOOLS FROM RAINBOW BAR, HILLHEAD By BRIAN HACK ABSTRACT Repeated searching of the beaches and other gravel spits

More information

Sediment and Sedimentary rock

Sediment and Sedimentary rock Sediment and Sedimentary rock Sediment: An accumulation of loose mineral grains, such as boulders, pebbles, sand, silt or mud, which are not cemented together. Mechanical and chemical weathering produces

More information

Pratice Surface Processes Test

Pratice Surface Processes Test 1. The cross section below shows the movement of wind-driven sand particles that strike a partly exposed basalt cobble located at the surface of a windy desert. Which cross section best represents the

More information

Erosion and Deposition

Erosion and Deposition Erosion and Deposition The Erosion-Deposition Process What do you think? Read the two statements below and decide whether you agree or disagree with them. Place an A in the Before column if you agree with

More information

Weathering, Mass Wasting and Karst

Weathering, Mass Wasting and Karst Weathering, Mass Wasting and Karst Capable of wearing down anything that the internal processes can build. Gravity, water, wind and ice Denudation - the overall effect of disintegration, wearing away and

More information

Archaeopress Open Access

Archaeopress Open Access Proceedings of the Seminar for Arabian Studies 45 (2015): 329 336 Found: the Palaeolithic of Qatar (poster) Summary The seeming lack of evidence for a Palaeolithic presence in Qatar has been enigmatic.

More information

Topic 6: Weathering, Erosion and Erosional-Deposition Systems (workbook p ) Workbook Chapter 4, 5 WEATHERING

Topic 6: Weathering, Erosion and Erosional-Deposition Systems (workbook p ) Workbook Chapter 4, 5 WEATHERING Topic 6: Weathering, Erosion and Erosional-Deposition Systems (workbook p. 95-125) Workbook Chapter 4, 5 THE BIG PICTURE: Weathering, erosion and deposition are processes that cause changes to rock material

More information

1. Any process that causes rock to crack or break into pieces is called physical weathering. Initial product = final product

1. Any process that causes rock to crack or break into pieces is called physical weathering. Initial product = final product Weathering 1. Any process that causes rock to crack or break into pieces is called physical weathering. Initial product = final product End Result of physical weathering is increased surface area. 2. Physical

More information

Be able to understand the processes which occurred during the last ice age.

Be able to understand the processes which occurred during the last ice age. Glaciation Learning Intentions Be able to understand the processes which occurred during the last ice age. Be able to describe and explain the formation of features formed during glacial periods. 1 Water

More information

NEAR KEMPTON. (PL. I. AND PL. II.)

NEAR KEMPTON. (PL. I. AND PL. II.) NOTES ON A CHIPPED BOULDER FOUND NEAR KEMPTON. (PL. I. AND PL. II.) By Fritz Noetling, M.A., Ph.D., etc. (Read May nth, 1908.) It has rather been a problem whence the Tasmanian Aborigines obtained the

More information

ANALECTA ARCHAEOLOGICA RESSOVIENSIA VOLUME 12 RZESZÓW 2017

ANALECTA ARCHAEOLOGICA RESSOVIENSIA VOLUME 12 RZESZÓW 2017 ANALECTA ARCHAEOLOGICA RESSOVIENSIA VOLUME 12 RZESZÓW 2017 Marta Połtowicz-Bobak* DOI: 10.15584/anarres.2017.12.18 Tadeusz Wiśniewski (ed.) Klementowice. A Magdalenian site in eastern Poland, Institute

More information

Mechanical Weathering Processes

Mechanical Weathering Processes Mechanical Weathering Processes How Rock Fragmentation Influences Weathering 1. Smaller particles transport more easily. 2. Fractured materials have decreased strength, and concentrate stresses at crack

More information

Weathering, Erosion, Deposition

Weathering, Erosion, Deposition Weathering, Erosion, Deposition The breakdown of rocks at or near the Earth s Surface. Physical Chemical - The breakdown of rock into smaller pieces without chemical change. - Dominant in moist /cold conditions

More information

PHASE 1 ARCHAEOLOGICAL ASSESSMENT OF A PORTION OF MAIN ROAD 174 N1 TO KLIPHEUWEL

PHASE 1 ARCHAEOLOGICAL ASSESSMENT OF A PORTION OF MAIN ROAD 174 N1 TO KLIPHEUWEL PHASE 1 ARCHAEOLOGICAL ASSESSMENT OF A PORTION OF MAIN ROAD 174 N1 TO KLIPHEUWEL Prepared for Erica Van Den Honert (Environmental Consultant) March 1998 Prepared by Archaeology Contracts Office Department

More information

Engineering Geology ECIV 3302

Engineering Geology ECIV 3302 Engineering Geology ECIV 3302 Instructor : Dr. Jehad Hamad 2019-2018 Chapter (5) Weathering & Soil Chapter 5: Weathering, Soil, and Mass Wasting External processes include : (1) Weathering (2) Mass wasting

More information

RAINBOW BAR: SOME OBSERVATIONS AND THOUGHTS

RAINBOW BAR: SOME OBSERVATIONS AND THOUGHTS I Lithics 21, 2000, 36-44 RAINBOW BAR: SOME OBSERVATIONS AND THOUGHTS Brian Hack INTRODUCTION Rainbow Bar is the name given to a small gravel spit that occurs adjacent to the tiny harbour at Hill Head,

More information

LITHIC ASSEMBLAGES: TRANSITIONS OF HOLOCENE TECHNOLOGICAL ORGANIZATION

LITHIC ASSEMBLAGES: TRANSITIONS OF HOLOCENE TECHNOLOGICAL ORGANIZATION Chapter 10: Lithic Assemblages 177 10 LITHIC ASSEMBLAGES: TRANSITIONS OF HOLOCENE TECHNOLOGICAL ORGANIZATION John Dockall and Charlotte D. Pevny This chapter details the results of technological and functional

More information

Davide Delpiano, Marco Peresani & Andreas Pastoors. Exploring Neanderthal skills from 3D knapping reconstruction

Davide Delpiano, Marco Peresani & Andreas Pastoors. Exploring Neanderthal skills from 3D knapping reconstruction Davide Delpiano, Marco Peresani & Andreas Pastoors Exploring Neanderthal skills from 3D knapping reconstruction Objectivs: Verify the contribution of 3D approach for the analysis of Lithic Refitting TECHNICAL

More information

With an Appendix by Brian Sloan, Centre for Archaeological Fieldwork, Queen s University, Belfast

With an Appendix by Brian Sloan, Centre for Archaeological Fieldwork, Queen s University, Belfast Supplement to Report No. 52 Henry Welsh Surface Artefact Collection Ballytaylor County Antrim With an Appendix by Brian Sloan, Centre for Archaeological Fieldwork, Queen s University, Belfast 2 Ulster

More information

THE SCIENCE OF MAPS. ATL Skill: Critical thinking - Use models and simulations to explore complex systems and issues

THE SCIENCE OF MAPS. ATL Skill: Critical thinking - Use models and simulations to explore complex systems and issues THE SCIENCE OF MAPS 8.9C interpret topographic maps and satellite views to identify land and erosional features and predict how these features may be reshaped by weathering ATL Skill: Critical thinking

More information

Leland W. Patterson; Louis V. Hoffman; Rose Marie Higginbotham; Ruth D. Simpson

Leland W. Patterson; Louis V. Hoffman; Rose Marie Higginbotham; Ruth D. Simpson Analysis of Lithic Flakes at the Calico Site, California Leland W. Patterson; Louis V. Hoffman; Rose Marie Higginbotham; Ruth D. Simpson Journal of Field Archaeology, Vol. 14, No. 1. (Spring, 1987), pp.

More information

Mechanical Weathering

Mechanical Weathering Weathering is the disintegration and decomposition of material at or near the surface. Erosion is the incorporation and transportation of material by a mobile agent, usually water, wind, or ice. Geologists

More information

Figure 1 The map shows the top view of a meandering stream as it enters a lake. At which points along the stream are erosion and deposition dominant?

Figure 1 The map shows the top view of a meandering stream as it enters a lake. At which points along the stream are erosion and deposition dominant? 1. In which type of climate does chemical weathering usually occur most rapidly? 1. hot and dry 3. cold and dry 2. hot and wet 4. cold and wet 2. Figure 1 The map shows the top view of a meandering stream

More information

0$.+$'0$$1(61$16,7( of its excavation.

0$.+$'0$$1(61$16,7( of its excavation. Vermeersch P.M. & E. Paulissen & D. Huyge, 2000. Makhadma 2, An Esnan Site, in Pierre M. Vermeersch (Ed.), Palaeolithic Living Sites in Upper and Middle Egypt. Leuven, Leuven University Press: 211-226.

More information

What factors affect the angle of a slope?

What factors affect the angle of a slope? Climate Rock type and Structure What factors affect the angle of a slope? Aspect Fast mass movements Slides: Slides are movements along the SLIP PLANE, i.e. a line of weakness in the rock or soil structure.

More information

1$*$+0('(/.+$/,)$$1$&+(8/($16,7(

1$*$+0('(/.+$/,)$$1$&+(8/($16,7( Vermeersch P.M. & E. Paulissen, M. Otte & G. Gijselings, 2000. Nag Ahmed el Khalifa, An Acheulean Site, in Pierre M. Vermeersch (Ed.), Palaeolithic Living Sites in Upper and Middle Egypt. Leuven, Leuven

More information

Excavations at Clocken Syke Farm, Dairy Lane,Dacre By Nidderdale Iron-age Archaeology community group 2015 and 2016

Excavations at Clocken Syke Farm, Dairy Lane,Dacre By Nidderdale Iron-age Archaeology community group 2015 and 2016 Excavations at Clocken Syke Farm, Dairy Lane,Dacre By Nidderdale Iron-age Archaeology community group 2015 and 2016 1 Introduction The Nidderdale Iron-Age group and its forerunners have been investigating

More information

Weathering: the disintegration, or breakdown of rock material

Weathering: the disintegration, or breakdown of rock material Weathering: the disintegration, or breakdown of rock material Mechanical Weathering: no change in chemical composition--just disintegration into smaller pieces Chemical Weathering: breakdown as a result

More information

Erosion and Deposition

Erosion and Deposition Erosion and Deposition Erosion Sediment natural forces move rock/soil from one place to another. gravity, water, wind, glaciers, waves are causes material moved by erosion Deposition when erosion lays

More information

Page 1 of 9 Name: Base your answer to the question on the diagram below. The arrows show the direction in which sediment is being transported along the shoreline. A barrier beach has formed, creating a

More information

Quaternary Research. New insights into hominin lithic activities at FLK North Bed I, Olduvai Gorge, Tanzania

Quaternary Research. New insights into hominin lithic activities at FLK North Bed I, Olduvai Gorge, Tanzania Quaternary Research 74 (2010) 376 387 Contents lists available at ScienceDirect Quaternary Research journal homepage: www.elsevier.com/locate/yqres New insights into hominin lithic activities at FLK North

More information

Adaptive Radiations in Prehistoric Panama

Adaptive Radiations in Prehistoric Panama Adaptive Radiations in Prehistoric Panama Edited by Olga F. Linares Smithsonian Tropical Research Institute and Anthony J. Ranere Temple University PEABODY MUSEUM OF ARCHAEOLOGY AND ETHNOLOGY HARVARD UNIVERSITY,

More information

Boreholes. Implementation. Boring. Boreholes may be excavated by one of these methods: 1. Auger Boring 2. Wash Boring 3.

Boreholes. Implementation. Boring. Boreholes may be excavated by one of these methods: 1. Auger Boring 2. Wash Boring 3. Implementation Boreholes 1. Auger Boring 2. Wash Boring 3. Rotary Drilling Boring Boreholes may be excavated by one of these methods: 4. Percussion Drilling The right choice of method depends on: Ground

More information

Rocks don't form into the three types of rocks and stay there. The Earth is constantly changing and in motion. The rock cycle demonstrates how a rock

Rocks don't form into the three types of rocks and stay there. The Earth is constantly changing and in motion. The rock cycle demonstrates how a rock Rocks don't form into the three types of rocks and stay there. The Earth is constantly changing and in motion. The rock cycle demonstrates how a rock can start out as one type and change into another.

More information

1/6/ th Grade Earth s Surface. Chapter 3: Erosion and Deposition. Lesson 1 (Mass Movement)

1/6/ th Grade Earth s Surface. Chapter 3: Erosion and Deposition. Lesson 1 (Mass Movement) Lesson 1 (Mass Movement) 7 th Grade Earth s Surface Chapter 3: Erosion and Deposition Weathering the chemical and physical processes that break down rock at Earth s surface Mechanical weathering when rock

More information

13. Sedimentary Rocks I (p )

13. Sedimentary Rocks I (p ) 13. Sedimentary Rocks I (p. 194-208) Sediment Deposition Weathering results in rock being broken down into smaller fragments, called regolith. This regolith is then broken down to form soil. The regolith

More information

Relative Dating Introduction: Types of Relative Dating:

Relative Dating Introduction: Types of Relative Dating: Relative Dating Introduction: In the early stage of prehistoric studies, dating of any event or site was obtained tentatively. A particular event or specimen is dated in relation to other event or some

More information

Journal of Anthropological Archaeology

Journal of Anthropological Archaeology Journal of Anthropological Archaeology 28 (2009) 274 289 Contents lists available at ScienceDirect Journal of Anthropological Archaeology journal homepage: www.elsevier.com/locate/jaa Were Olduvai Hominins

More information

Wednesday, October 10 th

Wednesday, October 10 th Wednesday, October 10 th Page 13a (left side) / Place Lab on table Objective: We will describe the different types of weathering and erosion and identify evidence of each type. Warm-up: 1. What is weathering?

More information

Earthquakes and Seismotectonics Chapter 5

Earthquakes and Seismotectonics Chapter 5 Earthquakes and Seismotectonics Chapter 5 What Creates Earthquakes? The term Earthquake is ambiguous: Applies to general shaking of the ground and to the source of the shaking We will talk about both,

More information

Bell Ringer. Are soil and dirt the same material? In your explanation be sure to talk about plants.

Bell Ringer. Are soil and dirt the same material? In your explanation be sure to talk about plants. Bell Ringer Are soil and dirt the same material? In your explanation be sure to talk about plants. 5.3 Mass Movements Triggers of Mass Movements The transfer of rock and soil downslope due to gravity is

More information

How mountains are made. We will talk about valleys (erosion and weathering later)

How mountains are made. We will talk about valleys (erosion and weathering later) How mountains are made We will talk about valleys (erosion and weathering later) http://www.ilike2learn.com/ilike2learn/mountainmaps/mountainranges.html Continent-continent plate convergence Less dense,

More information

UNIT SEVEN: Earth s Water. Chapter 21 Water and Solutions. Chapter 22 Water Systems. Chapter 23 How Water Shapes the Land

UNIT SEVEN: Earth s Water. Chapter 21 Water and Solutions. Chapter 22 Water Systems. Chapter 23 How Water Shapes the Land UNIT SEVEN: Earth s Water Chapter 21 Water and Solutions Chapter 22 Water Systems Chapter 23 How Water Shapes the Land Chapter Twenty-Three: How Water Shapes the Land 23.1 Weathering and Erosion 23.2

More information

AdditionalArch~eojogicaISiur\T~f

AdditionalArch~eojogicaISiur\T~f AdditionalArch~eojogicaISiur\T~f /' In Th~eDrfComalW8tershed,ComalCoIlntf, Sufith.Central Texas of'!....",i" THOMAS C. KELLY and THOMAS R. HESTER Center for Archaeological Research TheUni\Tersity of Texas

More information

Geog 1000 Lecture 17: Chapter 10

Geog 1000 Lecture 17: Chapter 10 Geog 1000 Lecture 17: Chapter 10 Landslides and Mass Movements Link to lectures: http://scholar.ulethbridge.ca/chasmer/classes/ Today s Lecture 1. Assignment 2 Due Pick up Assignment 1 if you don t have

More information

Hydraulics Prof. Dr. Arup Kumar Sarma Department of Civil Engineering Indian Institute of Technology, Guwahati

Hydraulics Prof. Dr. Arup Kumar Sarma Department of Civil Engineering Indian Institute of Technology, Guwahati Hydraulics Prof. Dr. Arup Kumar Sarma Department of Civil Engineering Indian Institute of Technology, Guwahati Module No. # 08 Pipe Flow Lecture No. # 05 Water Hammer and Surge Tank Energy cannot be consumed

More information

Chapter 2 Planet Earth

Chapter 2 Planet Earth Chapter 2 Planet Earth Section Notes Earth and the Sun s Energy Water on Earth The Land Close-up The Water Cycle World Almanac Major Eruptions in the Ring of Fire Quick Facts Chapter 2 Visual Summary Video

More information

1. The diagram below shows the stump of a tree whose root grew into a small crack in bedrock and split the rock apart.

1. The diagram below shows the stump of a tree whose root grew into a small crack in bedrock and split the rock apart. 1. The diagram below shows the stump of a tree whose root grew into a small crack in bedrock and split the rock apart. 4. Which process involves either a physical or chemical breakdown of earth materials?

More information

Name. 4. The diagram below shows a soil profile formed in an area of granite bedrock. Four different soil horizons, A, B, C, and D, are shown.

Name. 4. The diagram below shows a soil profile formed in an area of granite bedrock. Four different soil horizons, A, B, C, and D, are shown. Name 1. In the cross section of the hill shown below, which rock units are probably most resistant to weathering? 4. The diagram below shows a soil profile formed in an area of granite bedrock. Four different

More information

7.5. Weathering Breaks Down Rocks

7.5. Weathering Breaks Down Rocks 7.5 Weathering Breaks Down Rocks Preview the section and read the headings. How many types of weathering will you be learning about in this section? An old cemetery can be an interesting place to visit.

More information

Weathering and Erosion

Weathering and Erosion Have you ever looked at the land around you and wondered how it was shaped? The geologic features that help define the world are still being shaped by the natural processes of weathering, erosion, and

More information

Module 7: Plate Tectonics and Earth's Structure Topic 4 Content : Earthquakes Presentation Notes. Earthquakes

Module 7: Plate Tectonics and Earth's Structure Topic 4 Content : Earthquakes Presentation Notes. Earthquakes Earthquakes 1 Topic 4 Content: Earthquakes Presentation Notes Earthquakes are vibrations within the Earth produced by the rapid release of energy from rocks that break under extreme stress. Earthquakes

More information

Tips for Success on a Test

Tips for Success on a Test Number of Incorrect: Final Grade: Parent Signature: Top Tips for Success on a Test 1. Read the following statements at least two times. 2. Circle the key words in each question/ or statement. (*Remember

More information

SEDIMENTARY TEXTURES:

SEDIMENTARY TEXTURES: SEDIMENTARY TEXTURES: What are they? Grain size Grain shape Particle Surface texture Grain fabric Grain Size Depositional environment - subaerial, water depth, energy Sediment maturity - source, weathering

More information

UNIT 1 - Major Land and Water Forms

UNIT 1 - Major Land and Water Forms UNIT 1 - Major Land and Water Forms Chapter 1 - Landform Patterns and Processes Topography the natural and human features of the Earth s surface. ie. Surface features elevation - the height of a particular

More information

CONTENTS. An Analysis of the Lithic Artifact Assemblage From the Forbush Creek Site (31Ydl), Yadkin County, North Carolina... Jane M.

CONTENTS. An Analysis of the Lithic Artifact Assemblage From the Forbush Creek Site (31Ydl), Yadkin County, North Carolina... Jane M. STUDIES Volume XXXIV October 1985 The Southern Indian Studies was established in April, 1949, as a medium of publication and discussion of information pertaining to the life and customs of the Indians

More information

Soil Mechanics. Chapter # 1. Prepared By Mr. Ashok Kumar Lecturer in Civil Engineering Gpes Meham Rohtak INTRODUCTION TO SOIL MECHANICS AND ITS TYPES

Soil Mechanics. Chapter # 1. Prepared By Mr. Ashok Kumar Lecturer in Civil Engineering Gpes Meham Rohtak INTRODUCTION TO SOIL MECHANICS AND ITS TYPES Soil Mechanics Chapter # 1 INTRODUCTION TO SOIL MECHANICS AND ITS TYPES Prepared By Mr. Ashok Kumar Lecturer in Civil Engineering Gpes Meham Rohtak Chapter Outlines Introduction to Soil Mechanics, Soil

More information

ANALYSIS OF QUARTZ IN NORTHERN WISCONSIN: DEFICIENCIES, MISCONCEPTIONS AND GOALS

ANALYSIS OF QUARTZ IN NORTHERN WISCONSIN: DEFICIENCIES, MISCONCEPTIONS AND GOALS University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Nebraska Anthropologist Anthropology, Department of 2005 ANALYSIS OF QUARTZ IN NORTHERN WISCONSIN: DEFICIENCIES, MISCONCEPTIONS

More information

1. Which type of climate has the greatest amount of rock weathering caused by frost action? A) a wet climate in which temperatures remain below

1. Which type of climate has the greatest amount of rock weathering caused by frost action? A) a wet climate in which temperatures remain below 1. Which type of climate has the greatest amount of rock weathering caused by frost action? A) a wet climate in which temperatures remain below freezing B) a wet climate in which temperatures alternate

More information

Prehistoric Clay Sources: A Forensic Exercise in Geoarchaeology

Prehistoric Clay Sources: A Forensic Exercise in Geoarchaeology Prehistoric Clay Sources: A Forensic Exercise in Geoarchaeology Lynn Ketterhagen Faculty Sponsor: Dean Wilder, Department of Geography and Earth Science ABSTRACT The prehistoric Oneota culture of the Upper

More information

What type of land feature is located at Point A? A Cliff B Delta C Mountain D Valley

What type of land feature is located at Point A? A Cliff B Delta C Mountain D Valley 1 What type of land feature is located at Point A? A Cliff B Delta C Mountain D Valley Alfred Wegener s theory of continental drift was 2 not accepted by scientists when the theory was first proposed.

More information

LAB 6: TRINIDAD BEACH FIELD TRIP

LAB 6: TRINIDAD BEACH FIELD TRIP OBJECTIVES: LAB 6: TRINIDAD BEACH FIELD TRIP 1) to develop your powers of observation, especially of geological phenomena; 2) to identify the rocks exposed at Trinidad Beach; 3) to reconstruct some of

More information

Introduction to Weathering

Introduction to Weathering Name: Date: Period: Unit 9: Earth s Destructive Forces A. Kinds of Weathering Introduction to Weathering Distinguish between two major processes that change the Earth surface. Identify two types of weathering.

More information

All About Rocks. What Exactly Are Rocks? 298 words. Born from Magma: Igneous Rock 223 words. Layer After Layer: Sedimentary Rock 192 words

All About Rocks. What Exactly Are Rocks? 298 words. Born from Magma: Igneous Rock 223 words. Layer After Layer: Sedimentary Rock 192 words ARTICLE-A-DAY All About Rocks 6 Articles Check articles you have read: What Exactly Are Rocks? 298 words Born from Magma: Igneous Rock 223 words Layer After Layer: Sedimentary Rock 192 words Changing Form:

More information

Kara-Bom: new investigations of a Palaeolithic site in the Gorny Altai, Russia

Kara-Bom: new investigations of a Palaeolithic site in the Gorny Altai, Russia Kara-Bom: new investigations of a Palaeolithic site in the Gorny Altai, Russia Natalia E. Belousova 1,2,, Evgeny P. Rybin 1,2, Alexander Yu. Fedorchenko 1,2 &AntonA.Аnoykin 1,2 New archaeological investigations

More information

Minerals and Rocks Chapter 20

Minerals and Rocks Chapter 20 Minerals and Rocks Chapter 20 Emily and Megan Earth System Science Interconnected Rocks and minerals Interior processes Erosion and deposition Water and air Elements of Earth by weight Made of atoms Earth

More information

Lab 3: Minerals and the rock cycle. Rocks are divided into three major categories on the basis of their origin:

Lab 3: Minerals and the rock cycle. Rocks are divided into three major categories on the basis of their origin: Geology 101 Name(s): Lab 3: Minerals and the rock cycle Rocks are divided into three major categories on the basis of their origin: Igneous rocks (from the Latin word, ignis = fire) are composed of minerals

More information

Cover Page. The handle holds various files of this Leiden University dissertation.

Cover Page. The handle   holds various files of this Leiden University dissertation. Cover Page The handle http://hdl.handle.net/1887/19054 holds various files of this Leiden University dissertation. Author: Zwyns, Nicolas Title: Laminar technology and the onset of the Upper Paleolithic

More information

2011 Iredell Statesville Schools 4 th Grade Science Q1 Q2 Q3 Q4. Forces and Motion

2011 Iredell Statesville Schools 4 th Grade Science Q1 Q2 Q3 Q4. Forces and Motion Essential Standard: 4.P.1 Explain how various forces affect the motion of an object. Forces and Motion Q1 Q2 Q3 Q4 Clarifying Objectives: 4.P.1.1 Explain how magnets interact with all things made of iron

More information

Stratigraphy: Establishing a Sequence from Excavated Archaeological Evidence

Stratigraphy: Establishing a Sequence from Excavated Archaeological Evidence Stratigraphy: Establishing a Sequence from Excavated Archaeological Evidence THE PRINCIPLES OF STRATIGRAPHY In order to explain how and why cultural and social forms change through time, archaeologists

More information

Emily and Megan. Earth System Science. Elements of Earth by weight. Crust Elements, by weight. Minerals. Made of atoms Earth is mostly iron, by weight

Emily and Megan. Earth System Science. Elements of Earth by weight. Crust Elements, by weight. Minerals. Made of atoms Earth is mostly iron, by weight Emily and Megan Chapter 20 MINERALS AND ROCKS Earth System Science Interconnected Rocks and minerals Interior processes Erosion and deposition Water and air Elements of Earth by weight Made of atoms Earth

More information

Objectives: Define Relative Age, Absolute Age

Objectives: Define Relative Age, Absolute Age S6E5. Students will investigate the scientific view of how the earth s surface is formed. c. Classify rocks by their process of formation. g. Describe how fossils show evidence of the changing surface

More information

Fill in the blank with the word that completes the sentence. Then, find that work in the puzzle.

Fill in the blank with the word that completes the sentence. Then, find that work in the puzzle. Classwork #1 Name: 2 nd Grade PSI Fill in the blank with the word that completes the sentence. Then, find that work in the puzzle. 1. When the Earth is facing the sun, it is time. 2. Another word for spins

More information

Copyright Dawn T. Nicholson

Copyright Dawn T. Nicholson opyright awn T. Nicholson 2003. -mail d.nicholson@mmu.ac.uk ROSIONL LNORMS: HUTS hutes are quasi-channels down which material is transported. They might or might not be produced as a result of deterioration,

More information

Unit 3 Study Guide -- Greenberg science, 6C

Unit 3 Study Guide -- Greenberg science, 6C Unit 3 Study Guide -- Greenberg science, 6C Name Pd. Date / / 2018 + +5 extra credit points on the test if submitted complete and correct ON THE TEST DATE. + A copy can be found on my website mgreenberg.weebly.com

More information

THE CHANGING SURFACE OF THE EARTH

THE CHANGING SURFACE OF THE EARTH THE CHANGING SURFACE OF THE EARTH Key words Drain geological agent weathering erosion Sediment deposition transport The landscape is a consequence of the action of two types of geological processes; internal

More information

TAKE HOME EXAM 8R - Geology

TAKE HOME EXAM 8R - Geology Name Period Date TAKE HOME EXAM 8R - Geology PART 1 - Multiple Choice 1. A volcanic cone made up of alternating layers of lava and rock particles is a cone. a. cinder b. lava c. shield d. composite 2.

More information

GCSE ready intervention tasks

GCSE ready intervention tasks 7. Earth 1 LEARNING CONTEXT AQA Big idea: 3.7 Earth AQA Strand: 3.7.1 Earth structure 3.7.2 Universe AQA Enquiry processes: 2.3 Draw conclusions 2.7 Critique claims How this provides GCSE readiness: The

More information

Sediment and sedimentary rocks Sediment

Sediment and sedimentary rocks Sediment Sediment and sedimentary rocks Sediment From sediments to sedimentary rocks (transportation, deposition, preservation and lithification) Types of sedimentary rocks (clastic, chemical and organic) Sedimentary

More information

Chapter 2. Wearing Down Landforms: Rivers and Ice. Physical Weathering

Chapter 2. Wearing Down Landforms: Rivers and Ice. Physical Weathering Chapter 2 Wearing Down Landforms: Rivers and Ice Physical Weathering Weathering vs. Erosion Weathering is the breakdown of rock and minerals. Erosion is a two fold process that starts with 1) breakdown

More information

AN ANALYSIS OF THE LITHIC COLLECTIONS FROM RAINBOW BAR, HAMPSHIRE

AN ANALYSIS OF THE LITHIC COLLECTIONS FROM RAINBOW BAR, HAMPSHIRE AN ANALYSIS OF THE LITHIC COLLECTIONS FROM RAINBOW BAR, HAMPSHIRE J. Sommerville 1 and E. A. Tetlow 2 ABSTRACT In the present paper the site of Rainbow Bar on the Hampshire coast is discussed. Lithics

More information

Weathering, Erosion & Soils Quiz

Weathering, Erosion & Soils Quiz Weathering, Erosion & Soils Quiz Multiple Choice Identify the choice that best completes the statement or answers the question. 1. The diagram below shows a cross-section of a rock layer. Erosion is the

More information

GEOG 1010A. Come to the PASS workshop with your mock exam complete. During the workshop you can work with other students to review your work.

GEOG 1010A. Come to the PASS workshop with your mock exam complete. During the workshop you can work with other students to review your work. It is most beneficial to you to write this mock midterm UNDER EXAM CONDITIONS. This means: Complete the midterm in 1.5 hours. Work on your own. Keep your notes and textbook closed. Attempt every question.

More information

Water - most influential force in erosion

Water - most influential force in erosion Erosion and Deposition Agents, Forces, and Results What Caused This? What is Erosion? Erosion - moving of rock material from one place to a new location For erosion to occur three processes must take place:

More information

Periglacial Geomorphology

Periglacial Geomorphology Periglacial Geomorphology Periglacial Geomorphology Periglacial: literally means around glacial - term introduced in 1909 to describe landforms and processes around glaciated areas. Periglacial environments:

More information

How to Build a Mountain and other Geologic Structures. But first a short review

How to Build a Mountain and other Geologic Structures. But first a short review How to Build a Mountain and other Geologic Structures But first a short review Where do we see deep earthquakes? What is happening there? What can happen at a plate boundary? 1. Plates can move apart

More information