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25

SAGVNTVM (PLAV) 45 2013 25 - 38

ISSN 0210-3729

ISSN online 2174-517X

DOI 107203SAGVNTVM452007

Texto recibido el 01012013

Texto aceptado el 30052013

HVGH OD ORFDOLW]DFLy L H[FDYDFLy VLVWHPjWLFD GmiddotDV-sentaments a lrsquoaire lliure en les darreres degravecades el tre-

EDOO VREUH FRYHV KD SHUGXW FHUWD HPEUDQ]LGD HVSUpVGmiddotHQWHQGUH TXH HOV KjELWDWV L JUDQ SDUW GH OHV DFWLYLWDWVHFRQzPLTXHVVmiddotKDQGXWDWHUPHDOmiddotDLUHOOLXUHOHVFRYHVKDQTXHGDWVRYLQWOOLJDGHVDDFWLYLWDWVVHFXQGjULHVUHODFL-RQDGHV DPE OmiddotHPPDJDW]HPDWJH SH[ VLWJHVIRVVD D ODampRYD DPE OD WUDQVKXPjQFLD L HVWDEXODFLy SH[ampRYDampRORPHUDRampRYDGHODXLQHXRDPEODLQKXPDFLy

(p ex Cova de lrsquoAvellaner) entre drsquoaltres vinculades

drsquouna manera o altra a assentaments a lrsquoaire lliure Mo-

GHOVGmiddotDTXHVWHVWLOVmiddotKDQSURSRVDWSHU3ODQVDOORVDLODYDOOGHOOLHUFDRVFKRSHUOHVXL[HUHVGH9LOREtLlrsquoAlt Penedegraves (Mestres i Ribeacute 1992)

Al Prepirineu i Pirineu a lrsquooest del riu Segre les dades

VREUHSRVVLEOHVDVVHQWDPHQWVDOmiddotDLUHOOLXUHVyQPROWHVFDV-VHVLHVOLPLWHQDFHUWHVWUREDOOHVGHVFRQWH[WXDOLW]DGHVR WD-OOHUVGHVtOH[micro5RGDQpVL5DPyQ2PVet al 2009)

(QDTXHVWWUHEDOOHVSUHVHQWHQOHVGDGHVUHIHUHQWVDODampRYDampRORPHUD6DQW(VWHYHGHOD6DUJD3DOODUV-XVVjGXUDQWHO1HROtWLFFDUGLDOAgraveQDO$SDUWLUGHOVGLIHUHQWV VRQGHMRVGXWVD WHUPHGHVGH OmiddotDQ VmiddotKDSRJXWREVHUYDU ODYDULHWDWGmiddotXVRV L IXQFLRQDOLWDWVGHO MDFLPHQWHQPRPHQWVSRWHQFLDOPHQWVLQFUzQLFV3HUXQDEDQGDXQD]RQDRQSUHGRPLQHQOHVHVWUXFWXUHVGHFDLUHGRPqVWLFIRJDUVIRVVHVLIRUDWVGHSDOTXHHQVPRVWUHQOHVGDGHVHQWRUQOmiddotKjELWDWDOMDFLPHQWLSHUDOWUDEDQGDXQJUDQVHFWRUGHODFDYLWDWGHGLFDWDOmiddotHVWDEXODFLyGHUDPDWVDPEsediments de tipus IXPLHULSUREDEOHPHQWWDPEpDOmiddotHPPDJDW]HPDWJH7RWDL[zVXFFHHL[HQXQHVGDWDFLRQVGmiddotHQWUHL3$TXHVWHVGDGHVHVFRQWH[WXDOLW]HQDPEOHVGmiddotDOWUHVMDFLPHQWVGHOD]RQDSLULQHQFDXQjPELWTXHVHPSUHKDHVWDWGHAgraveQLWHQODELEOLRJUDAgraveDFRPXQHVSDLGHSDVHQWUHGLIHUHQWVELzWRSVHFROzJLFVGHOHVSODQHVIqUWLOVDOHVSDVWXUHVGmiddotHVWLX

Paraules clauKjELWDWHQFRYDHVWDEXODFLy1HROtWLFDQWLF3UHSLULQHXGHOHLGD

CAVE SETTLEMENT AND HERDING SPACES CA 6200-6000 BP THE EARLY NEOLITHIC AT COVA COLOMERA (PRE-PYRENEES OF LLEIDA) PRELIMINARY RESULTS

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Key wordsFDYHKDELWDWKRXVLQJ(DUO1HROLWKLF3UH3UHQHHVRIOHLGD

HAgraveBITAT EN COVA I ESPAI PELS RAMATS CA 6200-6000 BP LA COVA COLOMERA (PREPIRINEU DE LLEIDA) DURANT EL

NEOLIacuteTIC ANTIC

F XAVIER OMS JUAN M LOacutePEZ-GARCIacuteA XAVIER MANGADO PATRICIA MARTIN SUSANA MENDIELA

-8$1025$(605($3(52$11$525Igrave8(=shy$7$525Igrave8(=amp17$60$5$lt8(52

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HVRSFLRQVSHUH[SOLFDUDTXHVWDPDQFDGHMDFLPHQWVVyQGXHVSRVVLEOHIDOWDGHSURVSHFFLyRGmiddotREUHVYLjULHVRGmiddotXQWLSXVVLPLODUTXHQmiddotKDJLQIDFLOLWDWODWUREDOODRKjELWDWGLV-SHUVTXHQRQHFHVVLWDULDGHJUDQVDVVHQWDPHQWVTXHKDJLQGHL[DW HPSUHPWHV acuteDUTXHROzJLTXHVmicro GmiddotHQWLWDW HQ DTXHVWVWHUULWRULV3HUDTXHVWPRWLX OmiddotH[FDYDFLyGHFDYLWDWVFRQWL-QXDVHQWOmiddot~QLFDPDQHUDGHFDUDFWHULW]DUHOVWLSXVGmiddotDFWLYLWDWKXPDQDHQDTXHVWD]RQD(QDTXHVWVHQWLWOHVGDGHVFRPHQ-

FHQDVHULPSRUWDQWVHVGHODGqFDGDGHOVDQVGHOVVREUHWRWD$UDJyVmiddotKDQH[FDYDWXQLPSRUWDQWQRPEUHGHMDFLPHQWVHQWUHHOVTXDOVGHVWDTXHQODampXHYDGHampKDYHVODampXHYDGHO0RURGH2OYHQDROmiddot(VSOXJDGHOD3XDVFDGDHQWUHPROWVGmiddotDOWUHV$ampDWDOXQDOHVGDGHVKDQHVWDWPH-QRUVSHUzHQHOVGDUUHUVDQVVmiddotKDQLQFUHPHQWDWGHPDQHUDimportant amb la recerca a la Cova del Parco la Cova Gran

GH6DQWDLQDRODampRYDampRORPHUDHQWUHGmiddotDOWUHV0ROWVDOWUHVMDFLPHQWVMDFRQHJXWVGHVGHOVLLQLFLVGHOPRVWUHQGDGHVVREUHOmiddotRFXSDFLyGHO3UHSLULQHXDOmiddotRHVWGHOULX6HJUHWRWLTXHQRFRPSWHQDPEGDGHVHVWUDWLJUjAgraveTXHV(Oms et al 2012) Malauradament les dades disponibles

GHMDFLPHQWVDOmiddotDLUHOOLXUHFRQWLQXHQVHQWTXDVLQXOAtildeOHVVLH[FHSWXHPHOVFDVRVGH3ODQVDOORVDRVFKet al 1999) i la

Font del Ros (Pallareacutes et al 1997) al Prepirineu oriental

FDWDOjLHOVMDFLPHQWVGH7RUUROOyQL)RUQLOORVDO3UHSLULQHXdrsquoOsca (Utrilla 2012)

LA COVA COLOMERA CONTEXT GEOGRAgraveFIC I GEOLOgraveGIC

Al liacutemit occidental del Prepirineu de Lleida (Catalu-

QDWUREHPOD6HUUDGHO0RQWVHFXQHVSDLQDWXUDODPESURWHFFLySDUFLDOLTXHDPLGDXQVNPGHOODUJHQVHQWLW(2FRQYHUWLQWVHHQXQDXWqQWLFPXUTXHVHSDUDOHVSOD-QHVGHOHLGDDO6LODampRQFDGH7UHPSMXVWDEDQVGHOV3LULQHXVDO1DVHUUDWpXQDPLWMDGmiddotDOoDGDGmiddotHQWUHHOVPVQPLDVVROHL[XQDDOWXUDPj[LPDGHPDOSLFGH6DQW$OtVHVYDOOVTXHHVOOLXUHQDO0RQWVHFHVWUREHQDPVQPSHO6YDOOGmiddotshyJHULPVQPSHON (vall de Sant Esteve) La serra del Montsec es troba

tallada perpendicularment per tres rius (drsquoO a E Noguera

5LEDJRUoDQD1RJXHUD 3DOODUHVD L RL[ TXH KDQ REHUWVHQJOHVFRQJRVWV0RQWUHEHL7HUUDGHWV L3DV1RXTXHKDQ HVWDW SDVVRV FOjVVLFV SHU OD WUDYHVVD GH OD VHUUD(OQRPEUHGHMDFLPHQWVSUHKLVWzULFVHQDTXHVWD]RQDpVPROWHOHYDWLFRPSUqQGHVGHO3DOHROtWLFPLWMjAgraveQVHOAgraveQDOGHOmiddotHGDWGHOURQ]H2PVet al 2009)

La Cova Colomera situada al bell mig del Congost

de Montrebei a una alccedilada de 670 msnm i a 150 m per

sobre el riu teacute unes coordenades UTM (31N ED50) de

ltAgraveJ$DFDYLWDWpVUHVXOWDWGHOmiddotHURVLySDUFLDOGmiddotXQSDTXHW

GHFDOFjULHVVHFXQGjULHVGHO0DDVWULFKWLjLGHJUDQSDUWGmiddotXQD GLjFODVL GmiddotRULHQWDFLy1(62 (OV SURFHVVRV Ej-VLFVGHODVHYDHYROXFLyVyQXQDSULPHUDIDVHGmiddotREHUWXUDDPE SUHGRPLQL GmiddotDJHQWV GH FRUURVLyGLVROXFLy SURFH-GHQWVGHOHVAgraveOWUDFLRQVGHODSODWDIRUPDVXSHULRUSURSHUDa la carena de la serra i una segona de caiguda de blocs

SHUGHVFDOFLAgraveFDFLyGHOVHVWUDWV$OJXQVGmiddotDTXHVWVIHQz-

PHQVVyQGHJUDQPDJQLWXGLSURYRTXHQJUDQVDFXPXOD-FLRQVGHEORFVHQGLIHUHQWVVHFWRUVGHODFRYDHVVHYHVGLPHQVLRQVVyQPGmiddotDOWSHUGmiddotDPSODGDHQODERFDprincipal i una galeria de 180 m de llarg amb una alccedila-

GDPLWMDQDGHPHQWRWDODFRYDDFRYDSUHVHQWDXQYHVWtEXODPSOLLOOXPLQyVHQHOSXQWWRSRJUjAgraveFPpVelevat amb un espai planer drsquouns 60 m

2URGHMDWGHJUDQVEORFVHVWUXFWXUDOV$SDUWLUGmiddotDTXHVWSXQWVmiddotLQLFLDODJUDQJDOHULDHQXQDSHQGHQWPLWMDGmiddotXQVTXHDVVROHL[HOAgraveQDOGHODFDYLWDWDPGHOYHVWtEXO8QDDOWUDSH-

tita boca es troba a lrsquoinici de la portada principal de la

FRYD(VWUDFWDGmiddotXQDJDOHULDDVFHQGHQWTXHPHQDDXQFRUULROTXHWUDQVFRUUHGXUDQWPWRWDOPHQWSHQMDWVR-

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)LJRFDOLW]DFLyLSODQWDGHOMDFLPHQWDPELQGLFDFLyGHOVVRQGH-MRVamp(Lamp9

27

HAgraveBITAT EN COVA I ESPAI PELS RAMATS CA 6200-6000 BP LA COVA COLOMERA (PREPIRINEU DE LLEIDA) DURANT EL NEOLIacuteTIC ANTIC

GyQDDFFpVDOVFRQWUDIRUWVERVFRVRVGmiddotREDJDGHO0RQW-VHF L D SHWLWHV YDOOV L ]RQHV GH EDOPHV DL[t FRP D ODPlana de Montrebei (entre 920 i 974 msnm)

CONTEXT CULTURAL I CRONOLOgraveGIC

La Cova Colomera es troba integrada en un grup de

MDFLPHQWVGHO3LULQHXL3UHSLULQHXHQWUHODYDOOGHO6HJUHLOD]RQDGmiddot2VFDUDQSDUWGmiddotDTXHVWVDVVHQWDPHQWVHVPHQ-

WDWV D OD LQWURGXFFLy VHJXHL[HQ XQHV SDXWHV VLPLODUV HQTXDQW D UHJLVWUH FHUjPLF L D GDWDFLRQV UDGLRFDUEzQLTXHVHV FDUDFWHUtVWLTXHV PpV EjVLTXHV KDQ HVWDW UHFHQWPHQWDQDOLW]DGHV2PVet al 2012)

SHUFHQWDWJHVPHQRUVDOGHGHFRUDFLyFDUGLDOSURIXVLyGHOHVGHFRUDFLRQVLPSUHVHVGmiddotLQVWUXPHQW

(c 30-50)

- inici de les decoracions acanalades

UHSUHVHQWDFLyGHGHFRUDFLRQVLQFLVRLPSUHVHVGHWL-SXVERTXLTXH

- continuiumltat amb les sintaxis decoratives meacutes simples

del Neoliacutetic cardial

IRUTXLOODFURQROzJLFDDSUR[LPDGD3$TXHVWVWUHWVHVWUREHQSUHVHQWVHQMDFLPHQWVFRPOD

Cova del Parco (Petit 1996) Cueva de Chaves Ia i Cueva

GHO0RUR GH2OYHQD acuteFiPDUD VXSHULRUmicro 5DPyQ DL[tFRPHQGmiddotDOWUHVMDFLPHQWVDOVXGLQRUGGHOV3LULQHXV

Pel cas particular de la Cova Colomera tot i algunes

SHWLWHVGLIHUqQFLHVHQHOV UHJLVWUHVGHOVGLIHUHQWVQLYHOOVGHO1HROtWLFDQWLFFUHLHPTXHPRVWUHQXQPDWHL[KRULW]yprou homogeni (Oms 2008) Les datacions radiocarbograveni-

TXHV GLVSRQLEOHV AgraveJ PRVWUHQ DTXHVWD GLQjPLFD QRREVWDQW OD GDWD GHO QLYHOO amp( PRVWUD XQD GLVSHUVLyOOHXJHUDPHQWDOOXQDGDGHODUHVWDSHUzHOUHJLVWUHGLVSR-

QLEOHpVGHOWRWKRPRJHQLAgraveJLSRVVLEOHPHQWDTXHVWDGDWDFLyPRVWUDULDXQODSVHAgraveQDOGHODIDVHDTXtDQDOLW]DGD

)LJ0DWHULDOVFHUjPLFVGHOQHROtWLFDQWLFGHOVVRQGHMRVamp(Lamp9

)LJDWDFLRQVGHOVQLYHOOVGHO1HROtWLFDQWLFGHODampRYDampRORPHUDFDOLEUDGHVPLWMDQoDQWHOVRIWZDUHampDO3DOmiddotFRUED+XO~

28

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ELS AgraveMBITS DE LA COVA

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JUjAgraveFDPHQWPpVHOHYDGDGHODFDYLWDWPHQWUHTXHOmiddotDOWUHVmiddotKDUHDOLW]DWDODGUHWDGHODSULPHUDJUDQVDODGHODFDYL-WDW6RQGHLJamp(VREUHXQJUDQWDO~VTXHHQIRUPDGHventall davalla del vestiacutebul i arriba amb una moderada

SHQGHQWAgraveQVHOAgraveQDOGHODSULPHUDJUDQVDOD(VWDQDOOX-

QDWVDPEGyVVRQGHMRV~QLFDPHQWSHUVLVPHWUHVSHUzHQHVSDLV FRPSOHWDPHQWGLIHUHQWVmiddotHOHFFLyGHOV HVSDLV HVYDUHDOLW]DUDSDUWLUGHOHVH[FDYDFLRQVQRUHJXODGHVGXWHVDWHUPHDODFRYDGXUDQWODGqFDGDGHOVDQVGHOSDVVDWVHJOH H OD9HJD$TXHVWV WUHEDOOV SUHWqULWV YDQIRUQLUXQFRQMXQWGHPDWHULDOVPROWH[WHQVSHUzVHQVHFDSFRQWH[WHVWUDWLJUjAgraveFAgraveDEOHWDQWGHODampRYDampRORPHUDFRPGmiddotDOWUHVMDFLPHQWVGHODVHUUDGHO0RQWVHFLKDQHVWDWUH-visats recentment per nosaltres (Oms et al 2009)

621(amp((63$middot(67$8$ampETH

Els nivells del Neoliacutetic antic de la Cova Colomera

srsquoestenen en aproximadament 13 m2 del Sondeig CE (Co-

ORPHUD(VW$TXHVWHVSDLHVFRUUHVSRQDPEODSDUWEDL[DGHOWDO~VVHGLPHQWDULTXHIRUPDHOFRQGHOYHVWtEXOYHUVlrsquointerior de la cavitat

6middotKDQLGHQWLAgraveFDWAgraveQVHOPRPHQWWUHVQLYHOOVDUTXHROz-

JLFVFRUUHVSRQHQWVDDTXHVWD IDVHamp(amp( Lamp((Oms et alHOVTXDOVHVSUHVHQWHQGHPDQHUDPpV

RPHQVKRULW]RQWDOWRWLTXHDPEDOJXQHVSHUWRUEDFLRQVKDELWXDOV HQ DTXHVW WLSXV GH VHGLPHQWV R QLYHOOV FRPFDXV FORWV GH IXUWLXV R HVWUXFWXUHV SUHKLVWzULTXHV FRPXQDVLWMDIRVVDGHOURQ]HDQWLF2PVet al 2009) o un

UHWDOOLUUHJXODUGHO1HROtWLFAgraveQDO9HUD]LjQLYHOOamp(GR-

FXPHQWDWDOVTXDGUHVLlt(OV WUHV QLYHOOV QHROtWLFV GRFXPHQWDWV VyQGH WLSXV

fumierpVDGLUQLYHOOVGmiddotHVWDEXODFLyGHUDPDWV$TXHVWVUHVSRQHQDXQDFRPSRVLFLyRUJjQLFDGmiddotHVIHUzOLWVAgraveWzOLWVGLDWRPHHVDJUHJDWVFULVWDOAtildeOLQVHWFDGDO$OMD-FLPHQWVmiddotLGHQWLAgraveTXHQFRPXQDVXSHUSRVLFLyGHFDSHVGHGLIHUHQWVFRORUVTXHYDQGHVGHOQHJUHEDL[DWHPSHUDWX-

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HUJDGjURFKLHUDGDO$OOXpHPDQHUDSUHOLPLQDUHVSRWDAgraveUPDUTXHOHVPRVWUHVGHPLFURPRUIRORJLDGHODampRORPHUDSUHVHQWHQXQDWRWDOVLQ-

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elements drsquoorigen excremental ovicapriacute (com pers Mer-

FqHUJDGj7RWLTXHHOGHEDWFRQWLQXDREHUWHVSURSRVDTXH ODAgraveQDOLWDWGDUUHUDVLJXL OmiddotHOLPLQDFLy LQWHQFLRQDOGHUHVLGXVH[FUHPHQWVLSDUjVLWVHOVTXDOVSRGLHQDIHFWDUODsalubritat i lrsquohabitabilitat de la cova per part dels grups

KXPDQVHUJDGjet al 2005 Angelucci et al 2009) No

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$TXHVWDGHJUDGDFLyFURPjWLFDVHPEODUHVSRQGUHDGLIH-rents temperatures assolides a lrsquointerior de lrsquoamuntega-

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(OVWUHVQLYHOOVDUTXHROzJLFVFRPSWHQDPEXQDSRWqQ-

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baix a la dreta amb macro

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DIHFWDWV SHU WUDPSOLQJV i per lrsquoepisodi drsquoabandonament

de la cavitat amb caigudes de grans blocs (nivell CE11)

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ralesa cendrosa de tots els nivells i per tant de la seva

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VHUYDQWVH VHPSUH XQ FDUjFWHU UHSHWLWLX HQ OD GLVSRVLFLyGmiddotDTXHVWVQLYHOOVFUHPDWV9HUJqVet al 2008 Angelucci et alampDGDQLYHOOHVWjFRPSRVWSHUXQJUXSGHIjFLHVTXHHVUHSHWHL[HQVHPSUHDPEODPDWHL[DGLVSRVLFLy$ODEDVHOHVIjFLHVc r o m carbonoses perograve sense massa im-

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dria indicar la curta permanegravencia a la cova no obstant la

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den correspondre amb cabanes o tancats dins de coves

compta amb exemples meacutes escassos com les cabanes de

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Al sondeig CE la presegravencia de nivells de tipus fumier

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espai drsquoaproximadament 20 m2 pels nivells CE 13 i

amp( ampRP VmiddotKD GLW DTXHVW jPELW KDXULD HVWDW HPSUDWFRPDPtQLPHQWUHVIDVHVPRPHQWVHQTXHVmiddotKDXULDHV-tabulat ramats i posteriorment srsquohaurien amuntegat els

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table proximitat entre els nivellsmoments CE13 i CE14

LDOPDWHL[WHPSVOHVGDGHVDUTXHR]RROzJLTXHVLQGLTXHQFLFOHVFRPSOHWVGmiddotHVWDEXODFLyDPEFULDin situ) en els ni-

vells CE12 i CE14

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$PDQFDGHMDFLPHQWVDOmiddotDLUHOOLXUHGRQFVDOmiddotRHVWGHOULX6HJUHOHVFRYHVVyQOHV~QLTXHVTXHSHOPRPHQWSRGHQSURSRUFLRQDUGDGHVUHVSHFWHOmiddotKjELWDWLXVRVGHWHUULWRULGX-

UDQWHO1HROtWLFDQWLFAgraveJ3HUXQDEDQGDFRYHVDEULFVper sota els 700 msnm com la Cueva de Chaves o la Cova

UDQDPEXQDFODUDYRFDFLyKDELWDFLRQDOLSUREDEOHPHQWYHUWHEUDGRUHV GH OD RFXSDFLy GHO WHUULWRUL DOWUHV TXH KRFRPELQDULHQDPEOmiddotHVWDEXODFLyGHUDPDWVampRYDampRORPH-UDLLQFO~VOmiddotHPPDJDW]HPDWJHampRYDGHO3DUFR(QDTXHVWPDWHL[ELzWRSFRYHVRDEULFVGHGLIHUHQWWLSRORJLDLDPEXQHVFDUDFWHUtVWLTXHVPHQVDSWHVSHUOmiddotKjELWDWSHUPDQHQWo semipermanent podrien haver tingut usos meacutes especiacute-

AgraveFVHO)RUDWGHODampRQTXHWDHPPDJDW]HPDWJHLODampRYDGHOampRVFROORODampXHYDGHO0RURGH2OYHQDLQKXPDFLyUHIXJLSXQWXDOHQVHULHQERQVH[HPSOHV(QFDQYLHOVMD-FLPHQWVVLWXDWVSHUVREUHHOVPVQPSRGULHQVHUUHIX-

gis puntuals (Cova del Sardo Cova del Pas de la Lloba

HWFR]RQDGHSDVWUDQVKXPDQW(VSOXJDGHOD3XDVFDGD

CONCLUSIONS

La Cova Colomera esdeveacute un bon exemple drsquousos

complexos drsquouna cavitat ca3HQXQKRULW]yGHFHUjPLTXHVLPSUHVHV2PVVmiddotKLKDH[FDYDWXQjPELWGmiddotHVWDEXODFLyGHUDPDWVLXQDOWUHTXHVHPEODGHV-WLQDWDOmiddotKjELWDW

(OTXHGHPRVWUDDTXHVWH[HPSOHDL[tFRPHOGmiddotDOWUHVMDFLPHQWVGHODYHVVDQWVXGGHOV3LULQHXVRULHQWDOVpVTXHDTXHVWVWHUULWRULVVyQEHQFRQHJXWVLHPSUDWVSHOVJUXSVKXPDQV MD VLJXL GmiddotXQDPDQHUDPpV RPHQV HVWDEOH Rlligat com srsquoha considerat tradicionalment a la transhu-

PjQFLDGmiddotXQDHVFDODHQFDUDGHVFRQHJXGDmiddotKjELWDWDOmiddotDLUHOOLXUHGXUDQWHO1HROtWLFDQWLFpVXQ

IHW IHIDHQW GRFXPHQWDW GHPDQHUDPROW SUROtAgraveFD HQ DO-JXQV WHUULWRULV GXUDQW HOV GDUUHUV DQV VREUHWRW SHU OHV]RQHVRQKDH[LVWLWXQDUHFHUFDPDMRUOOLJDGDDSURMHFWHVGHUHFHUFDREpDOmiddotDUTXHRORJLDSUHYHQWLYDFDVRVGHO3H-QHGqV9DOOqVDUFHORQDRLURQD1RREVWDQWOHV]RQHVWUDGLFLRQDOPHQWPpVGHSULPLGHVSHOTXHIDDODUHFHUFDLOHVLQIUDHVWUXFWXUHVFRPVyQHOVjPELWVSLULQHQFVSHUPH-WHQLREOLJXHQHQFDUDH[FDYDUMDFLPHQWVTXHIRUQHL[HQGmiddotXQDLQIRUPDFLyDOWHUQDWLYDTXHSHUPHWSURSRVDUTXHOHVFRYHVQRHUHQQRPpVELYDFVRHVSDLVGmiddotXWLOLW]DFLyVHFXQ-

GjULDVLQyTXHWDPEpFRPSWDYHQDPEXQDHVWUXFWXUDFLy

37

HAgraveBITAT EN COVA I ESPAI PELS RAMATS CA 6200-6000 BP LA COVA COLOMERA (PREPIRINEU DE LLEIDA) DURANT EL NEOLIacuteTIC ANTIC

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portant en la vida dels grups humans

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$$($7(1=$93DVWRVHVWLpUFRORVQLYHOHVde corral en la Cova de les Cendres La Cova de les Cen-GUHV0RUDLUD7HXODGD$OLFDQWH-HUQDEpXO0ROLQDeds) Alacant 141-146

$(289875$3H1pROLWKLTXHHQ$UDJRQLe 1pROLWKLTXHGXQRUGRXHVW0HGLWpUUDQpHQHampRQJUpV3UpKLVWR-rique de France-9DTXHUHGampDUFDVVRQQH

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DOI httpdxdoiorg103989tp1997v54i2372

(5$shy00amp(5shy$0(675(6-3UiFWLFDVGHHVWDEXODFLyQGXUDQWHHO1HROtWLFR$QWLJXRHQampDWDOXxDDWUDYpV GH OD PLFURPRUIRORJtD D ampXHYD GH D XLQHX)RQW5XEt$OW3HQHGpVDUFHORQDampRQJUHVRGHO1HR-liacutetico en la Peniacutensula Ibeacuterica3$ULDVamp2QWDxyQampampDUFtD0RQFyQHGV6DQWDQGHU

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tal 7UDEDMRVGH3UHKLVWRULD 51 (1) 55-75

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