<?xml version="1.0" encoding="UTF-8"?>
<XML><RECORDS>
<RECORD>
	<REFERENCE_TYPE>0</REFERENCE_TYPE>
	<AUTHORS>
		<AUTHOR>Battisti, C.</AUTHOR>
		<AUTHOR>Trener, G.B.</AUTHOR>
	</AUTHORS>
	<YEAR>1900</YEAR>
	<TITLE>Variazioni del sistema idrografico della Valle di Piné - Le piramidi di Segonzano.</TITLE>
	<SECONDARY_TITLE>Tridentum</SECONDARY_TITLE>
	<VOLUME>3</VOLUME>
	<NUMBER>5-6</NUMBER>
	<PAGES>193-203</PAGES>
	<KEYWORDS>
		<KEYWORD>Geomorfologia,</KEYWORD>
		<KEYWORD>glaciale,</KEYWORD>
		<KEYWORD>fluviale,</KEYWORD>
		<KEYWORD>alluvionale,</KEYWORD>
		<KEYWORD>Altopiano</KEYWORD>
		<KEYWORD>di</KEYWORD>
		<KEYWORD>Piné,</KEYWORD>
		<KEYWORD>Valle</KEYWORD>
		<KEYWORD>di</KEYWORD>
		<KEYWORD>Cembra,</KEYWORD>
		<KEYWORD>Pleistocene,</KEYWORD>
		<KEYWORD>Olocene,</KEYWORD>
		<KEYWORD>Valsugana</KEYWORD>
	</KEYWORDS>
	<NOTES>Anche in estratto in St. Tr. Sc. Nat. 34 (1957)
</NOTES>
</RECORD>
</RECORDS></XML>