4,999 research outputs found
Emma Bell Miles journal, 1908-1911
No full textJournal authored by Walden's Ridge naturalist, artist, and author Emma Bell Miles from 1908 May 24 to 1911 April 25
Emma Bell Miles journal, 1911-1914
No full textJournal authored by Walden's Ridge naturalist, artist, and author Emma Bell Miles from 1911 January 9 to 1914 May 3
Emma Bell Miles journal, 1915-1918
No full textJournal authored by Walden's Ridge naturalist, artist, and author Emma Bell Miles from 1915 November 11 to 1918 August 8
Emma Bell Miles journal, 1915-1918
No full textJournal authored by Walden's Ridge naturalist, artist, and author Emma Bell Miles from 1915 November 11 to 1918 August 8
Emma Bell Miles journal, 1911-1914
No full textJournal authored by Walden's Ridge naturalist, artist, and author Emma Bell Miles from 1911 January 9 to 1914 May 3
Emma Bell Miles journal, 1908-1911
No full textJournal authored by Walden's Ridge naturalist, artist, and author Emma Bell Miles from 1908 May 24 to 1911 April 25
Emma Bell Miles journal, 1915
No full textJournal authored by Walden's Ridge naturalist, artist, and author Emma Bell Miles from 1915 June 15 to 1915 September 22. The journal also includes newspaper clippings of Miles' Fountain Square Conversation column authored for the Chattanooga News
Emma Bell Miles journal, 1915
No full textJournal authored by Walden's Ridge naturalist, artist, and author Emma Bell Miles from 1915 June 15 to 1915 September 22. The journal also includes newspaper clippings of Miles' Fountain Square Conversation column authored for the Chattanooga News
Carmen G. Prieto leyendo la mano a Emma Castro Yahuada en el patio de una casa.
No full textI.O. ""Emma Castro Tahuada"
I brachipodi delle calcareniti di Castro Marina (Lecce).
No full textVengono studiate due successioni affioranti a Castro Marina (Lecce). I risultati di questa ricerca indicano, per tutte e due, un’età pleistocenica inferiore ed un ambiente Neritico Circalittorale, ma precisano anche notevoli differenze. - SEZIONE A – Gli organismi appartengono probabilmente ad una paleobiocenosi del Detritico Costiero infangato di profondità tra i -90 e i -150 m, che non ha subito trasporto. La successione si è deposta nell’Emiliano sui Calcari di Castro, in un clima temperato caldo. - SEZIONE B – E’ più recente (Siciliano) e costituisce una successione clinostratificata con evidenti segni di rimaneggiamento, connessa ad ambienti di profondità minore (da –50 a -90 m), in cui proliferavano associazioni di tipo foramol. Questi risultati confermano l’ipotesi di Tropeano et alii (2004) che li ritengono depositi di scarpata e di base di scarpata sottomarina
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