Inland, along the whole northern bank of the Plata, I saw, besides modern tertiary beds, only one small patch of slightly metamorphosed rock, which alone could have formed a part of the original capping of the granitic series.
Lur barruan, Plata ibaiaren iparralde guztian zehar, tertziarioko geruza modernoz gain, harri arinki metamorfikozko unadatxo bat besterik ez nuen ikusi, harriok serie granitikoaren jatorrizko estalkiaren zati izan zitezkeelarik.