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<br /> <br />-17- <br /> <br /> Network Vector <br />. <br /> 0 2 0 1 0 1 0 1 0 1 <br /> 2 2 0 1 0 2 0 1 1 0 <br />. <br /> 2 1 0 1 1 0 1 1 1 2 <br /> 2 0 1 0 1 1 1 2 0 0 <br /> 2 1 2 2 1 2 0 1 0 1 <br /> 1 1 2 0 1 1 2 0 1 2 <br /> 1 2 1 0 1 0 1 0 1 0 <br /> 2 0 1 2 0 1 0 0 1 1 <br /> 0 2 1 2 2 1 2 <br /> <br />Stream <br /> <br />Orders <br /> <br />1 st <br />2nd <br />3rd <br />4th <br /> <br />FIGURE 4. Drainage network of the Neponset basin. <br /> <br />and terraces typically display pronounced breaks in slope and occupy <br />particular locations in the terrain, whereas till generally produces <br />more subdued landforms and slope elements. In retrospect, total reli- <br />ance on landform interpretation might have been preferable for the sake <br />of uniformity. Nevertheless, it was used in a complementary fashion <br /> <br />with available geologic maps in the study. Limited verification of this <br />