. Harmony : a course of study . 107. This chord is not used for the present for harmonizing purposes,but will be considered later on under chromatic passing tones. The submediant is a major triad, the parallel of the subdominant. Note. The root of the submediant in major is frequently doubled, but in minornever if preceded or succeeded by the dominant. 108. The leading tone triad is also diminished, and coincides with theleading tone of the tonic major triad, being in fact the third, fifth, andseventh of a dominant seventh chord. Both diminished triads aremore frequently used in their first in
. Harmony : a course of study . 107. This chord is not used for the present for harmonizing purposes,but will be considered later on under chromatic passing tones. The submediant is a major triad, the parallel of the subdominant. Note. The root of the submediant in major is frequently doubled, but in minornever if preceded or succeeded by the dominant. 108. The leading tone triad is also diminished, and coincides with theleading tone of the tonic major triad, being in fact the third, fifth, andseventh of a dominant seventh chord. Both diminished triads aremore frequently used in their first inversions, usually with the thirdor fifth doubled, than in the fundamental HARMONY. Si etc. I 5±$=j=W %E_=l 1 The root of the supertonic triad is more frequently doubled, how-ever, than that of the leading tone. The rules for the use of thesechords are the same as in Lessons X, XI, XII, and XIII. EXERCISES TO LESSON XV. m^mmmw^m ^m 3RE ^ap^ i=t n°6 VI n°« vn°« P &d t=4 1 r ■^<- q» M -S- » l z=i- 3 T= K 1. Figured bass given,6 6 6Q 6 6 7 3 C*# h ^ i *-).. 17 fS r f* — 1 1 -y u u q <^j ! O ! 1 m LJ 1 u_ ^ —d I—&-• . a ^ 6p II 3fcS -ffl- SE^e p jO. 56 6 6 7 4 7 6 4 5 6 54 3 6 Ptf 6 7 ^^E[7/f37iSB^W^£^B 5* HARMONY. /3. Unfigured bass. m&& t=t SL &—g*- 4. Melody given H 5 l|EiE^prfSi *=«: t=t *=4 V=± =t33l» II bfcg ^^^^g^^^^^^^^^^^ P=p: f=±«=p=^Ei==tf=f=E:f=5=FEE3==rz3^3=^=f ti^i^§!L=z=z^^bL^^r~^^ LESSON XVI. SUMMARY. We have now considered all the triads that it is possible to erectupon the various degrees of the major and minor scales, with theirfirst and second inversions. The following table gives a s
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