SKU: AP.47402
UPC: 038081547817. English.
Energetic and fast-paced, this musical burst of energy is a perfect choice for a concert or contest opener or as an encore on any program. Attention to vivid dynamic contrasts, punctuating articulations, and, of course, rhythmic clarity will ensure success. A fanfare-style original that will draw acclaim! (2:00) This title is available in MakeMusic Cloud.
SKU: AP.47402S
UPC: 038081547824. English.
Energetic and fast-paced, this musical burst of energy is a perfect choice for a concert or contest opener or as an encore on any program. Attention to vivid dynamic contrasts, punctuating articulations, and, of course, rhythmic clarity will ensure success. A fanfare-style original that will draw acclaim! (2:00) This title available in MakeMusic Cloud.
SKU: CF.CAS7
ISBN 9780825847578. UPC: 798408047573. 8.5 X 11 inches. Key: D major.
When you have the good fortune to visit Red Rock country in the southwestern United States, you will all at once feel that majesty and beauty in the towering red landscape. You can trek, bike, paddle, ride horseback or drive through the canyons, past the strangely shaped rocks and over the enormous boulders. Each time you turn a corner you will be dazzled by yet another magnificent vista. The Red Rock areas in Utah, Nevada, Arizona and New Mexico formed millions of years ago when that part of North America was primarily under water. The water left behind the shells and skeletons of sea creatures that gradually turned into limestone and similar rocks. Beginning 225 million years ago, the earth's crust began to move and the seabed slowly rose. Streams entering the shallow water deposited mud and sand that turned into shale and marine sandstone. As the land continued to rise and dry out, some of the rocks oxidized (combined with oxygen) and turned red in color. Subsequently the area was covered with sands that eventually compressed into what is called Aztec sandstone. Sometimes, when iron was concentrated in the rock, the sandstone turned a bright red color. Following the introduction, the music in Red Rock Rag takes on a typical ragtime melody and rhythm. It then transitions by changing key, time signature and the structure into a swing waltz. At m. 60, it moves into a combined time signature of one measure of 3/4 time and two measures of 2/4 time with an occasional lick in the bass line. Finally, it moves back into the swing-waltz style and finishes with the original ragtime melody. Red Rock Rag is challenging stylistically and rhythmically. It would be appropriate to study both the ragtime and swing styles while working on it.When you have the good fortune to visit Red Rock country in the southwestern United States, you will all at once feel that majesty and beauty in the towering red landscape. You can trek, bike, paddle, ride horseback or drive through the canyons, past the strangely shaped rocks and over the enormous boulders. Each time you turn a corner you will be dazzled by yet another magnificent vista. The Red Rock areas in Utah, Nevada, Arizona and New Mexico formed millions of years ago when that part of North America was primarily under water. The water left behind the shells and skeletons of sea creatures that gradually turned into limestone and similar rocks. Beginning 225 million years ago, the earth's crust began to move and the seabed slowly rose. Streams entering the shallow water deposited mud and sand that turned into shale and marine sandstone. As the land continued to rise and dry out, some of the rocks oxidized (combined with oxygen) and turned red in color. Subsequently the area was covered with sands that eventually compressed into what is called Aztec sandstone. Sometimes, when iron was concentrated in the rock, the sandstone turned a bright red color. Following the introduction, the music in Red Rock Rag takes on a typical ragtime melody and rhythm. It then transitions by changing key, time signature and the structure into a swing waltz. At m. 60, it moves into a combined time signature of one measure of 3/4 time and two measures of 2/4 time with an occasional lick in the bass line. Finally, it moves back into the swing-waltz style and finishes with the original ragtime melody.A Red Rock RagA is challenging stylistically and rhythmically. It would be appropriate to study both the ragtime and swing styles while working on it.When you have the good fortune to visit Red Rock country in the southwestern United States, you will all at once feel that majesty and beauty in the towering red landscape. You can trek, bike, paddle, ride horseback or drive through the canyons, past the strangely shaped rocks and over the enormous boulders. Each time you turn a corner you will be dazzled by yet another magnificent vista. The Red Rock areas in Utah, Nevada, Arizona and New Mexico formed millions of years ago when that part of North America was primarily under water. The water left behind the shells and skeletons of sea creatures that gradually turned into limestone and similar rocks. Beginning 225 million years ago, the earth's crust began to move and the seabed slowly rose. Streams entering the shallow water deposited mud and sand that turned into shale and marine sandstone. As the land continued to rise and dry out, some of the rocks oxidized (combined with oxygen) and turned red in color. Subsequently the area was covered with sands that eventually compressed into what is called Aztec sandstone. Sometimes, when iron was concentrated in the rock, the sandstone turned a bright red color. Following the introduction, the music in Red Rock Rag takes on a typical ragtime melody and rhythm. It then transitions by changing key, time signature and the structure into a swing waltz. At m. 60, it moves into a combined time signature of one measure of 3/4 time and two measures of 2/4 time with an occasional lick in the bass line. Finally, it moves back into the swing-waltz style and finishes with the original ragtime melody.A Red Rock RagA is challenging stylistically and rhythmically. It would be appropriate to study both the ragtime and swing styles while working on it.When you have the good fortune to visit Red Rock country in the southwestern United States, you will all at once feel that majesty and beauty in the towering red landscape. You can trek, bike, paddle, ride horseback or drive through the canyons, past the strangely shaped rocks and over the enormous boulders. Each time you turn a corner you will be dazzled by yet another magnificent vista. The Red Rock areas in Utah, Nevada, Arizona and New Mexico formed millions of years ago when that part of North America was primarily under water. The water left behind the shells and skeletons of sea creatures that gradually turned into limestone and similar rocks. Beginning 225 million years ago, the earth's crust began to move and the seabed slowly rose. Streams entering the shallow water deposited mud and sand that turned into shale and marine sandstone. As the land continued to rise and dry out, some of the rocks oxidized (combined with oxygen) and turned red in color. Subsequently the area was covered with sands that eventually compressed into what is called Aztec sandstone. Sometimes, when iron was concentrated in the rock, the sandstone turned a bright red color. Following the introduction, the music in Red Rock Rag takes on a typical ragtime melody and rhythm. It then transitions by changing key, time signature and the structure into a swing waltz. At m. 60, it moves into a combined time signature of one measure of 3/4 time and two measures of 2/4 time with an occasional lick in the bass line. Finally, it moves back into the swing-waltz style and finishes with the original ragtime melody. Red Rock Rag is challenging stylistically and rhythmically. It would be appropriate to study both the ragtime and swing styles while working on it.When you have the good fortune to visit Red Rock country in the southwestern United States, you will all at once feel that majesty and beauty in the towering red landscape. You can trek, bike, paddle, ride horseback or drive through the canyons, past the strangely shaped rocks and over the enormous boulders. Each time you turn a corner you will be dazzled by yet another magnificent vista. The Red Rock areas in Utah, Nevada, Arizona and New Mexico formed millions of years ago when that part of North America was primarily under water. The water left behind the shells and skeletons of sea creatures that gradually turned into limestone and similar rocks. Beginning 225 million years ago, the earth's crust began to move and the seabed slowly rose. Streams entering the shallow water deposited mud and sand that turned into shale and marine sandstone. As the land continued to rise and dry out, some of the rocks oxidized (combined with oxygen) and turned red in color. Subsequently the area was covered with sands that eventually compressed into what is called Aztec sandstone. Sometimes, when iron was concentrated in the rock, the sandstone turned a bright red color. Following the introduction, the music in Red Rock Rag takes on a typical ragtime melody and rhythm. It then transitions by changing key, time signature and the structure into a swing waltz. At m. 60, it moves into a combined time signature of one measure of 3/4 time and two measures of 2/4 time with an occasional lick in the bass line. Finally, it moves back into the swing-waltz style and finishes with the original ragtime melody. Red Rock Rag is challenging stylistically and rhythmically. It would be appropriate to study both the ragtime and swing styles while working on it.When you have the good fortune to visit Red Rock country in the southwestern United States, you will all at once feel that majesty and beauty in the towering red landscape. You can trek, bike, paddle, ride horseback or drive through the canyons, past the strangely shaped rocks and over the enormous boulders. Each time you turn a corner you will be dazzled by yet another magnificent vista.The Red Rock areas in Utah, Nevada, Arizona and New Mexico formed millions of years ago when that part of North America was primarily under water. The water left behind the shells and skeletons of sea creatures that gradually turned into limestone and similar rocks. Beginning 225 million years ago, the earth's crust began to move and the seabed slowly rose. Streams entering the shallow water deposited mud and sand that turned into shale and marine sandstone. As the land continued to rise and dry out, some of the rocks oxidized (combined with oxygen) and turned red in color. Subsequently the area was covered with sands that eventually compressed into what is called Aztec sandstone. Sometimes, when iron was concentrated in the rock, the sandstone turned a bright red color.Following the introduction, the music in Red Rock Rag takes on a typical ragtime melody and rhythm. It then transitions by changing key, time signature and the structure into a swing waltz. At m. 60, it moves into a combined time signature of one measure of 3/4 time and two measures of 2/4 time with an occasional lick in the bass line. Finally, it moves back into the swing-waltz style and finishes with the original ragtime melody. Red Rock Rag is challenging stylistically and rhythmically. It would be appropriate to study both the ragtime and swing styles while working on it.
SKU: HL.49046544
ISBN 9781705122655. UPC: 842819108726. 9.0x12.0x0.224 inches.
I composed the Piano Concerto in two stages: the first three movements during the years 1985-86, the next two in 1987, the final autograph of the last movement was ready by January, 1988. The concerto is dedicated to the American conductor Mario di Bonaventura. The markings of the movements are the following: 1. Vivace molto ritmico e preciso 2. Lento e deserto 3. Vivace cantabile 4. Allegro risoluto 5. Presto luminoso.The first performance of the three-movement Concerto was on October 23rd, 1986 in Graz. Mario di Bonaventura conducted while his brother, Anthony di Bonaventura, was the soloist. Two days later the performance was repeated in the Vienna Konzerthaus. After hearing the work twice, I came to the conclusion that the third movement is not an adequate finale; my feeling of form demanded continuation, a supplement. That led to the composing of the next two movements. The premiere of the whole cycle took place on February 29th, 1988, in the Vienna Konzerthaus with the same conductor and the same pianist. The orchestra consisted of the following: flute, oboe, clarinet, bassoon, horn, trumpet, tenor trombone, percussion and strings. The flautist also plays the piccoIo, the clarinetist, the alto ocarina. The percussion is made up of diverse instruments, which one musician-virtuoso can play. It is more practical, however, if two or three musicians share the instruments. Besides traditional instruments the percussion part calls also for two simple wind instruments: the swanee whistle and the harmonica. The string instrument parts (two violins, viola, cello and doubles bass) can be performed soloistic since they do not contain divisi. For balance, however, the ensemble playing is recommended, for example 6-8 first violins, 6-8 second, 4-6 violas, 4-6 cellos, 3-4 double basses. In the Piano Concerto I realized new concepts of harmony and rhythm. The first movement is entirely written in bimetry: simultaneously 12/8 and 4/4 (8/8). This relates to the known triplet on a doule relation and in itself is nothing new. Because, however, I articulate 12 triola and 8 duola pulses, an entangled, up till now unheard kind of polymetry is created. The rhythm is additionally complicated because of asymmetric groupings inside two speed layers, which means accents are asymmetrically distributed. These groups, as in the talea technique, have a fixed, continuously repeating rhythmic structures of varying lengths in speed layers of 12/8 and 4/4. This means that the repeating pattern in the 12/8 level and the pattern in the 4/4 level do not coincide and continuously give a kaleidoscope of renewing combinations. In our perception we quickly resign from following particular rhythmical successions and that what is going on in time appears for us as something static, resting. This music, if it is played properly, in the right tempo and with the right accents inside particular layers, after a certain time 'rises, as it were, as a plane after taking off: the rhythmic action, too complex to be able to follow in detail, begins flying. This diffusion of individual structures into a different global structure is one of my basic compositional concepts: from the end of the fifties, from the orchestral works Apparitions and Atmospheres I continuously have been looking for new ways of resolving this basic question. The harmony of the first movement is based on mixtures, hence on the parallel leading of voices. This technique is used here in a rather simple form; later in the fourth movement it will be considerably developed. The second movement (the only slow one amongst five movements) also has a talea type of structure, it is however much simpler rhythmically, because it contains only one speed layer. The melody is consisted in the development of a rigorous interval mode in which two minor seconds and one major second alternate therefore nine notes inside an octave. This mode is transposed into different degrees and it also determines the harmony of the movement; however, in closing episode in the piano part there is a combination of diatonics (white keys) and pentatonics (black keys) led in brilliant, sparkling quasimixtures, while the orchestra continues to play in the nine tone mode. In this movement I used isolated sounds and extreme registers (piccolo in a very low register, bassoon in a very high register, canons played by the swanee whistle, the alto ocarina and brass with a harmon-mute' damper, cutting sound combinations of the piccolo, clarinet and oboe in an extremely high register, also alternating of a whistle-siren and xylophone). The third movement also has one speed layer and because of this it appears as simpler than the first, but actually the rhythm is very complicated in a different way here. Above the uninterrupted, fast and regular basic pulse, thanks to the asymmetric distribution of accents, different types of hemiolas and inherent melodical patterns appear (the term was coined by Gerhard Kubik in relation to central African music). If this movement is played with the adequate speed and with very clear accentuation, illusory rhythmic-melodical figures appear. These figures are not played directly; they do not appear in the score, but exist only in our perception as a result of co-operation of different voices. Already earlier I had experimented with illusory rhythmics, namely in Poeme symphonique for 100 metronomes (1962), in Continuum for harpsichord (1968), in Monument for two pianos (1976), and especially in the first and sixth piano etude Desordre and Automne a Varsovie (1985). The third movement of the Piano Concerto is up to now the clearest example of illusory rhythmics and illusory melody. In intervallic and chordal structure this movement is based on alternation, and also inter-relation of various modal and quasi-equidistant harmony spaces. The tempered twelve-part division of the octave allows for diatonical and other modal interval successions, which are not equidistant, but are based on the alternation of major and minor seconds in different groups. The tempered system also allows for the use of the anhemitonic pentatonic scale (the black keys of the piano). From equidistant scales, therefore interval formations which are based on the division of an octave in equal distances, the twelve-tone tempered system allows only chromatics (only minor seconds) and the six-tone scale (the whole-tone: only major seconds). Moreover, the division of the octave into four parts only minor thirds) and three parts (three major thirds) is possible. In several music cultures different equidistant divisions of an octave are accepted, for example, in the Javanese slendro into five parts, in Melanesia into seven parts, popular also in southeastern Asia, and apart from this, in southern Africa. This does not mean an exact equidistance: there is a certain tolerance for the inaccurateness of the interval tuning. These exotic for us, Europeans, harmony and melody have attracted me for several years. However I did not want to re-tune the piano (microtone deviations appear in the concerto only in a few places in the horn and trombone parts led in natural tones). After the period of experimenting, I got to pseudo- or quasiequidistant intervals, which is neither whole-tone nor chromatic: in the twelve-tone system, two whole-tone scales are possible, shifted a minor second apart from each other. Therefore, I connect these two scales (or sound resources), and for example, places occur where the melodies and figurations in the piano part are created from both whole tone scales; in one band one six-tone sound resource is utilized, and in the other hand, the complementary. In this way whole-tonality and chromaticism mutually reduce themselves: a type of deformed equidistancism is formed, strangely brilliant and at the same time slanting; illusory harmony, indeed being created inside the tempered twelve-tone system, but in sound quality not belonging to it anymore. The appearance of such slantedequidistant harmony fields alternating with modal fields and based on chords built on fifths (mainly in the piano part), complemented with mixtures built on fifths in the orchestra, gives this movement an individual, soft-metallic colour (a metallic sound resulting from harmonics). The fourth movement was meant to be the central movement of the Concerto. Its melodc-rhythmic elements (embryos or fragments of motives) in themselves are simple. The movement also begins simply, with a succession of overlapping of these elements in the mixture type structures. Also here a kaleidoscope is created, due to a limited number of these elements - of these pebbles in the kaleidoscope - which continuously return in augmentations and diminutions. Step by step, however, so that in the beginning we cannot hear it, a compiled rhythmic organization of the talea type gradually comes into daylight, based on the simultaneity of two mutually shifted to each other speed layers (also triplet and duoles, however, with different asymmetric structures than in the first movement). While longer rests are gradually filled in with motive fragments, we slowly come to the conclusion that we have found ourselves inside a rhythmic-melodical whirl: without change in tempo, only through increasing the density of the musical events, a rotation is created in the stream of successive and compiled, augmented and diminished motive fragments, and increasing the density suggests acceleration. Thanks to the periodical structure of the composition, always new but however of the same (all the motivic cells are similar to earlier ones but none of them are exactly repeated; the general structure is therefore self-similar), an impression is created of a gigantic, indissoluble network. Also, rhythmic structures at first hidden gradually begin to emerge, two independent speed layers with their various internal accentuations. This great, self-similar whirl in a very indirect way relates to musical associations, which came to my mind while watching the graphic projection of the mathematical sets of Julia and of Mandelbrot made with the help of a computer. I saw these wonderful pictures of fractal creations, made by scientists from Brema, Peitgen and Richter, for the first time in 1984. From that time they have played a great role in my musical concepts. This does not mean, however, that composing the fourth movement I used mathematical methods or iterative calculus; indeed, I did use constructions which, however, are not based on mathematical thinking, but are rather craftman's constructions (in this respect, my attitude towards mathematics is similar to that of the graphic artist Maurits Escher). I am concerned rather with intuitional, poetic, synesthetic correspondence, not on the scientific, but on the poetic level of thinking. The fifth, very short Presto movement is harmonically very simple, but all the more complicated in its rhythmic structure: it is based on the further development of ''inherent patterns of the third movement. The quasi-equidistance system dominates harmonically and melodically in this movement, as in the third, alternating with harmonic fields, which are based on the division of the chromatic whole into diatonics and anhemitonic pentatonics. Polyrhythms and harmonic mixtures reach their greatest density, and at the same time this movement is strikingly light, enlightened with very bright colours: at first it seems chaotic, but after listening to it for a few times it is easy to grasp its content: many autonomous but self-similar figures which crossing themselves. I present my artistic credo in the Piano Concerto: I demonstrate my independence from criteria of the traditional avantgarde, as well as the fashionable postmodernism. Musical illusions which I consider to be also so important are not a goal in itself for me, but a foundation for my aesthetical attitude. I prefer musical forms which have a more object-like than processual character. Music as frozen time, as an object in imaginary space evoked by music in our imagination, as a creation which really develops in time, but in imagination it exists simultaneously in all its moments. The spell of time, the enduring its passing by, closing it in a moment of the present is my main intention as a composer. (Gyorgy Ligeti).
SKU: HL.14021749
ISBN 9788759889817. Danish.
Poul Ruders' MONODRAMA, dedicated to percussion virtuoso Gert Sorensen and commissioned by The Danish Radio, was written in New York in the early winter 1988 and makes the centre as well as the middle of the tri-part opus called The Drama Trilogy. All three works employ the word Drama in their title, Drama in the original meaning of the word: event. No specified event, but a premonition or omen rather, that something is afoot, a free Drama-offer from which anyone may populate the stage of his private, inner theatre.The first piece of the series DRAMAPHONIA for piano and chamber ensemble was premiered in London in the spring of 1988 by Lontano and Poul Rosenbaum. This piece is emotionally and rhythmically unstable as opposed to MONODRAMA (single-event) which is modelled from the archetypal idea of obtaining accomplishment from nothingness. The 31 instruments of the orchestra (no flutes and no violins or violas) are more or less wrapped around the solo-part to become one with that and thus emerge as one, gigantic percussion instrument. The rhythmical patterns of the orchestral part more or less follow those of the percussionpart, a single-event also on the rhythmical level.After 20 minutes climbing toward the peak of rage, the composition casts its slough and is reborn into a chorale-like march and the struggle between totally depopulated sound-scapes and ferociously roaring sub-oceanic storms begin and the piece paces toward the abyss; rage becomes despondency, New Rage as opposed to New Age, the spineless worshipper of beauty without pain.The third instalment of the DRAMA TRILOGY, the cello concerto POLYDRAMA will be premiered in Stockholm May 1990.MONODRAMA lasts aprox. 32 minutes.Poul Ruders.
SKU: HL.14041525
ISBN 9788759871829. UPC: 196288071020. 9.5x14.25x0.167 inches. Danish-English.
Programme Note During the composition of my tenth string quartet a flower-name, host-tidlos, came to my mind - and it would not me leave again. [hosttidlos is actually autumn crocus in English, but the composer prefers harvest-timeless, to maintain some of the associations of the Danish flower-name, red.] The paradoxical union of a seasonal time (harvest) and no-time-at-all was a good fit to the sections of the work that I had composed at that time, and I decided to tentatively stick to that title for the work-in-progress, and now, having finished the piece, I can say that is is still a fitting title - and it stands. Enough about the title, I will go on to describe themusic, a somewhat more precarious project. My tenth string quartet is probably the most basic string quartet that I have composed: melodically - and in sound - it employs the naturally based overtones and undertones (perceived at major and minor, respectively), and rhythmically it is based on growth, on the principles of the Golden Section, and the structure itself contrasts abundance and exuberance with sections of immobility and contemplation. However, Melos, melody, is definitely the dominating aspect of my STRING QUARTET NO. 10: behind even the most rhythmically complex or pure sonoric sections lies a firm - if hidden - basis of melodic or polyphonic ideas. The work was composed in 2004-2005 for the Kroger Quartet.
SKU: PR.446413390
UPC: 680160667383. 9 x 12 inches.
Concertino is about relationships and how they change over time. My first goal in writing the piece was to create two distinct characters, in this case the Oboe and English Horn. The Oboe begins with a berceuse-like melody, while the English Horn's entrance is more ambiguous and rhythmically jagged. Over the course of the piece, these two characters interact through a variety of musical settings, their material or personalities continually developing. The strings, more than mere accompaniment, provide commentary on the dramatic action, much like a Greek chorus. They establish each musical scene, interact with the two woodwinds, and further develop the musical material. And while there is a strong concertante element in the piece, it is essentially chamber music. There is a conversational quality, a sense of give-and-take between everyone involved that makes the two woodwinds first among equals as opposed to featured concert soloists. Each of the eight instruments has something unique and important to say.Concertino is about relationships and how they change over time. My first goal in writing the piece was to create two distinct characters, in this case the Oboe and English Horn. The Oboe begins with a berceuse-like melody, while the English Horn’s entrance is more ambiguous and rhythmically jagged. Over the course of the piece, these two characters interact through a variety of musical settings, their material or personalities continually developing.The strings, more than mere accompaniment, provide commentary on the dramatic action, much like a Greek chorus. They establish each musical scene, interact with the two woodwinds, and further develop the musical material. And while there is a strong concertante element in the piece, it is essentially chamber music. There is a conversational quality, a sense of give-and-take between everyone involved that makes the two woodwinds first among equals as opposed to featured concert soloists. Each of the eight instruments has something unique and important to say.
SKU: AP.1-ADV8415
UPC: 805095084153. English. Traditional.
In writing these arrangements for clarinet quartet, Frank Reinshagen has created little masterpieces, which broaden the rhythmical and harmonic context of the original tunes in an interesting manner without detracting from their archaic and melancholic character. These original tunes are---in a direct or wider sense---of Celtic origin. In other words, they have been borrowed from the Irish, Scottish, and Gaelic musical tradition. These through-composed arrangements are rather easy to perform from the rhythmical and technical point of view. Yet, they are quite demanding in respect of the key they are written in, their intonation, and especially, their interpretation. Their different instrumentations are fully compatible with each other and, due to their overall structure, they are also suitable to be played with multi-scored parts. Annotation on Aignish on the Machair: The arrangement of Aignish on the Machair, Folksong from The Hebrides, illustrates, above all, the melancholic character inherent in the harmonies of the original tune. A short rubato passage is followed by several variations over the flowing melody in 3/4-time. The short triplet passages embedded in these variations are quite demanding from the technical point of view; considering the key they are written in, however, these passages are not too difficult to play.
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