Streams

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: CF.CAS113F

ISBN 9781491151693. UPC: 680160909193. 9 x 12 inches.

Composed by Bruce W. Tippette, Drifting?utilizes musical passages to allude to the image of something drifting down a river in the woods. It journeys through twists and turns, placid streams and roaring rapids, eventually making a grand entrance into open waters.
The musical passages in this piece for string orchestra conjure images of something, perhaps a leaf, gently drifting down a river in the woods. It journeys through twists and turns, placid streams and roaring rapids, eventually making a grand entrance into open waters. As Drifting opens, soft pizzicato strings are uttered in the lower string voices, while the upper voices slowly swell into the appearance of the main motive in m. 9. This theme develops and passes through several voices until being replaced by a new motive in m. 36, accompanied by driving rhythms and frequent modulations. A powerful resurgence of the original motive occurs in m. 60. Melodic remnants of the previous sections are presented in a new fashion as the piece comes to a dramatic close with all voices playing in rhythmic unison in the closing measures..
The musical passages in this piece for string orchestra conjure images of something, perhaps a leaf, gently drifting down a river in the woods. It journeys through twists and turns, placid streams and roaring rapids, eventually making a grand entrance into open waters. As Drifting opens, soft pizzicato strings are uttered in the lower string voices, while the upper voices slowly swell into the appearance of the main motive in m. 9. This theme develops and passes through several voices until being replaced by a new motive in m. 36, accompanied by driving rhythms and frequent modulations. A powerful resurgence of the original motive occurs in m. 60. Melodic remnants of the previous sections are presented in a new fashion as the piece comes to a dramatic close with all voices playing in rhythmic unison in the closing measures..
The musical passages in this piece for string orchestra conjure images of something, perhaps a leaf, gently drifting down a river in the woods. It journeys through twists and turns, placid streams and roaring rapids, eventually making a grand entrance into open waters. As Drifting opens, soft pizzicato strings are uttered in the lower string voices, while the upper voices slowly swell into the appearance of the main motive in m. 9. This theme develops and passes through several voices until being replaced by a new motive in m. 36, accompanied by driving rhythms and frequent modulations. A powerful resurgence of the original motive occurs in m. 60. Melodic remnants of the previous sections are presented in a new fashion as the piece comes to a dramatic close with all voices playing in rhythmic unison in the closing measures.

About Carl Fischer Concert String Orchestra Series

This series of pieces (Grade 3 and higher) is designed for advancing ensembles. The pieces in this series are characterized by:

• Expanded use of rhythms, ranges and keys but technical demands are still carefully considered
• More comprehensive bowing techniques
• Viola T.C. included
• Careful selection of keys and degree of difficulty for advancing musicians

SKU: AY.FC3274PM

ISBN 9790543572638.

Relic radiation is in a sense equivalent to time stream. It is the first link on the reaction of hydrogen's synthesis. The basic energy is connected with thermonuclear reaction, and these ones arise at the expense of interaction with relic radiation which is the time stream. There is a question about the transformation of time into energy and simultaneously with this, it is possible to qualify the relic radiation as a time's carrier, the physics of the relict. Each line of a flute means a separate fragment of a relic radiation stream. The organ means an integral sounding of incorporated streams. The development is an interaction of relic radiation streams taken from different intervals of time.

SKU: BT.GOB-000917-010

Trimbeka can be translated as “three streams,” and refers to the streams that once flowed around a market town in Holland called Georredijk. Opening with the sinister sounds of the moorland on the edge of the town, we then hear the hustle and bustle of the market itself. A slower middle section is an ode to the beautiful surrounding scenery.

Trimbeka. Dat is de historische naam van de Noord-Nederlandse plaats Gorredijk. In het gebied rondom Gorredijk stroomden vroeger drie beken, Trimbeets of wel Trimbeka. Wittrock verwoordt muzikaal de levendigheid van het dorp,de onheilspellendheid van het nabijgelegen moeras en de vrolijkheid van de jaarlijkse markt. Hij schreef dit fascinerende werk ter gelegenheid van het jubileum van muziekvereniging De Vlecke in Gorredijk.

Der Titel Trimbeka erinnert an den alten Namen des heutigen Dorfes Gorredijk in Holland, das dieses Werk in Auftrag gab. Trimbeka bedeutet so viel wie drei Bäche“, die einst rund um den Ort flossen. Außerdem lag der Ort an einer wichtigen Wegkreuzung und war damit Marktort. Nach unheilvollen Klängen, die von der Moorlandschaft am Rande des Dorfes zeugen, ist die Geschäftigkeit des Marktes zu hören. Der langsame Mittelteil ist eine Ode an die schöne Landschaft.

Trimbeka est une composition qui doit son existence la date anniversaire de l’Orchestre d’Harmonie de Vlecke (Gorredijk - Pays-Bas). Autrefois, Gorredijk était une ville florissante, un grand village vivifiant, situé au carrefour d’importantes routes de liaisons. Des sons inquiétants font allusions aux dangers des tourbières et des marécageux qui parcourent la région, tandis que résonne des rires et cris de joies : la foire annuelle ouvre ses portes. Le mouvement central lent est une ode la beauté du paysage entourant le village.

Trimbeka è l’antico nome della cittadina di Gorredijk (Olanda), che ha commissionato il brano. Trimbeka significa “tre ruscelli”, che scorrevano nelle vicinanze della localit . La posizione di Gorredijk erano molto strategica e punto d’incontro dei commerci. La musica è all’inizio vivace, nel segno delle attivit degli abitanti cittadini. La parte centrale, caratterizzata da musica più lenta, è un’ode allo splendido paesaggio di questa parte dell’Olanda.

SKU: CF.O4804

ISBN 9780825806247. UPC: 680160913114.

SKU: FT.FM275

ISBN 9790570481743.

Flute and Piano. This is a mini suite for Flute and Piano with rainy and sad Autumn; frosty and calm Winter; melting snow, streams, awakening of nature in Spring; funny and jazzy Summer. Autumn was a mandatory piece at Moscow 2012 International Children’s Competition My Favorite Flute.

SKU: TM.05325CHS

Banda = 2 tpt,snare. P/C not in set.

SKU: MN.56-0108

UPC: 688670221255. English, Latin. Psalms 142; Jeremiah 3:48, 52, 56.

Invictus: A Passion addresses one of the world’s most powerful stories through the lens of the modern world. The texts, written or inspired by women, describe not only human suffering and persecution but also the human capacity for love and humility in the face of tyranny. Composer Howard Goodall is uniquely suited to bring these texts to life with music of emotional clarity and sweeping force. This excerpt is scored for soprano solo, SATB choir and piano. This fourth movement of the larger work is inspired by the extraordinary story of Irena Sendler née Krzyżanowska, a Polish nurse and head of Żegota, the Polish Council to Aid Jews in the Second World War, whose personal interventions saved the lives of approximately 2,500 Jewish children in the Warsaw Ghetto, smuggling them to safety, acts of humanitarian bravery that eventually caused her arrest and torture by the Gestapo. She is honoured as Righteous Amongst the Nations at Yad Vashem, Jerusalem. The Latin texts of this movement are taken from the Book of Lamentations (“My eye hath run down with streams of water, for the destruction of the daughter of my people. My enemies have chased me and caught me like a bird, without cause…”) and from Psalm 142, the Old Testament being the meeting-point of Sendler’s Catholicism and the Jewish tradition of those whose lives she saved. Duration 6:19.

SKU: MN.50-4069

UPC: 688670540691. English. Psalm 42:1-2; 43:3-4.

A flowing and soothing setting of Psalm 42. Appropriate for use in Easter Vigil services or many other times throughout the year.

SKU: BR.EOS-20472-19

Today, it is hard to believe that Bedrich Smetana kept receiving rejections when he tried to get his enormously popular Moldau printed.

ISBN 9790004184974. 10 x 12.5 inches.

What is also amazing is that the first text-critical edition prepared by the Czech Smetana expert Milan Pospisil in 1999, which had entailed an exhaustive evaluation of the sources and been given a full text-critical editorial treatment as a Eulenburg study score, had no resonance of any kind among performers since no performance material had been published. After 15 years, Pospisils edition is finally being completed in a manner suitable for practice: with a conducting score and orchestral parts which will ensure that all future performances are based on a musical text that is as reliable as can be.

The work depicts the course of the river Vltava, beginning with its first two sources, the cold and warm Vltava, and the confluence of the two streams that join to form a single river; then the course of the Vltava through forests and meadows, and through open countryside where a peasant wedding is being celebrated; water-sprites dance by the light of the moon; on the nearby cliffs castles, mansions and ruins rise proudly into the air; the Vltava eddies in the St John's Rapids, then flows in a broad stream as it continues its course towards Prague, where the Vysehrad appears, before the river finally disappears into the distance as it flows majestically into the Elbe.

Vltava (The Moldau), Smetana's best-known and most frequently performed orchestral work, was written between 19 November and 8 December 1874, at a time when Smetana was already completely deaf. The world premiere took place in Prague on 4 April 1875, but the score was not published until 1880.

SKU: MN.50-4069A

UPC: 688670008931.