Orchestra String Orchestra - Grade 3

SKU: CF.CAS7

Composed by Doris Gazda. Edited by Amy Rosen. FS-SWs. Carl Fischer Concert String Orchestra Series. Score and Parts. With Standard notation. 20+24+24+6+15+15+15 pages. Carl Fischer Music #CAS7. Published by Carl Fischer Music (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.

Concert Band/Harmonie - Grade 3

SKU: BT.DHP-1196201-140

Composed by Thierry Deleruyelle. Concert and Contest Collection CBHA. Concert Piece. Score Only. Composed 2019. 31 pages. De Haske Publications #DHP 1196201-140. Published by De Haske Publications (BT.DHP-1196201-140).

English-German-French-Dutch.

Golden Peak is a concert piece that takes us deep into the world of volcanoes of the Auvergne in central France. They are dormant volcanoes whose origins date back from 7,000 to over 65 million years ago. Among the most well-known are the 80 volcanoes of the Chaîne des Puys, a spectacular natural environment ranking among the most fascinating landscapes in the world. The title of this dynamic and rhythmic piece is a reference to the local spa town of Mont-Dore and calls upon all sections of the orchestra. The central theme is very mellow yet riveting and the music depicts both the dynamism and tranquillity of the region.

Golden Peak is een concertwerk dat ons meeneemt naar een vulkanische wereld: die van de Auvergne in het midden van Frankrijk. De vulkanen daar zijn slapende; hun oorsprong gaat terug naar 7000 tot meer dan 65 miljoen jaar geleden. Tot de bekendste behoren de tachtig vulkanen van de Chaîne des Puys, een uniek natuurgebied dat tot de boeiendste landschappen van de wereld behoort. De titel van deze dynamische en ritmische compositie verwijst naar de plaats Mont-Dore aldaar. Het werk doet een beroep op alle secties in het orkest. Het centrale thema is mild en tegelijk meeslepend, en verder beschrijft de muziek zowel de vitaliteit als de rust van de streek.

Golden Peak ist ein Konzertstück, das uns tief in die Welt der Vulkane in der Auvergne in Mittelfrankreich entführt. Es handelt sich um erloschene Vulkane, deren Ursprünge zwischen 7.000 bis 65 Millionen Jahren vor unserer Zeit liegen. Zu den bekanntesten gehören die 80 Vulkane der Chaîne des Puys, eine spektakuläre Gegend, die zu den faszinierendsten Landschaften der Welt zählt. Der Titel dieses dynamischen und rhythmischen Stücks, in dem alle Instrumentengruppen des Orchesters verwendet werden, bezieht sich auf die Kurstadt Mont-Dore. Das zentrale Thema ist sehr sanft und voller Emotionen und die Musik beschreibt sowohl die Betriebsamkeit als auch die Ruhe dieserRegion.

Golden Peak est une œuvre de concert qui nous plonge dans l’univers des volcans d’Auvergne, au centre de la France. Ce sont des volcans endormis dont l’ ge s’étend de 65 millions d’années jusqu’ seulement 7000 ans. Parmi les plus célèbres, la Chaîne des Puys compte 80 volcans et forme un environnement naturel qui se place parmi les plus fascinants au monde. Le titre de cette pièce dynamique et rythmique, qui fait appel tous les pupitres de l’orchestre, se rapporte la ville thermale de Mont-Dore. Très serein, le thème central est fascinant, tandis que la musique dépeint la fois le dynamisme et la quiétude de la région.

Saxophone quartet - Advanced

SKU: FT.FM473

Composed by Russell Hepplewhite. Saxophone Quartet SATB. Score and parts. Forton Music #FM473. Published by Forton Music (FT.FM473).

ISBN 9790570483723.

The first movement Chocolate Hills explores an unearthly but colourful image of enormous hills turned brown from the dry season and located in the Phillipines.  The second movement Socotra focuses on an area of Yemen so remote and with a climate so unforgiving it is amazing any species can survive there at all, and yet the image I based my music upon is bursting with life including dragon's blood trees, Socotra sunbirds and legless lizards. The third movement Moeraki Boulders takes us to a beach in New Zealand to ponder the ghostly appearance of clusters of spherical rocks formed several million years ago; while the final movement Stone Forest ends our musical journey imagining an area in China in which vast stalagmite-like formations rise from the ground and create the appearance of petrified trees.  .

(Tenor Voice). For Voice (Tenor voice). Vocal Collection. Singer's Library of Musical Theatre. Broadway. Book and 2 CDs. 208 pages

Concert Band - Grade 1.5

SKU: AP.46651

Composed by Edward Kennedy. Concert Band; Performance Music Ensemble; Single Titles. Alfred Debut Series. Programmatic. Score and Part(s). 128 pages. Alfred Music #00-46651. Published by Alfred Music (AP.46651).

UPC: 038081532912. English.

Australian water dragons are fairly large lizards that have been around for 20 million years or so, and they can be seen along the rivers and waterways of Eastern Australia. For some Australian Aborigines, the water dragon is said to bring divine presence and a gateway to the astral world. This programmatic work portrays these mystical primordial creatures playing around in the midday sun.

Tenor Book/Online Audio Pack. Edited by Richard Walters. Vocal Collection. Piece for the NFMC Vocal event with the National Federation of Music Clubs (NFMC) Festivals Bulletin 2008-2009-2010. Musical theatre, Broadway, Play along. Softcover Audio Online. 224 pages. Published by Hal Leonard

(Tenor Book Only). By Various. Edited by Richard Walters. Vocal Collection. Softcover. 216 pages. Published by Hal Leonard

(Tenor Accompaniment CDs Only). By Various. Edited by Richard Walters. Vocal Collection. CD only. 8 pages. Published by Hal Leonard

(100 Songs Excerpted for Successful Auditions). Edited by Michale Dansicker. For tenor voice solo and piano accompaniment. Vocal Collection. Broadway, Movies and Pop. Difficulty: medium. Songbook. Vocal melody, lyrics, piano accompaniment, chord names and introductory text. 174 pages. Published by Hal Leonard

By Adele. Piano/Vocal/Guitar Artist Songbook. Softcover. 72 pages. Published by Hal Leonard

Concert Band Concert Band - Grade 3.5; Grade 4

SKU: FJ.B1709

Composed by Erik Morales. Concert Band. FJH Concert Band. Programmatic. Score and Part(s). Duration 5:45. The FJH Music Company Inc #98-B1709. Published by The FJH Music Company Inc (FJ.B1709).

UPC: 241444379738. English.

Approximately 66 million years ago scientists believe an asteroid impacted the earth and caused the extinction of seventy-five percent of all life. Reign of Fire illustrates the period of chaos which ensued during this transformative event. Unusual and haunting harmonies prevail in this wonderful programmatic piece that also features many of your woodwind soloists.

About FJH Concert Band

Designed for high school groups and upper-level middle school groups. Independence is encouraged, but many lines are cross-cued. Usually includes an expanded percussion section. Grades 3 - 3.5

(Trombone). By Adele. For Trombone (Trombone). Instrumental Play-Along. Softcover Audio Online. 24 pages. Published by Hal Leonard