PARTITIONS GRATUITES : QUINTETTE DE CUIVRES : 2 TROMPETTES, 1 COR, 1 TROMBONE, 1 TUBA
- Nevada

Concert Band - Grade 4

SKU: HL.44006738

Grade 4 - Score Only. Composed by Philip Sparke. Closer. Anglo Music Concert Band. Concert. Score Only. Composed 2006. 24 pages. Anglo Music Press #AMP157. Published by Anglo Music Press (HL.44006738).

UPC: 884088142513. 9x12 inches. English-German-French-Dut ch.

This work presents the listener with the wondrous grandeur of one of the great mountain ranges in America, the Sierra Nevada. When the music begins, the listener is greeted with the awakening of an early morning in the Sierras, complete with a mysterious, foggy mist that creates a feeling of complete stillness and peace with the world. As the mist slowly dissipates, hidden forms begin to make their presence known and gradually become a tremendous panorama of grand snow-covered mountain peaks. Grandiose and immense in all their beauty and glory, they stand before you with a sense of undeniable power, extending in all directions as far as the eye can see. Upon closer inspection one can imagine the circling golden eagles, the regal elk and royal stags, all lazily wandering the hills and canyons of conifers that stand tall, reaching for the passing clouds in hopes of gaining a few rays of life-giving sunshine and moisture. Look in another direction and you will see the immense rolling hillsides of colourful wild flowers, fluttering butterflies, birds darting about, sparkling waterfalls and all critters existing in harmony. After the day's activities the sun begins to slip below the horizon, the mist returns, and all living things prepare for another still night of sleep, serenity and the warmth of their secure bedding places.

Schaum Recital Repertoire 6 Original Piano Solos. Educational Piano. Recital. Softcover. Published by Schaum Publications, Inc.

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.

Trombone Quintet - Advanced

SKU: CY.CC3135

Composed by Henry Wolking. Classical. Score and Parts. Cherry Classics #CC3135. Published by Cherry Classics (CY.CC3135).

ISBN 9790530111048. 8.5 x 11 in inches.

Henry Wolking's The Best Dam Trombone Quintet Ever may just be! It is a fun, feel-good piece to perform and to listen to. The undulating rhythms and close harmonies produce a pleasing mood with a hint of a jazz feel. The music gives you a big hug. Here is a description of the work by the composer: In the summer of 2017 my wife and I moved to the Nevada Dam town of Boulder City. The town began as a construction camp in early 1930s for the workers of the Boulder Dam (later renamed the Hoover Dam). The dam is one of the worlds great construction projects of the 20th century and has over a million yearly visitors. My house is less than ten minutes away from the dam, and because the dam in one way or another affects everyone living in this unique Nevada town, my newest trombone quintet (composed in January 2018) is the best, well you get the picture. It is a high energy single movement work inspired by the Hoover Dam and Lake Mead. Ranges are fairly moderate with a high C# in the first trombone at the end. This is a fun romp for five dam fine trombonists. The 4 1/2 minute work is appropriate for advanced performers.

By L. Carter, O. Nevada. Arranged by Deke Sharon And Anne Raugh. (TTBB A Cappella). Choral. 11 pages. Published by Hal Leonard.

String Orchestra - beginner

SKU: XC.HSO2102FS

Composed by Caryn Wiegand Neidhold. Excelcia Music Publishing String Orchestra. Concert and Contest. Concert & Contest. Score. Excelcia Music Publishing #HSO2102FS. Published by Excelcia Music Publishing (XC.HSO2102FS).

UPC: 812598037203. 9 x 12 inches.

Brave Fires, featuring Drum Set, is a cool and fun new work about a serious subject. Composer Caryn Wiegand Neidhold writes Brave Fires honors the families impacted by devastating forest fires in Northern Nevada and Northern California and recognizes Wildland Firefighters’ and their support staff’s heroic work. Music can bring healing, and Brave Fires reaches out with energy and strength..

Concert Band - Grade 2.5

SKU: AP.44911S

Composed by Roland Barrett. Concert Band; Performance Music Ensemble; Single Titles. Belwin Young Band. Score. 32 pages. Duration 4:00. Belwin Music #00-44911S. Published by Belwin Music (AP.44911S).

UPC: 038081516189. English.

Inspired by the Valley of Fire state park in the southwest United States that boasts stunning red sandstone formations created more than 150 million years ago. Located in Nevada's oldest state park in the Mojave Desert, at certain times of the day, when reflecting the sun's rays, these brilliant sandstone formations create the visual illusion of actually being on fire. An emotional composition that is a perfect for concert and contest performances alike. Juxtaposing bold and peaceful musical statements, this compelling composition concludes with burning intensity. (4:00).