SKU: GI.G-10377

ISBN 9781574635324.

A unique resource for both novice and experienced band directors gathering effective teaching tools from the best in the field including more than 40 chapters dealing with every aspect of teaching instrumental music from curriculum to valuable websites. This best-selling and highly praised text has become the method of choice for university methods courses throughout the United States and Canada. What's New in the Revised Edition? Curriculum—updated to 2014 National Music Education Standards, including relevant learning theories, modalities, and music instruction theories. Resources—for concert band, marching band, pep band, jazz ensemble, and chamber groups School Law—learn more about the teacher’s Code of Ethics, music copyright law, and examine common ethical teaching scenarios. Anatomy of Music-Making—presents effective methods for teaching tone quality, balance, blend, intonation, pulse, rhythm, technique, style, articulation, phrasing, interpretation, and expression. STEPS© Method—for creating rehearsal plans and providing a theoretical approach to understanding the ensemble to improve score study and objective assessment. Motivation—surveys current intrinsic and extrinsic methods, and explores the development of leadership and character in the instrumental program, including Social Emotional Learning (SEL). Job Readiness—new teacher assessment and certification requirements, as well as valuable information guiding the new teacher throughout the music practicum and the job interview. Intonation—expanded tools for training the ear in both the individual student and full ensemble. Program Administration— the “nuts and bolts” of managing the instrumental program have been updated with topics on assessment, evaluation, rehearsal planning, score study, repertoire selection, programming, rehearsal facilities, auditions, seating, recruiting and retention, budget planning, music library management, basic instrument repair, booster groups, advocacy, time management, practicing tips, and classroom management and discipline. Mind Your P’s and Q’s—considers the implications and relationships of Professional Growth, Personal Growth, Intelligence Quotient, and Emotional Quotient. Supplementary Website—numerous charts, figures, templates, a balanced instrumentation calculator, teaching tools, recruiting materials, assessment rubrics, various learning activities. Learn more about this new resouce in this short video below: Click here to download Lesson Plan Forms.   A wonderful resource for all music educators! Dr. Jagow’s book is comprehensive and impressive in scope. An excellent book! Bravo! —Frank L. Battisti Finally, an exceptional text that offers the depth of understanding our students need in critically important topic areas. Bravo! —Don Harris So many important facets are uncovered and solutions revealed. It’s a must for the library of any serious music educator. —H. Robert Reynolds There are a growing number of fine books dealing with different aspects of the wind band and ensemble, none cover so many essential aspects in so much detail. —Tim Reynish Dr. Jagow's book is a fantastic resource for instrumental conductors, both the young and the more experienced! —George Edge . . . a book which contains a wonderfully diverse wealth of knowledge that is 'hands on' for the informed music educator. . . . an excellent resource for both beginning teachers and veteran music educators. —Dr. Linda R. Moorhouse From creating artistic musical experiences to establishing a first-class organization blueprint, there is no stone left unturned. This is not a book to be recommended, but a book to be REQUIRED. —Tim Lautzenheiser.

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: PR.41641576L

UPC: 680160636549. 11 x 17 inches.

The 1712 Overture stands out in P.D.Q. Bach's oeuvre for two reasons, among others: it is by far the most programmatic instrumental piece among those by the minimeister of Wein-am-Rhein so far unearthed, and 2) its discovery has led to a revelation about the composer's father, Johann Sebastian Bach, that has exploded like a bombshell on the usually serene musicological landscape. The overture is based on an anecdote told to P.D.Q. Bach by a cousin, Peter Ulrich. Since P.U. Bach lived in Dudeldorf, only a few miles down the road from Wein-am-Rhein, he was P.D.Q.'s closest relative, and he was, in fact, one of the few members of the family who was on speaking terms with P.D.Q. The story, related to P.D.Q. (fortunately for us posterity types) in a letter, may be summarized thus: The town of Dudeldorf was founded by two brothers, Rudi and Dieter Dudel, early in the 18th century. Rudi remained mayor of the newborn burg for the rest of his long life, but Dieter had a dream of starting a musicians' colony, an entire city devoted to music, which dream, he finally decided, could be realized only in the New World. In 1712, he and several other bagpipers sailed to Boston, never to return to Germany. (Henceforth, Rudi became known as der deutscher Dudel and Dieter as the Yankee Dudel). Unfortunately, the head of the Boston Musicians' Guild had gotten wind of Dudel's plans, and Wilhelm Wiesel (pron. VEE-zle), known none too affectionately around town as Wiesel the Weasel, was not about to share what few gigs there were in colonial America with more foreigners and outside agitators. He and his cronies were on hand to meet Dudel's boat when it pulled into Boston Harbor; they intended to prevent the newcomers' disembarkation, but Dudel and his companions managed to escape to the other side of the bay in a dinghy, landing with just enough time to rent a carriage and horses before hearing the sound of The Weasel and his men, who had had to come around the long way. The Germans headed West, with the Bostonians in furious pursuit. soon the city had been left far behind, and by midnight so had the pursuers; Dieter Dudel decided that it was safe for him and his men to stop and sleep until daybreak. When they awoke, they found that they were in a beautiful landscape of low, forested mountains and pleasant fields, warmed by the brilliant morning sun and serenaded by an entrancing variety of birds. Here, Dudel thought, her is where I will build my colony. The immigrants continued down the road at a leisurely pace until they came upon a little church, all by itself in the countryside, from which there suddenly emanated the sounds of a pipe organ. At this point, the temptation to quote from P.U. Bach's letter to P.D.Q. cannot be resisted: They went inside and, after listening to the glorious music for a while, introduced themselves to the organist. And who do you think it was? Are you ready for this -- it was your old man! Hey, no kidding -- you know, I'm sure, that your father was the guy to get when it came to testing new organs, and whoever had that one in Massachusetts built offered old Sebastian a tidy sum to go over there and check it out. The unexpected meeting with J.S. Bach and his sponsors was interrupted by the sound of horse hooves, as the dreaded Wiesel and his men thundered on to the scene. They had been riding all night, however, and they were no spring chickens to start with, and as soon as they reached the church they all dropped, exhausted, to the ground. The elated Germans rang the church bells and offered to buy everyone a beer at the nearest tavern. There they were taught, and joined in singing, what might be called the national anthem of the New World. The melody of this pre-revolutionary patriotic song is still remembered (P.D.Q. Bach quotes it, in the bass instruments, near the end of the overture), but is words are now all but forgotten: Freedom, of thee we sing, Freedom e'er is our goal; Death to the English King, Long live Rock and Ross. The striking paucity of biographical references to Johann Sebastian Bah during the year 1712 can now be explained: he was abroad for a significant part of that year, testing organs in the British Colonies. That this revelation has not been accepted as fact by the musicological establishment is no surprise, since it means that a lot of books would have to be rewritten. The members of that establishment haven't even accepted the existence of P.D.Q. Bach, one of whose major works the 1712 Overture certainly is. It is also a work that shows Tchaikowsky up as the shameless plagiarizer that some of us have always known he was. The discovery of this awesome opus was made possible by a Boston Pops Centennial Research Commission; the first modern performance took place at the opening concert of the 100th anniversary season of that orchestra, under the exciting but authentic direction of John Williams.

SKU: HL.1728550

UPC: 196288280262.

SJC's most popular snare drum to date, now with a signature touch – literally! This stage authentic snare features a 3mm brushed bell brass shell, “Spooky” hoop inlays, and a badge hand-signed by Josh Dun himself! The Josh Dun Signature Goliath will equip you with the most powerful and dynamic tones under the Midwest Indigo. You can literally feel the weight and punch when you dig into it yet also produce a smooth, sensitive response when you need to hear those ghost notes. Uparalleled sound makes teh Goliath a must-have for any studio or stage. Specs: • 3mm Bell Brass shell • Raw brushed brass finish • Flat black hardware • Double ended tube lugs • 3.0mm triple flanged hoops with red and black “spooky” inlays • Black t-rods • 20 strand wires • Goliath brass badge signed by Josh Dun.