Composed by Liam
Ramsey-White. Contest.
Intermezzo. Score.
Excelcia Music Publishing
#ISO2203FS. Published by
Excelcia Music Publishing
(XC.ISO2203FS).
12 x 9
inches.
Inspired by
a fond memory of trudging
through the mud at a
volleyball game, this new
work for string orchestra
is both quirky and
charming. You and your
students will love Mud
Trudge.
Composed by Liam
Ramsey-White. Contest.
Intermezzo. Contest.
Score and set of parts.
Excelcia Music Publishing
#ISO2203. Published by
Excelcia Music Publishing
(XC.ISO2203).
12 x 9
inches.
Inspired by
a fond memory of trudging
through the mud at a
volleyball game, this new
work for string orchestra
is both quirky and
charming. You and your
students will love Mud
Trudge.
SKU: CA.608300 Composed by Gerhard Trubel, Michael Praetorius, and Sethus...(+)
SKU: CA.608300
Composed by Gerhard
Trubel, Michael
Praetorius, and Sethus
Calvisius. German title:
Mit Meinem Gott Geh Ich
Zur Ruh (3). Sacred vocal
music, Morning, midday,
evening. Full score.
Carus Verlag #CV
06.083/00. Published by
Carus Verlag (CA.608300).
(El Triangulo de las Bermudas). Composed by Jose Alberto Pina. For concert band....(+)
(El Triangulo de las
Bermudas). Composed by
Jose Alberto Pina. For
concert band. Grade 5.
Score only. Duration 18
minutes. Published by
Molenaar Edition
The Bermuda Triangle Orchestre d'harmonie [Conducteur et Parties séparées] - Intermédiaire Molenaar Edition
(El Triangulo de las Bermudas). By Jose Alberto Pina. For concert band. Grade 5....(+)
(El Triangulo de las
Bermudas). By Jose
Alberto Pina. For concert
band. Grade 5. Score and
set of parts. Duration 18
minutes. Published by
Molenaar Edition
by Stacy Phillips. For fiddle. All styles, fiddle tunes. Level: Multiple Levels....(+)
by Stacy Phillips. For
fiddle. All styles,
fiddle tunes. Level:
Multiple Levels. Book.
Solos. Size 8.75x11.75.
268 pages. Published by
Mel Bay Pub., Inc.
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.
Bermuda Islands Piano seul - Intermédiaire Alfred Publishing
Composed by Betty Lea Martocchio. Piano Suite; Piano Supplemental; Solo. Reci...(+)
Composed by Betty Lea
Martocchio. Piano Suite;
Piano Supplemental; Solo.
Recital Suite Series.
Form:
Suite. Recital. Sheet. 12
pages. Alfred Music #00-
47928. Published by
Alfred
Music
Guitar SKU: HL.49010855 Guitar Solo. Composed by Various. Edited b...(+)
Guitar
SKU:
HL.49010855
Guitar
Solo. Composed by
Various. Edited by Konrad
Ragossnig. Arranged by
Konrad Ragossnig. This
edition: Saddle
stitching. Sheet music.
Gitarren-Archiv (Guitar
Archive). Classical. 39
pages. Schott Music
#GA442. Published by
Schott Music
(HL.49010855).
ISBN
9790001096911. UPC:
073999469875.
9.0x12.0x0.161
inches.
Contents:
Kemp's Jig (anon) *
Fantasie (Bakfark) *
Guillemente (Besard) *
Pavan (Bulman) * Due
Ricercari (Capirola) *
Walsingham (Cutting) *
Calata ala spagnola
(Dalza) * Fantasia,
Villanella, Finale
(Dluggoraj) * Lachrimae
Pavan (Dowland) * The
Queen Elizabeth her
Galliard (Dowland) * The
Earl of Essex his
Galliard (Dowland) * Sir
John Smith his Almaine
(Dowland) * Galiarda
Manfredina (Garsi) * La
ne mente per la gola
(Garsi) * Alman (Johnson)
* Passemeze (Le Roy) *
Passemeze more shorter
(plus diminue) (Le Roy) *
Gallarda (Mudarra) *
Pavana de Alexandre
(Mudarra) * der Juden
Tantz (Neusidler) * Psalm
V (Sweelinck).
Balkan Fluet Duets 2 Flûtes traversières (duo) [Conducteur] Universal Edition
Composed by Traditional. Arranged by Hidan Mamudov. Performance score. 24 pages....(+)
Composed by Traditional.
Arranged by Hidan
Mamudov. Performance
score. 24 pages.
Universal Edition
#UE33043. Published by
Universal Edition
(PR.UE033043).
Six Cameos Basson [Partie séparée] - Intermédiaire/avancé Howard J. Buss Publications
Composed by Roger Vogel (1947-). Edited by Howard J. Buss. These musical cameos ...(+)
Composed by Roger Vogel
(1947-). Edited by Howard
J. Buss. These musical
cameos reflect the
characters of 6 people:
the movements are
entitled Sailor, Dreamer,
Dancer, Curmudgeon, Blues
Bassoonist, and Runner.
21st Century. Solo part.
Composed 2011. Duration
15'. Published by Howard
J. Buss Publications
(B7.B931).
VHS Video. Performed by Muddy Waters. By Bob Margolin. Star Licks Master Session...(+)
VHS Video. Performed by
Muddy Waters. By Bob
Margolin. Star Licks
Master Sessions
(Instructional video).
Popular. VHS Video. Size
4.7x8 inches. Published
by Star Licks.
SKU: CA.607800 Composed by Gerhard Trubel. German title: Der Mond Ist Auf...(+)
SKU: CA.607800
Composed by Gerhard
Trubel. German title: Der
Mond Ist Aufgegangen (3).
Unison hymns, Secular
choral music, Morning,
midday, evening. Full
score. Carus Verlag #CV
06.078/00. Published by
Carus Verlag (CA.607800).
Guitar Signature Licks DVD. Performed by Muddy Waters. By Bob Margolin. Dvd. DVD...(+)
Guitar Signature Licks
DVD. Performed by Muddy
Waters. By Bob Margolin.
Dvd. DVD (Digital Video
Disc). Size 5.3x7.5
inches. Published by Hal
Leonard Corporation.
Performed by Muddy Waters. For guitar and voice. Format: guitar tablature songbo...(+)
Performed by Muddy
Waters. For guitar and
voice. Format: guitar
tablature songbook. With
guitar tablature,
standard notation, vocal
melody, lyrics, chord
names, performance notes,
introductory text, guitar
notation legend and black
and white photos. Blues
and chicago blues.
Series: Hal Leonard
Guitar Recorded Versions.
184 pages. 9x12 inches.
Published by Hal Leonard.
