Rockin' Ol' St. Nick Orchestre à Cordes [Conducteur et Parties séparées] - Débutant Alfred Publishing
Arranged by Michael Story and Michael Story. Orchestra. Part(s); Score; String O...(+)
Arranged by Michael Story
and Michael Story.
Orchestra. Part(s);
Score; String Orchestra.
Orchestra Expressions
Book 1. Christmas;
Novelty; Rock; Secular;
Winter. Grade 1. 80
pages. Published by
Alfred Music Publishing
We Will Rock You Orchestre à Cordes [Conducteur et Parties séparées] - Débutant Hal Leonard
We Will Rock You by Queen. By Brian May. Arranged by Paul Lavender. Score and Pa...(+)
We Will Rock You by
Queen. By Brian May.
Arranged by Paul
Lavender. Score and
Parts. Essential Elements
String Performer. Grade
1-1.5. Softcover.
Published by Hal Leonard
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.
Danny Rocks Orchestre à Cordes - Intermédiaire Alfred Publishing
Arranged by Bob Phillips. Traditional. For String Orchestra. String Orchestra. S...(+)
Arranged by Bob Phillips.
Traditional. For String
Orchestra. String
Orchestra. String
Alternatives. Folk Song.
Level: 3 (grade 3).
Conductor Score and
Parts. 144 pages.
Published by Alfred
Publishing.
Danny Rocks Orchestre à Cordes [Conducteur] - Intermédiaire Alfred Publishing
Arranged by Bob Phillips. Traditional. For String Orchestra. String Orchestra. S...(+)
Arranged by Bob Phillips.
Traditional. For String
Orchestra. String
Orchestra. String
Alternatives. Folk Song.
Level: 3 (grade 3).
Conductor Score. 16
pages. Published by
Alfred Publishing.
Holiday Mash-Up Orchestre à Cordes [Conducteur] - Intermédiaire Alfred Publishing
(As featured on Glee (Featuring: Have Yourself a Merry Little Christmas /...(+)
(As featured on
Glee (Featuring:
Have Yourself a Merry
Little Christmas / Jingle
Bell Rock)). Arranged by
Patrick Roszell.
Orchestra. Full
Orchestra; Score. Pop
Intermediate Full
Orchestra. Form: Medley.
Christmas; Secular; TV;
Winter. Grade 3. 16
pages. Published by
Alfred Music
Croc Rock Orchestre à Cordes [Conducteur et Parties séparées] - Facile Alfred Publishing
By Andy Firth. Arranged by Bob Phillips. By Andy Firth / arr. Bob Phillips. For ...(+)
By Andy Firth. Arranged
by Bob Phillips. By Andy
Firth / arr. Bob
Phillips. For String
Orchestra. String
Orchestra. Belwin
Beginning String
Orchestra. Level: grade 2
Red. Conductor Score &
Parts. 39 pages.
Published by Alfred
Publishing.
As recorded by DNCE. Composed by Justin Tranter, Robin Fredriksson, Matti...(+)
As recorded by
DNCE. Composed by
Justin Tranter, Robin
Fredriksson, Mattias
Larsson, and Joe Jonas
[DNCE]. Arranged by
Victor Lopez. Score;
String Orchestra. Pop
Intermediate String
Orchestra. Pop/Rock. 12
pages. Published by
Alfred Music (AP.45833S).
Cake by the Ocean Orchestre à Cordes [Conducteur et Parties séparées] - Intermédiaire Alfred Publishing
As Recorded by DNCE. Composed by Justin Tranter, Robin Fredriksson, Matti...(+)
As Recorded by
DNCE. Composed by
Justin Tranter, Robin
Fredriksson, Mattias
Larsson, and Joe Jonas
[DNCE]. Arranged by
Victor Lopez. Part(s);
Score; String Orchestra.
Pop Intermediate String
Orchestra. Pop; Pop/Rock.
152 pages. Published by
Alfred Music (AP.45833).
Score Only.
Arranged by Kathryn
Griesinger. Series;
String Orchestra. FJH
Developing Strings.
Holiday Pops. Score.
Duration 2:00. The FJH
Music Company Inc
#98-ST6432S. Published by
The FJH Music Company Inc
(FJ.ST6432S).
English.
A
rocking celebration of
the season! Set in first
position with simple
rhythms and no slurs,
this contemporary
arrangement includes the
familiar carols Deck the
Hall, Hark, the Herald
Angels Sing, and Ding,
Dong, Merrily On High.
Every section of the
orchestra is featured and
the energetic cello/bass
groove is driven by
optional drum set and
sleigh bells. An
exuberant finale for your
holiday concert!
About FJH
Developing
Strings
Sl
ightly more advanced than
Beginning Strings, this
series begins to involve
more position work and a
slightly more complex
rhythmic figures.
Rehearsal piano is often
provided. Ideal for
middle school and smaller
high school programs.
Grade 2 - 2.5
(Featuring: Paint It, Black / Ruby Tuesday / (I Can't Get No) Satisfaction). Orc...(+)
(Featuring: Paint It,
Black / Ruby Tuesday / (I
Can't Get No)
Satisfaction). Orchestra.
Score; SmartMusic; String
Orchestra. Pop Concert
String Orchestra. Form:
Medley. Rock. Grade 3.5.
20 pages. Published by
Alfred Music
The Rolling Stones on Tour Orchestre à Cordes [Conducteur et Parties séparées] - Intermédiaire Alfred Publishing
(Featuring: Paint It, Black / Ruby Tuesday / (I Can't Get No) Satisfaction). Orc...(+)
(Featuring: Paint It,
Black / Ruby Tuesday / (I
Can't Get No)
Satisfaction). Orchestra.
Part(s); Score; String
Orchestra. Pop Concert
String Orchestra. Form:
Medley. Rock. Grade 3.5.
136 pages. Published by
Alfred Music Publishing
Rocksteady Reggae Orchestre à Cordes [Conducteur et Parties séparées] - Facile Alfred Publishing
By Matt Turner. Orchestra. Part(s); Score; String Orchestra. Highland String Alt...(+)
By Matt Turner.
Orchestra. Part(s);
Score; String Orchestra.
Highland String
Alternatives. Light
Concert; Rock. Grade 2.5.
130 pages. Published by
Alfred Music Publishing
First Snow Orchestre à Cordes [Conducteur et Parties séparées] - Facile Alfred Publishing
As Performed by Trans- Siberian Orchestra. Composed by Paul O'Neill [Trans- Sib...(+)
As Performed by Trans-
Siberian Orchestra.
Composed
by Paul O'Neill [Trans-
Siberian Orchestra].
Arranged by Bob Phillips.
Part(s); Score; String
Orchestra. Pop Concert
String Orchestra.
Christmas;
Pop/Rock; Rock; Secular;
Winter. 140 pages.
Published
by Alfred Music
Siberian Sleigh Ride Orchestre à Cordes [Conducteur et Parties séparées] - Intermédiaire Alfred Publishing
(As Performed by Trans-Siberian Orchestra). Composed by Paul O'Neill [Trans-Sibe...(+)
(As Performed by
Trans-Siberian
Orchestra). Composed by
Paul O'Neill
[Trans-Siberian
Orchestra]. Arranged by
Bob Phillips. Orchestra.
Part(s); Score; String
Orchestra. Pop Concert
String Orchestra.
Christmas; Rock; Secular;
Winter. Grade 3. 148
pages. Published by
Alfred Music
Overture Orchestre à Cordes [Conducteur et Parties séparées] - Intermédiaire Alfred Publishing
As Performed by Trans-Siberian Orchestra. Composed by Beethoven/Mozart. A...(+)
As Performed by
Trans-Siberian
Orchestra. Composed
by Beethoven/Mozart.
Arranged by Paul O'Neill
[Trans-Siberian
Orchestra]. Part(s);
Score; SmartMusic; String
Orchestra. Pop Concert
String Orchestra. Form:
Overture. Pop/Rock; Rock;
Secular. 140 pages.
Published by Alfred Music
(AP.44817).
Led Zeppelin Medley Orchestre à Cordes [Conducteur et Parties séparées] - Intermédiaire Alfred Publishing
(Featuring: Communication Breakdown / Immigrant Song / Stairway to Heaven / Daze...(+)
(Featuring: Communication
Breakdown / Immigrant
Song / Stairway to Heaven
/ Dazed and Confused /
Rock and Roll). Arranged
by Bob Phillips.
Orchestra. String
Orchestra. Pop Concert
String Orchestra. Light
Concert; Rock. Grade 3.5.
Conductor Score and
Parts. 132 pages
Siberian Sleigh Ride Orchestre à Cordes [Conducteur] - Intermédiaire Alfred Publishing
(As Performed by Trans-Siberian Orchestra). Composed by Paul O'Neill [Trans-Sibe...(+)
(As Performed by
Trans-Siberian
Orchestra). Composed by
Paul O'Neill
[Trans-Siberian
Orchestra]. Arranged by
Bob Phillips. Orchestra.
Score; String Orchestra.
Pop Concert String
Orchestra. Christmas;
Rock; Secular; Winter.
Grade 3. 44 pages.
Published by Alfred Music