A Thousand Years Orchestre à Cordes [Conducteur et Parties séparées] - Intermédiaire Hal Leonard
(from The Twilight Saga: Breaking Dawn, Pt. 1). By Christina Perri. By Christina...(+)
(from The Twilight Saga:
Breaking Dawn, Pt. 1). By
Christina Perri. By
Christina Perri and David
Hodges. Arranged by Larry
Moore. For String
Orchestra, Orchestra
(Score and Parts). Pop
Specials for Strings.
Grade 3-4. 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.
By Gioachino Rossini. Arranged by Harry Alshin. Music by Gioacchino Rossini / ar...(+)
By Gioachino Rossini.
Arranged by Harry Alshin.
Music by Gioacchino
Rossini / arr. Harry
Alshin. For String
Orchestra. String
Orchestra. String
Orchestra. Level: 3
(grade 3). Conductor
Score and Parts. 2 pages.
Published by Alfred
Publishing.
Strings All Around Orchestre à Cordes [Conducteur et Parties séparées] - Débutant Belwin
(An Orchestral Exordium). Arranged by Andrew H. Dabczynski. Orchestra. Part(s); ...(+)
(An Orchestral Exordium).
Arranged by Andrew H.
Dabczynski. Orchestra.
Part(s); Score;
Sing-Along; String
Orchestra. Belwin
Beginning String
Orchestra. Traditional.
Grade 1.5. 82 pages.
Published by Belwin Music
March from Symphony No. 6 Orchestre à Cordes [Conducteur et Parties séparées] - Facile Alfred Publishing
By Peter Ilyich Tchaikovsky (1840-1893). Arranged by Andrew H. Dabczynski. ...(+)
By Peter Ilyich
Tchaikovsky
(1840-1893). Arranged by
Andrew H. Dabczynski.
Orchestra. Masterworks;
Part(s); Score; String
Orchestra. Highland
String
Explorer. Form: March;
Transcription. Masterwork
Arrangement; Romantic.
Grade
2. 140 pages. Published
by
Alfred Music Publishing
Composed by Shirl Jae
Atwell. String Tracks
XVIII. Full set. Neil A.
Kjos Music Company
#SO387C. Published by
Neil A. Kjos Music
Company (KJ.SO387C).
ISBN 9788402704818.
UPC:
8402704816.
Allegretto from
Piano Sonata Op. 9, No.
1, is the 2nd movement
from the sonata, arranged
by Atwell in G Major. It
comes from Beethoven's
early years and showcases
the beautiful simplicity,
warmth, and lyricism of
his compositional genius.
It is minuet-like in
structure and style.
A French Noel Orchestre à Cordes [Conducteur] - Débutant Alfred Publishing
Arranged by Mark Williams. Traditional. For String Orchestra. String Orchestra. ...(+)
Arranged by Mark
Williams. Traditional.
For String Orchestra.
String Orchestra.
Strictly Strings Series.
Level: 1 (grade 1).
Conductor Score.
Published by Alfred
Publishing.
By Wolfgang Amadeus Mozart. Arranged by Brendan Mcbrien. For String Orchestra. S...(+)
By Wolfgang Amadeus
Mozart. Arranged by
Brendan Mcbrien. For
String Orchestra. String
Orchestra. Highland
String Orchestra. Level:
3 (grade 3). Conductor
Score. Published by
Alfred Publishing.
Egyptian Legacy Orchestre à Cordes [Conducteur et Parties séparées] - Intermédiaire/avancé FJH
By Soon Hee Newbold. FJH String Orchestra. A vast and mighty empire for thousand...(+)
By Soon Hee Newbold. FJH
String Orchestra. A vast
and mighty empire for
thousands of years, the
ancient Egyptian
civilization has
intrigued and fascinated
the modern world with its
art, culture, and amazing
architecture. The Great
Sphinx, giant pyramids,
and statues of pharaohs
are the powerful images
of Egypt. From King Tut
to Cleopatra, ancient
Egypt continues to be an
influence on societies of
today. Level: Grade 4.
Published by The FJH
Music Company Inc.
By Wolfgang Amadeus Mozart. Arranged by Brendan Mcbrien. By Wolfgang Amadeus Moz...(+)
By Wolfgang Amadeus
Mozart. Arranged by
Brendan Mcbrien. By
Wolfgang Amadeus Mozart /
arr. McBrien. For String
Orchestra. String
Orchestra. Highland
String Orchestra. Level:
3 (grade 3). Conductor
Score and Parts.
Published by Alfred
Publishing.
Sequential Repertoire for Solo Strings or String Ensemble (Piano / Score). ...(+)
Sequential Repertoire for
Solo Strings or String
Ensemble (Piano / Score).
Composed by Winifred
Crock,
William Dick, and Laurie
Scott.
Method/Instruction;
Score; String Orchestra
Method/Supplement;
Suzuki.
64 pages. Published by
Alfred Music
Orchestra String Orchestra - Grade 3 SKU: FJ.ST6418 Composed by Wolfgang ...(+)
Orchestra String
Orchestra - Grade 3
SKU: FJ.ST6418
Composed by Wolfgang
Amadeus Mozart. Arranged
by Robert D McCashin.
Series; String Orchestra.
FJH String Orchestra.
Masterwork Arrangement.
Score and Part(s).
Duration 4:30. The FJH
Music Company Inc
#98-ST6418. Published by
The FJH Music Company Inc
(FJ.ST6418).
UPC:
241444375464.
English.
This
delightful Serenade in D
(K. 100/62a) was
completed in 1769, when
Mozart was a mere 13
years of age (and this is
an ideal fact to share
with students)! The first
movement, even though
composed at such a young
age, provides challenges
for every musician in the
ensemble and is musically
appealing to players and
audience. This would be
an outstanding addition
at any point in a program
but works particularly
well as a concert
closer!
About FJH
String
Orchestra
More emphasis on bow
technique and
independence of lines.
For the accomplished
middle, high school,
college, or professional
group. Grade 3 and up
Arioso Orchestre à Cordes [Conducteur et Parties séparées] - Facile Belwin
Arranged by Douglas E. Wagner. Orchestra. Part(s); Score; String Orchestra. Belw...(+)
Arranged by Douglas E.
Wagner. Orchestra.
Part(s); Score; String
Orchestra. Belwin
Beginning String
Orchestra. Baroque;
Masterwork Arrangement.
Grade 2. 76 pages.
Published by Belwin Music
Arranged by Carrie Lane
Gruselle. Series; String
Orchestra. FJH Beginning
Strings. Masterwork
Arrangement. Score and
Part(s). Duration 1:50.
The FJH Music Company Inc
#98-ST6460. Published by
The FJH Music Company Inc
(FJ.ST6460).
UPC:
241444389560.
English.
This
extremely popular melody
was composed when Mozart
was a mere 6 years old
and surely predicts his
remarkable genius!
Written for the youngest
of musicians, this
arrangement features
simple phrases infused
with contrasting dynamics
and articulations.
About FJH
Beginning
Strings
Ap
propriate for first year
string students. All
instruments stay in first
position, and optional
third violin (viola)
parts and piano are
included to aid in
rehearsal and performance
situations. Grade 1 -
1.5
By Johann Sebastian Bach (1685-1750). Arranged by Bob Lipton. Orchestra. Masterw...(+)
By Johann Sebastian Bach
(1685-1750). Arranged by
Bob Lipton. Orchestra.
Masterworks; Score;
String Orchestra.
Highland String
Orchestra. Form:
Transcription. Baroque;
Masterwork Arrangement.
Grade 2.5. 8 pages.
Published by Alfred Music
Publishing
Composed by Leo Delibes (1836-1891). Arranged by Frank J. Halferty. For string o...(+)
Composed by Leo Delibes
(1836-1891). Arranged by
Frank J. Halferty. For
string orchestra. Concert
String Orchestra. Grade 3
. Score and parts.
Published by Kendor Music
Inc
Prelude for String Orchestra Orchestre à Cordes [Conducteur et Parties séparées] - Intermédiaire Boosey and Hawkes
By Gerald Finzi (1901-1956). Score and Parts. Boosey and Hawkes Orchestra. Grade...(+)
By Gerald Finzi
(1901-1956). Score and
Parts. Boosey and Hawkes
Orchestra. Grade 3-4. 25
pages. Boosey and Hawkes
#M060830594. Published by
Boosey and Hawkes
(For String Orchestra, Harp, Timpani, And Percussion). By Arvo Part (1935-). For...(+)
(For String Orchestra,
Harp, Timpani, And
Percussion). By Arvo Part
(1935-). For String
Orchestra, Harp, Timpani,
Percussion. Study score.
58 pages. Duration 34
minutes. Published by
Universal Edition
Composed by Shirl Jae
Atwell. String Tracks
XVIII. Score. Neil A.
Kjos Music Company
#SO387F. Published by
Neil A. Kjos Music
Company (KJ.SO387F).
UPC:
8402704817.
Allegretto from
Piano Sonata Op. 9, No.
1, is the 2nd movement
from the sonata, arranged
by Atwell in G Major. It
comes from Beethoven's
early years and showcases
the beautiful simplicity,
warmth, and lyricism of
his compositional genius.
It is minuet-like in
structure and style.
Three Pieces Orchestre à Cordes [Conducteur et Parties séparées] - Intermédiaire Grand Mesa Music
Composed by Ludwig Maurer. Edited by J. Cameron Law. Arranged by Bob Lipton....(+)
Composed by Ludwig
Maurer.
Edited by J. Cameron Law.
Arranged by Bob Lipton.
For
string orchestra. Grade
3+.
Score and set of parts.
Duration 4 minutes, 20
seconds
(total). Published by
Grand
Mesa Music
Composed by Alan Lee Silva. Concert String Orchestra. Full score (study). With S...(+)
Composed by Alan Lee
Silva. Concert String
Orchestra. Full score
(study). With Standard
notation. Carl Fischer
Music #CAS86F. Published
by Carl Fischer Music
(CF.CAS86F).
0.5
By Johann Sebastian Bach (1685-1750). Arranged by Bob Lipton. Orchestra. For str...(+)
By Johann Sebastian Bach
(1685-1750). Arranged by
Bob Lipton. Orchestra.
For string. Masterworks;
Part(s); Score; String
Orchestra. Highland
String Orchestra. Form:
Transcription. Baroque;
Masterwork Arrangement.
Grade 2.5. 62 pages.
Published by Alfred Music
Publishing
Composed by William
Hofeldt. Score only. Neil
A. Kjos Music Company
#SO348F. Published by
Neil A. Kjos Music
Company (KJ.SO348F).
UPC:
084027043653.
This
gorgeous and gentle
ballad is written for and
dedicated to Ms. Dorothy
Straub, whose lifelong
career in music education
has touched students and
educators worldwide for
many years. Includes an
optional (and highly
recommended) harp part. G
Minor & G
Major.
