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Abdon Bryant
Drum notation is different than sheet music, although they look similar and use some of the same concepts. In sheet music, the symbols on the staff correspond to different notes. In drum notation, the symbols represent different parts of the drum set (snare, hi-hat, bass drum, etc.) to be played. This is useful for beginners learning to coordinate their limbs, helping to develop the necessary skill sets to both comfortably keep steady time and play the correct part of the drum set.
Like the English language, drum notation is read from left to right. The staff is made up of five lines and four spaces, but notes can be positioned above or below the staff as well. Notes are placed in the staff based on which part of the drum set should be played at any given time. Notice below that the bass drum is in a different position on the staff than the snare or ride cymbal.
Some of the most common drum beats are whole notes, half notes, quarter notes, eighth notes, sixteenth notes, and thirty-second notes. There are different types of triplets that can be played as well, where you play three notes in the space normally occupied by two notes.
Drum tab notation is a simplified version of drum notation. Instead of using the typical notes you would read in a piece of music, drum tablature uses a series of vertical and horizontal lines with different characters to represent rhythm and patterns for the drummer to play. All drummers are different and learn in different ways.
Ghost notes are often played as light, bouncy notes on a snare drum that can sound like many quick notes played in succession. This technique is often used in drum beats to help create more rhythmic movements within a piece of music, and can be played with both the right and left hands.
A soft one-handed roll is played by lightly striking the drum and then letting the bottom of the stick rest against the rim, followed by bouncing the stick back toward the drum to get a second stroke. This technique can be used to achieve more notes quickly with one hand.
An accented one-handed roll is the same as the above but contains an accent with one of the notes. You can strike either of the two notes more loudly or softly than the other to create a unique rhythm.
For beginners, learning to read drum notation is a lot like learning a new language. Use associations early on to remember what certain things mean on the drums. For example, certain words contain syllables that are applicable to different rhythms.
As the footnotes grow in proportion to the text proper, Morley simultaneously begins a new approach to holding our attention within the main text by compiling various greatest songs- and albums-of-all-time lists. In their comprehensive quirkiness, these lists alone are probably worth the price of the book. We find lists such as:
Metamorphic rocks started out as some other type of rock, but have been substantially changed from their original igneous, sedimentary, or earlier metamorphic form. Metamorphic rocks form when rocks are subjected to high heat, high pressure, hot mineral-rich fluids or, more commonly, some combination of these factors. Conditions like these are found deep within the Earth or where tectonic plates meet.
Process of Metamorphism:
The process of metamorphism does not melt the rocks, but instead transforms them into denser, more compact rocks. New minerals are created either by rearrangement of mineral components or by reactions with fluids that enter the rocks. Pressure or temperature can even change previously metamorphosed rocks into new types. Metamorphic rocks are often squished, smeared out, and folded. Despite these uncomfortable conditions, metamorphic rocks do not get hot enough to melt, or they would become igneous rocks!
Foliated Metamorphic Rocks:
Some kinds of metamorphic rocks -- granite gneiss and biotite schist are two examples -- are strongly banded or foliated. (Foliated means the parallel arrangement of certain mineral grains that gives the rock a striped appearance.) Foliation forms when pressure squeezes the flat or elongate minerals within a rock so they become aligned. These rocks develop a platy or sheet-like structure that reflects the direction that pressure was applied.
Non-Foliated Metamorphic Rocks:
Non-foliated metamorphic rocks do not have a platy or sheet-like structure. There are several ways that non-foliated rocks can be produced. Some rocks, such as limestone are made of minerals that are not flat or elongate. No matter how much pressure you apply, the grains will not align! Another type of metamorphism, contact metamorphism, occurs when hot igneous rock intrudes into some pre-existing rock. The pre-existing rock is essentially baked by the heat, changing the mineral structure of the rock without addition of pressure.
Glacier ice, like limestone (for example), is a type of rock. Glacier ice is actually a mono-mineralic rock (a rock made of only one mineral, like limestone which is composed of the mineral calcite). The mineral ice is the crystalline form of water (H2O). Most glacier ice forms through the metamorphism of tens of thousands of individual snowflakes into crystals of glacier ice. Each snow flake is a...
Igneous rocks (from the Latin word for fire) form when hot, molten rock crystallizes and solidifies. The melt originates deep within the Earth near active plate boundaries or hot spots, then rises toward the surface. Igneous rocks are divided into two groups, intrusive or extrusive, depending upon where the molten rock solidifies.Intrusive Igneous Rocks:Intrusive, or plutonic, igneous rock forms...
Sedimentary rocks are formed from pre-existing rocks or pieces of once-living organisms. They form from deposits that accumulate on the Earth's surface. Sedimentary rocks often have distinctive layering or bedding. Many of the picturesque views of the desert southwest show mesas and arches made of layered sedimentary rock. Common Sedimentary Rocks: Common sedimentary rocks include sandstone...
A mineral is a naturally occurring inorganic element or compound having an orderly internal structure and characteristic chemical composition, crystal form, and physical properties. Common minerals include quartz, feldspar, mica, amphibole, olivine, and calcite. A rock is an aggregate of one or more minerals, or a body of undifferentiated mineral matter. Common rocks include granite, basalt...
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