2. an exclusive privilege
1. Cancel appointment
2. cancel a contract
2. The new librarian is very polite.
3. The librarian is coding the new books.
4. The librarian is a very serious woman.
2. renew old acquaintanceship
3. renew one's knowledge
4. to renew provisions
2. due profits
3. due authority
5. Due esteem; all due respect.
2. On undergraduate advisor system
3. a third-year undergraduate.
5. a first-year undergraduate.
3. A good face is a letter of recommendation.
4. A good presence is a letter of recommendation.
2. Millennium Report
3. investigation report
4. Minority Report
The Applied Research Fund provides seed capital for technology ventures.
A central characteristic of Haydn's music is the development of larger structures out of very short, simple musical motifs, often derived from standard accompanying figures. The music is often quite formally concentrated, and the important musical events of a movement can unfold rather quickly.
Haydn's work was central to the development of what came to be called sonata form. His practice, however, differed in some ways from that of Mozart and Beethoven, his younger contemporaries who likewise excelled in this form of composition. Haydn was particularly fond of the so-called "monothematic exposition", in which the music that establishes the dominant key is similar or identical to the opening theme. Haydn also differs from Mozart and Beethoven in his recapitulation sections, where he often rearranges the order of themes compared to the exposition and uses extensive thematic development.
Haydn's formal inventiveness also led him to integrate the fugue into the classical style and to enrich the rondo form with more cohesive tonal logic (see sonata rondo form). Haydn was also the principal exponent of the double variation form—variations on two alternating themes, which are often major- and minor-mode versions of each other.
Perhaps more than any other composer's, Haydn's music is known for its humor. The most famous example is the sudden loud chord in the slow movement of his "Surprise" symphony; Haydn's many other musical jokes include numerous false endings (e.g., in the quartets Op. 33 No. 2 and Op. 50 No. 3), and the remarkable rhythmic illusion placed in the trio section of the third movement of Op. 50 No. 1.
Much of the music was written to please and delight a prince, and its emotional tone is correspondingly upbeat. This tone also reflects, perhaps, Haydn's fundamentally healthy and well-balanced personality. Occasional minor-key works, often deadly serious in character, form striking exceptions to the general rule. Haydn's fast movements tend to be rhythmically propulsive and often impart a great sense of energy, especially in the finales. Some characteristic examples of Haydn's "rollicking" finale type are found in the "London" symphony No. 104, the string quartet Op. 50 No. 1, and the piano trio Hob XV: 27. Haydn's early slow movements are usually not too slow in tempo, relaxed, and reflective. Later on, the emotional range of the slow movements increases, notably in the deeply felt slow movements of the quartets Op. 76 Nos. 3 and 5, Symphony No. 98, Symphony No. 102, and piano trio Hob XV: 23. The minuets tend to have a strong downbeat and a clearly popular character. As early as Op. 33 (1781) Haydn turned some of his minuets into "scherzi" which are much faster, at one beat to the bar.
The most common perception of a volcano is of a conical mountain, spewing lava and poisonous gases from a crater at its summit. This describes just one of many types of volcano, and the features of volcanoes are much more complicated. The structure and behavior of volcanoes depends on a number of factors. Some volcanoes have rugged peaks formed by lava domes rather than a summit crater, whereas others present landscape features such as massive plateaus. Vents that issue volcanic material (lava, which is what magma is called once it has escaped to the surface, and ash) and gases (mainly steam and magmatic gases) can be located anywhere on the landform.
Other types of volcano include cryovolcanoes (or ice volcanoes), particularly on some moons of Jupiter, Saturn and Neptune; and mud volcanoes, which are formations often not associated with known magmatic activity. Active mud volcanoes tend to involve temperatures much lower than those of igneous volcanoes, except when a mud volcano is actually a vent of an igneous volcano.