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FreeTTS is an open source speech synthesis system written entirely in the Java programming language. It is based upon Flite. FreeTTS is an implementation of Sun's Java Speech API. FreeTTS supports end-of-speech markers.
The rocks of the crust fall into two major categories – sial (aluminium silicate) and sima (magnesium silicate). [13] It is estimated that sima starts about 11 km below the Conrad discontinuity , [ 14 ] though the discontinuity is not distinct and can be absent in some continental regions.
Sima often takes the form of basalt when on the surface. In geology, sima (/ ˈ s aɪ m ə /) is an antiquated [1] blended term for the lower layer of Earth's crust. This layer is made of rocks rich in magnesium silicate minerals. Typically, when the sima comes to the surface, it is basalt, so sometimes this layer is called the 'ocean layer' of ...
Because of the large pressures, over geologic time, the sima flows like a very viscous liquid, so, in a real sense, the sial floats on the sima, in isostatic equilibrium. [9] Mountains extend down as well as up, much like icebergs on the ocean; [9] so that on the continental plates, the sial runs between 5 km and 70 km deep. [10]
An online research tool that allows the coding of text to build a causal map. Features: Qualitative coding of causal links in text; Display as a network; Filter and query the network; Ability to deal with multiple sources; Online Paid (Free trial available) Insight Maker [9] Full release Causal loop diagram builder. Can be used for stock and ...
Therefore, the seismologists of that time considered that the Conrad discontinuity should correspond to a sharply defined contact between the chemically distinct two layers, sial and sima. [2] Despite the fact that sial and sima are two solid layers, the lighter sial is thought to "float" on top of the denser sima layer.