Welcome to Anagrammer Crossword Genius! Keep reading below to see if effuse is an answer to any crossword puzzle or word game (Scrabble, Words With Friends etc). Scroll down to see all the info we have compiled on effuse.
effuse
Searching in Crosswords ...
The answer EFFUSE has 30 possible clue(s) in existing crosswords.
Searching in Word Games ...
The word EFFUSE is VALID in some board games. Check EFFUSE in word games in Scrabble, Words With Friends, see scores, anagrams etc.
Searching in Dictionaries ...
Definitions of effuse in various dictionaries:
verb - pour out
verb - flow or spill forth
verb - give out or emit (also metaphorically)
Word Research / Anagrams and more ...
Keep reading for additional results and analysis below.
| Possible Crossword Clues |
|---|
| Pour out freely |
| Flow out |
| Disseminate |
| Scattered |
| Flow outward |
| Pour out |
| Gush |
| Radiate |
| Pour forth |
| Pour or spread out |
| Possible Dictionary Clues |
|---|
| give off (a liquid, light, smell, or quality). |
| Give off (a liquid, light, smell, or quality) |
| Talk in an unrestrained, excited manner. |
| pour out |
| give out or emit (also metaphorically) |
| flow or spill forth |
| Botany Spreading out loosely. |
| To pour out (a liquid). |
| To radiate diffuse. |
| To spread or flow out. |
| Effuse might refer to |
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An Effusive eruption is a type of volcanic eruption in which lava steadily flows out of a volcano onto the ground. There are two major groupings of eruptions: effusive and explosive. Effusive eruption differs from explosive eruption, wherein magma is violently fragmented and rapidly expelled from a volcano. Effusive eruptions are most common in basaltic magmas, but they also occur in intermediate and felsic magmas. These eruptions form lava flows and lava domes, each of which vary in shape, length, and width. Deep in the crust, gasses are dissolved into the magma because of high pressures, but upon ascent and eruption, pressure drops rapidly, and these gasses begin to exsolve out of the melt. A volcanic eruption is effusive when the erupting magma is volatile poor (water, carbon dioxide, sulfur dioxide, hydrogen chloride, and hydrogen fluoride), which suppresses fragmentation, creating an oozing magma which spills out of the volcanic vent and out into the surrounding area. The shape of effusive lava flows is governed by the type of lava (i.e. composition), rate and duration of eruption, and topography of the surrounding landscape. * For an effusive eruption to occur, magma must be permeable enough to allow the expulsion of gas bubbles contained within it. If the magma is not above a certain permeability threshold, it cannot degas and will erupt explosively. Additionally, at a certain threshold, fragmentation within the magma can cause an explosive eruption. This threshold is governed by the Reynolds Number, a dimensionless number in fluid dynamics that is directly proportional to fluid velocity. Eruptions will be effusive if the magma has a low ascent velocity. At higher magma ascent rates, the fragmentation within the magma passes a threshold and results in explosive eruptions. Silicic magma also exhibits this transition between effusive and explosive eruptions, but the fragmentation mechanism differs. The 1912 Novarupta eruption and the 2003 Stromboli eruption both exhibited a transition between explosive and effusive eruption patterns. |