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stratovo

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The answer STRATOVO has 0 possible clue(s) in existing crosswords.

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The word STRATOVO is NOT valid in any word game. (Sorry, you cannot play STRATOVO in Scrabble, Words With Friends etc)

There are 8 letters in STRATOVO ( A¹O¹R¹S¹T¹V⁴ )

To search all scrabble anagrams of STRATOVO, to go: STRATOVO?

Rearrange the letters in STRATOVO and see some winning combinations

6 letters out of STRATOVO

OTTARS STATOR TAROTS TORTAS

5 letters out of STRATOVO

ARVOS OTTAR OTTOS RATOS ROAST ROOST ROOTS ROTAS ROTOS SAVOR SORTA START STOAT TAROS TAROT TARTS TOAST TOOTS TORAS TOROS TOROT TORSO TORTA TORTS TROTS

4 letters out of STRATOVO

3 letters out of STRATOVO

ARS ART ATT AVO OAR OAT OOT ORA ORS ORT OVA RAS RAT ROT SAT SOT TAO TAR TAS TAT TAV TOO TOR TOT VAR VAS VAT

2 letters out of STRATOVO

AR AS AT OR OS SO TA TO

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Definitions of stratovo in various dictionaries:

STRATOVO - A stratovolcano, also known as a composite volcano, is a conical volcano built up by many layers (strata) of hardened lava, tephra, pumice and ash. U...

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Stratovo might refer to
A stratovolcano, also known as a composite volcano, is a conical volcano built up by many layers (strata) of hardened lava, tephra, pumice and ash. Unlike shield volcanoes, stratovolcanoes are characterized by a steep profile with a summit crater and periodic intervals of explosive eruptions and effusive eruptions, although some have collapsed summit craters called calderas. The lava flowing from stratovolcanoes typically cools and hardens before spreading far due to high viscosity. The magma forming this lava is often felsic, having high-to-intermediate levels of silica (as in rhyolite, dacite, or andesite), with lesser amounts of less-viscous mafic magma. Extensive felsic lava flows are uncommon, but have travelled as far as 15 km (9.3 mi).Stratovolcanoes are sometimes called "composite volcanoes" because of their composite stratified structure built up from sequential outpourings of erupted materials. They are among the most common types of volcanoes, in contrast to the less common shield volcanoes. Two famous examples of stratovolcanoes are Krakatoa, best known for its catastrophic eruption in 1883 and Vesuvius, famous for its destruction of Pompeii and Herculaneum in 79 AD. Both eruptions claimed thousands of lives. In modern times, Mount Saint Helens and Mount Pinatubo have erupted catastrophically, with lesser losses of lives. * Existence of stratovolcanoes has not been proved on other terrestrial bodies of the solar system with one exception. Their existence was suggested for some isolated massifs on Mars, e.g., Zephyria Tholus.

Stratovo might refer to

A stratovolcano, also known as a composite volcano, is a conical volcano built up by many layers (strata) of hardened lava, tephra, pumice and ash. Unlike shield volcanoes, stratovolcanoes are characterized by a steep profile with a summit crater and periodic intervals of explosive eruptions and effusive eruptions, although some have collapsed summit craters called calderas. The lava flowing from stratovolcanoes typically cools and hardens before spreading far due to high viscosity. The magma forming this lava is often felsic, having high-to-intermediate levels of silica (as in rhyolite, dacite, or andesite), with lesser amounts of less-viscous mafic magma. Extensive felsic lava flows are uncommon, but have travelled as far as 15 km (9.3 mi).Stratovolcanoes are sometimes called "composite volcanoes" because of their composite stratified structure built up from sequential outpourings of erupted materials. They are among the most common types of volcanoes, in contrast to the less common shield volcanoes. Two famous examples of stratovolcanoes are Krakatoa, best known for its catastrophic eruption in 1883 and Vesuvius, famous for its destruction of Pompeii and Herculaneum in 79 AD. Both eruptions claimed thousands of lives. In modern times, Mount Saint Helens and Mount Pinatubo have erupted catastrophically, with lesser losses of lives.
* Existence of stratovolcanoes has not been proved on other terrestrial bodies of the solar system with one exception. Their existence was suggested for some isolated massifs on Mars, e.g., Zephyria Tholus.

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