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hammer-geology-breaks-rocks-and-is-used-a-lot

This hammer is great for breaking rocks!

Prospector's Hammer: The hammerhead breaks and trims small rocks as well as light chisel driving, and the sharp pick end lightly pries and breaks loose or weathered rock.
lava-lamp-what-lava-is

Ever heard of lava lamps?

Lava is molten rock generated by geothermal energy and expelled through fractures in planetary crust or in an eruption , usually at temperature from 700 to 1200 Celsius

May not work well on mobile device try to look at it in desktop mode to view.

geode-crystals-can-be-found-near-volcano-sites

Geodes are prominent at old volcano sites.

Volcanic ash beds, or regions containing limestone, are common geode locations.
arrow-pointing-toward-caldera

The mouth of a volcano once inactive

It called a caldera: This is the open concave area from a previously erupted volcano. Many will develop a natural lake.
Snowflake Obsidian

Snowfake Obsidian is formed when...

The felsic lava rapidly cools down with very minimum crystal growth. It's basically a volcanic glass that formed as an igneous rock. Obsidian's high silica content makes the lava it forms from highly viscous, or thick.
gases-released-from-a-voclano-and-steam-precentages

Gases and steam from a volcano:

The mixture of gases released by volcanoes varies but, consists mainly of: water vapour (steam) - about 78% carbon dioxide - about 12% Sulphur dioxide - about 7% other gases - about 3%.
Obsidian

Obsidian

(/ˌɒbˈsɪdiən/; /əb-/) is a naturally occurring volcanic glass formed when lava extruded from a volcano cools rapidly with minimal crystal growth. It is an igneous rock. Obsidian is produced from felsic lava, rich in the lighter elements such as silicon, oxygen, aluminum, sodium, and potassium. It is commonly found within the margins of rhyolitic lava flows known as obsidian flows. These flows have a high content of silica, giving them a high viscosity. The high viscosity inhibits diffusion of atoms through the lava, which inhibits the first step (nucleation) in the formation of mineral crystals. Together with rapid cooling, this results in a natural glass forming from the lava. It is hard, brittle, and amorphous; it can fractures wielding sharp edges. It has been used in the past as cutting and piercing tools, and it has been used experimentally as surgical scalpel blades.
arrow-pointing-to-lava-flow-area

Lava flow area

Here you can see where the lava once was flowing down the volcano where you would have a pretty good chance of finding obsidian and other lava rocks
lava-rocks-explode-when-they-have-water-heat-pressure

Lava Rocks are very light

Lava rocks are very porous like a sponge. Water can get trapped inside of lava rocks when they get wet. When the wet lava rocks get heated up by the fire, the water inside turns to steam and expands. This creates pressure inside of the lava rocks which can cause them to explode open.
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