davenn said:
and that's not total
that is PER DAY !
Good catch! Not sure why I left off the "per day" in that post.
Now I want to kick myself for not posting what I saw just a few minutes later.
USGS Volcanoes
Yesterday at 12:12
How much lava has erupted since May 3?
113.5 million cubic meters (0.11 cubic kilometers, 4008.2 million cubic feet)
That's enough to fill 45,400 Olympic-sized swimming pools, cover Manhattan Island to a depth of 6.5 feet, or fill 11.3 million average dump trucks.
I recall thinking, "11 isn't that much more than 9", I'll just leave it at that.
Maybe this is why people keep sending me links to "eyeglass sales".
BillTre said:
So this seems like a rather smallish eruption by volume.
This one might be 9 x 30 days (my approximation) = 270 x 1,000,000 cubic meters
Not that bad for an approximation.
Big eruptions seem to usually be measured in cubic kilometers (1,000,000,000 cubic meters).
It looks like explosive type volcanoes eruptive volumes are usually measured as volume of tuff, which to me seems like a fluffed up version of lava (due to released dissolved gasses) while effusive eruptions are just a volume of lava (gas free).
Big eruptions of both kinds can be 1,000's of cubic kilometers.
Someone should calculate the volume of "The Big Island", from its peak down to the sea floor. It's all old (and new) lava.

hmmm... I've got nothing to do.
Roughly 100,000 km
3
Age of the island: 500,000 years ?
(Is it really that young?)
If so, that's only 1/5 km
3 per year.
Or 200,000,000 m
3 per year.
hmm... If these calculations are anywhere close to being correct, it would appear that the people living in the "rift zone" have been very fortunate.
From the USGS reference above;
"That's a lot of lava, but it's only 1/2 the amount of the 1984 Mauna Loa eruption."
But then again:
Mantle supply rates [ref Oregon State University]:
...
Because the discharge rates of almost all tube-fed pahoehoe eruptions on both and Mauna Loa seem to have been between 2 and 5 cubic meters per second, this has been proposed to be the supply rate to each volcano from the mantle (Swanson 1972; Dzurisin et al. 1984; Rowland & Walker 1990). You may recall from the beginning of this review that dividing the total volume of Mauna Loa by its estimated age yields essentially the same value. This would imply that all magma supplied from the mantle is erupted onto the surface; this is definitely not the case. When the volume of lava erupted onto the surface at Mauna Loa since the arrival of westerners (1778) is divided by the time since 1778, the rate is only 1 cubic meter per second, and a similar calculation for Kilauea yields a value of only 0.2 cubic meter/sec.
These values are 3 and 15 times smaller than the proposed supply rate of about 3 meters per second. These relationships point out the pitfalls of looking only at the surfaces of volcanoes for short periods of their lives, and suggest that the ratio of intruded:erupted magma is high at both Mauna Loa and Kilauea.
2 m
3/sec = 60,000,000 m
3/year
5 m
3/sec = 160,000,000 m
3/year (Woo hoo! My maths might be correct!)
0.2 m
3/sec = 6,000,000 m
3/year
Conclusion: None.
But it's interesting to think about.