<- c(1492, 1585, 1646, 1677, 1712, 1949, 1971, 2021)
eruptions <- length(eruptions) n_eruptions
1 Introduction
In [1]:
In [2]:
par(mar = c(3, 1, 1, 1) + 0.1)
plot(eruptions, rep(0, n_eruptions),
pch = "|", axes = FALSE)
axis(1)
box()
In [3]:
<- mean(diff(eruptions[-n_eruptions]))
avg_years_between_eruptions avg_years_between_eruptions
[1] 79.83333
Based on data up to and including 1971, eruptions on La Palma happen every 79.8 years on average.
Studies of the magma systems feeding the volcano, such as Marrero et al. (2019), have proposed that there are two main magma reservoirs feeding the Cumbre Vieja volcano; one in the mantle (30-40km depth) which charges and in turn feeds a shallower crustal reservoir (10-20km depth).
Eight eruptions have been recorded since the late 1400s (Figure 1).
Data and methods are discussed in Section 2.
Let \(x\) denote the number of eruptions in a year. Then, \(x\) can be modeled by a Poisson distribution
\[ p(x) = \frac{e^{-\lambda} \lambda^{x}}{x !} \tag{1}\]
where \(\lambda\) is the rate of eruptions per year. Using Equation 1, the probability of an eruption in the next \(t\) years can be calculated.
Name | Year |
---|---|
Current | 2021 |
Teneguía | 1971 |
Nambroque | 1949 |
El Charco | 1712 |
Volcán San Antonio | 1677 |
Volcán San Martin | 1646 |
Tajuya near El Paso | 1585 |
Montaña Quemada | 1492 |
Table 1 summarises the eruptions recorded since the colonization of the islands by Europeans in the late 1400s.
La Palma is one of the west most islands in the Volcanic Archipelago of the Canary Islands (Figure 2).
Figure 3 shows the location of recent Earthquakes on La Palma.