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Table 1. Features of more representative boulders from Punta Saguerra; they have been chosen in function of their weight, a-axis orientation, elevation and distance from the coastline. The last two columns contain the calculated minimum heights of the storm wave and of the tsunami necessary to move boulders inland. The heights were obtained by applying the Pignatelli et al. (2009) equation starting from the boulder sizes.

From: The boulder berm of Punta Saguerra (Taranto, Italy): a morphological imprint of the Rossano Calabro tsunami of April 24, 1836?

Saguerra Cape

ID

a-axis (m)

b-axis (m)

c-axis (m)

Weight (t)

Storm wave height (m)

Tsunami height (m)

Q s = 2.2 g/cm3

BA01

3.00

1.10

0.70

4.97

9.44

2.36

BA02

4.10

3.30

0.90

26.18

12.13

3.03

BA04

3.30

1.63

0.87

10.06

11.73

2.93

BA16

3.40

1.60

1.07

12.52

14.43

3.61

BA35

3.70

3.10

1.20

29.59

16.18

4.04

BA43

1.20

1.12

0.60

1.73

8.09

2.02

BA55

0.90

0.64

0.65

0.74

8.76

2.19

BA72

1.36

1.10

0.26

0.84

3.51

0.88