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Tree-ring based record of intra-eruptive lahar activity: Axaltzintle valley, Malinche volcano, Mexico


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La Malinche volcano is located in the central-eastern part of the Trans-Mexican Volcanic belt (TMVB). The Landsat satellite imagery in composite RGB false colors illustrates the forest cover of the volcano and Axaltzintle valley on its NE slopes (white line). The white dots indicate the sampling sites.
La Malinche volcano is located in the central-eastern part of the Trans-Mexican Volcanic belt (TMVB). The Landsat satellite imagery in composite RGB false colors illustrates the forest cover of the volcano and Axaltzintle valley on its NE slopes (white line). The white dots indicate the sampling sites.

A) Abies religiosa forest growing near the Axaltzintle valley bottom. B) Low terraces point to the deposition of lahar material in the valley whereas trees point to their recent occurrence via impact scars of up to 1 m on their stems. C) Trees buried and impacted by recent lahars. T-1: upper terrace. T-2: lower terrace. AC: active channel.
A) Abies religiosa forest growing near the Axaltzintle valley bottom. B) Low terraces point to the deposition of lahar material in the valley whereas trees point to their recent occurrence via impact scars of up to 1 m on their stems. C) Trees buried and impacted by recent lahars. T-1: upper terrace. T-2: lower terrace. AC: active channel.

A) Living trees affected by lahars in general were sampled with increment cores. B) Partial cross sections were taken from a limited number of impact scars. C) Detailed views of different types of growth disturbances in Abies religiosa caused by lahars: injury (I), callus tissue (CT) and tangential rows of traumatic resin ducts (TRD).
A) Living trees affected by lahars in general were sampled with increment cores. B) Partial cross sections were taken from a limited number of impact scars. C) Detailed views of different types of growth disturbances in Abies religiosa caused by lahars: injury (I), callus tissue (CT) and tangential rows of traumatic resin ducts (TRD).

Evidence of lahar activity as identified in the trees sampled in the different geomorphic units of Axaltzintle valley. Solid lines are lahars reconstructed with >7 growth disturbances (GD); dashed lines stand for events with 2–5 disturbances. The 19 lines correspond to lahars in the final reconstruction.
Evidence of lahar activity as identified in the trees sampled in the different geomorphic units of Axaltzintle valley. Solid lines are lahars reconstructed with >7 growth disturbances (GD); dashed lines stand for events with 2–5 disturbances. The 19 lines correspond to lahars in the final reconstruction.

Trees affected by the 1998 and 2005 lahars. Gs = growth suppression, TRD = tangential rows of traumatic resin ducts, ExG = eccentric growth, I = injury, Cw = compression wood; and Gr = growth release. For details see text.
Trees affected by the 1998 and 2005 lahars. Gs = growth suppression, TRD = tangential rows of traumatic resin ducts, ExG = eccentric growth, I = injury, Cw = compression wood; and Gr = growth release. For details see text.

Spatial distribution and type of samples in the Axaltzintle valley.

T-1T2Inside of chanelTotal
Tree samples in A. religiosa5621986
Increment cores1113511157
Cross sections1315
Wedges1146
Total1133916168

Number and percentage of growth disturbances (GD) induced by lahars as reconstructed from the tree-ring records of Abies religiosa in the Axaltzintle valley.

GDs of A. religiosaNo.%
TRD10548
Growth suppression6630
Injury2210
Eccentric growth115
Compression wood63
Growth release52
Callus tissue21
Total217100
eISSN:
1897-1695
Language:
English
Publication timeframe:
Volume Open
Journal Subjects:
Geosciences, other