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Table 1: Quantitative dataset displaying the location of each Pink Stripe- Dog Biscuit Sequence outcrop studied. The table indicates the locations of the measured thicknesses (m) of each member identified.
Location | Coordinates (DDM) | Member Thickness (m) | ||||||||
Longitude | Latitude | Pink Stripe | Coroco | La Piña | Cactus | Las Eras | Rómpelo | Las Vigas | Dog Biscuit | |
Linde Vineyard Whole | -16.44908 | 28.2126 | 1 | 1.5 | 1.4 | 0.2 | 1.3 | Â | Â | Â |
Linde Vineyard Upper | -16.44946 | 28.2125 | Â | Â | Â | Â | Â | 0.75 | 0.5 | 0.5 |
Roadside Car Park | -16.42711 | 28.2019 | 0.75 | 1.6 | 0.8 | Â | 1.8 | 0.3 | 0.23 | 0.3 |
Madriguera Vineyard | -16.43202 | 28.2515 | Â | Â | Â | Â | Â | Â | Â | Â |
Fasnia Scoria Cone Lower | -16.43348 | 28.23175 | 1.2 | 2 | 1.2 | Â | Â | Â | Â | Â |
Fasnia Scoria Cone Upper | -16.434201 | 28.2323613 | Â | Â | Â | Â | 2.13 | 0.65 | 0.5 | 0.15 |
Barranco del Callo | -16.54949 | 28.09838 | Â | Â | 0.75 | Â | 1.35 | Â | Â | Â |
El Pino | -16.46825 | 28.20032 | Â | Â | 1.25 | 0.18 | 2.1 | Â | Â | Â |
Las Carretas | -16.4619 | 28.20911 | 0.6 | 1.7 | 1.4 | 0.21 | 1.85 | Â | Â | Â |
 |  | Average Thickness | 0.89 | 1.70 | 1.13 | 0.20 | 1.76 | 0.57 | 0.41 | 0.32 |
 |  | Max Thickness | 1.2 | 2 | 1.4 | 0.21 | 2.13 | 0.75 | 0.5 | 0.5 |
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Table 2: Quantitative dataset displaying the location of each Vegas Sequence outcrop studied. The table indicates the location of the measured thicknesses (m) of each member identified.
Las Vegas Formation | Coordinates (DDM) | ||
Longitude | Latitude | ||
-16.54697 | 28.14822 | ||
Member Thickness (m) | Unnamed Pumice Layer (1) | 1.8 | |
Paleo Soil/Ignimbrite (1) | 1.68 | ||
Las Vegas | 0.6 | ||
Paleo Soil (2) | 0.8 | ||
Unnamed Pumice Layer (2) | 0.25 | ||
Mena | 1.1 | ||
Paleo Soil with unnamed Pumice Bands (1) | 3.15 | ||
Blanquitos | 2.67 | ||
Paleo Soil with unnamed Pumice Bands (2) | 1.66 |
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Table 3: Qualitative dataset of the relative distance from the Guajara volcano vent from the locations where the maximum thickness of the named member was identified.
Location | Coordinates (DDM) | Member | Max Thickness (m) | Distance From Vent (Km) | |
Longitude | Latitude | ||||
Fasnia Scoria Cone Lower | -16.43348 | 28.23175 | Pink Stripe | 1.2 | 19.88 |
Fasnia Scoria Cone Lower | -16.43348 | 28.23175 | Coroco | 2 | 19.88 |
Las Carretas | -16.4619 | 28.20911 | La Piña | 1.4 | 16.75 |
Las Carretas | -16.4619 | 28.20911 | Cactus | 0.21 | 16.75 |
Fasnia Scoria Cone Upper | -16.434201 | 28.2323613 | Las Eras | 2.13 | 19.91 |
Linde Vineyard Upper | -16.44946 | 28.2125 | Rómpelo | 0.75 | 18.12 |
Linde Vineyard Upper | -16.44946 | 28.2125 | Las Vigas | 0.5 | 18.12 |
Fasnia Scoria Cone Upper | -16.434201 | 28.2323613 | 19.91 | ||
Linde Vineyard Upper | -16.44946 | 28.2125 | Dog Biscuit | 0.5 | 18.12 |
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Table 4: Fingerprint dataset showing the characteristics of each named member within the Pink Stripe- Dog Biscuit Sequence.
Pumice Fall Deposit | Pink Stripe | Coroco | La Piña | Cactus | Las Eras | Rómpelo | Las Vigas | Dog Biscuit |
Characteristics | Â | Â | Â | Â | Â | Â | Â | Â |
Average Thickness (m) | 0.89 | 1.7 | 1.13 | 0.2 | 1.76 | 0.57 | 0.41 | 0.32 |
Max Grain Size (cm) | ≤7 | ≤4 | ≤3 | ≤4 | ≤6 | ≤3 | ≤3 | ≤4 |
Average Grain Size (cm) | ~2 | ~2 | ~1 | ~1.5 | ~2 | ~2 | ~1.5 | ~2 |
Grain Gradation | Coarse-Fine-Coarse | Coarse (25cm) -Fine-Coarse | Coarse-Fine-Coarse-Fine-Coarse | None-observed | Fine-Coarse | Coarsening Upwards | Fining Upwards | Yes |
Grain Sorting | Moderately Sorted | Well Sorted | Well sorted | Moderately Sorted | Poorly Sorted | Poorly Sorted | Moderately Sorted | Moderately Sorted |
Matrix Type | Clast Supported | Clast Supported | Clast Supported | Clast Supported | Clast Supported | Clast Supported | Clast Supported | Clast Supported |
Composition of Pumice | Grey with brownish tint | Light Grey | Dark Grey with greenish tint | Grey with greenish tint | White/grey- greenish tint inside rocks | Cream/brown colour | Cream/orange colour | Cream/yellow pumice |
Pumice clasts >5cm | Yes | N/A | N/A | N/A | Yes | N/A | N/A | N/A |
Stratifications/ Bedding in member | Band in middle (fine-coarse-fine) | 2 bands of coarse pumice in top half | Alternating coarse-fine bands (5 total) | Homogenous | Homogenous | No bedding | Homogenous | Homogenous |
Lithics in Rocks | Yes | Yes | Yes | None-observed | None-observed | None-observed | None-observed | None-observed |
Oxides in Rocks | Yes | None-observed | None-observed | None-observed | Yes | None-observed | Yes | None-observed |
Bands in Rocks | None-observed | None-observed | None-observed | None-observed | None-observed | None-observed | Yes | None-observed |
Max Lithics Size (cm) | ≤2 | ≤0.5 | ≤1 (obsidian ≤0.4) | ≤0.5 | ≤4 | ≤1 | ≤1 | ≤0.5 |
Minerals Present | Microcrystals | Sanidine/ volcanic glass | Sanidine | None-observed | Sanidine/ volcanic glass | None-observed | None-observed | None-observed |
Lithics % Area | 5% | In coarse ~15%. In fine-coarse ~2% | 5% | 3% | 6-7% | 3-4% | 2% | 2% |
Pumice Fall Deposit | Unnamed Pumice Layer | Paleo Soil/ Ignimbrite (1) | Las Vegas | Paleo Soils (2) | Unnamed Pumice Layer (2) | Mena (Heavily Altered) | Paleo Soils with unnamed pumice bands (1) | Blanquitos | Paleo Soils with unnamed pumice bands (2) |
Characteristics | Â | Â | Â | Â | Â | Â | Â | Â | Â |
Average Thickness (m) | 1.8 | 1.68 | 0.6 | 0.8 | 0.25 | 1.1 | 3.15 | 2.67 | 1.66 |
Max Grain Size (cm) | 4 | 4 | 3 | 2 | 2.5 | 2.5 | 1.57 | 4 | 1.5 |
Average Grain Size (cm) | ~2 | ~2 | ~2 | ~1 | ~1.5 | ~2 | ~0.64 | ~2 | ~0.63 |
Grain Gradation | None Observed | Fining Upwards | Fining Upwards | None-observed | None-observed | Coarsening Upwards | Fine (paleo soils) - Coarse (pumice bands) | Coarse-Fine-Coarse | Fine-Coarse-Fine-Coarse |
Grain Sorting | Moderately Sorted | Well Sorted | Well Sorted | Poorly Sorted | Poorly Sorted | Moderately Sorted | Well Sorted | Well Sorted | Well Sorted |
Matrix Type | Clast Supported | Matrix supported | Clast Supported | Matrix Supported | Matrix Supported | Matrix Supported | Matrix supported (paleo soil) Clast Supported (pumice bands) | Clast Supported | Matrix supported (paleo soil) Clast Supported (pumice bands) |
Colour of Pumice | Dark grey/ greenish tint | N/A | White Pumice- Grey/Black pumice | Weathered Pumice | Light grey Pumice | Grey/ brown Pumice | Brown/ cream pumice | White/pale green Pumice | Cream-orange pumice |
Pumice clasts >5cm | N/A | N/A | N/A | N/A | N/A | N/A | N/A | N/A | N\A |
Stratifications/ Bedding in member | White banding (Water Table) | Homogenous | Top- Black/Green Pumice Band. Â Bottom-Fine grained band | Homogenous | Homogenous | Well Stratified | Well Stratified | Homogenous | Well stratified |
Lithics in Rocks | None-observed | None-observed | Yes | N/A | None-observed | None-observed | None-observed | Yes-obsidian | None-observed |
Oxides in Rocks | Yes | None-observed | Yes | N/A | Yes | None-observed | None-observed | None-observed | Yes |
Bands in Rocks | None Observed | None-observed | Yes | N/A | None-observed | None-observed | None-observed | Black/green bands in some | Found in pumice layers |
Max Lithics Size (cm) | ≤5 | ≤5 | ≤1 | N/A | N/A | ≤1 | N/A | ≤0.5 | ≤0.5 |
Minerals Present | Sanidine/ volcanic glass | None-observed | Sanidine/ volcanic glass | N/A | None-observed | Microcrystals | Biotite in 1 pumice clast. Sanidine/ volcanic glass | Microcrystals | Microcrystals/ Sanidine |
Lithics % Area | 3-4% | 2% | 3-4% | N/A | N/A | 5% | N/A | 3% | 2% |
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Table 6: Qualitative dataset displaying the outcrop’s locations, the access to these, and the named members situated at these outcrops.
Name | Coordinates | Access | Description | Present layers | |
Longitude | Latitude | ||||
Las Vegas | -16.54697 | 28.14822 | North to Las Vegas settlement next to the c Las Vegas Road | Road outcrop | Las Vegas, La Mena, Blanquitos |
Madriguera Vineyard | -16.43202 | 28.2515 | From TF-28 and dirt roads | Abandoned Vineyard | Zarza or Coroco? |
Linde Vineyard | -16.44946 | 28.2125 | From TF-28 and dirt roads | Cultivated Vineyard | Pink stripe, Coroco, La Pina, Las Eras, Rómpelo, Las Vigas, Dog Biscuit |
Fasnia Scoria Cone | -16.43348 | 28.2323613 | From TF-620 and Ctra. los Roques | Bottom of the Fasnia Scoria Cone, towards Barranco Del Morito. | Coroco, La Pina, Las Eras, Rómpelo, Las Vigas, Dog Biscuit |
Barranco del Callo | -16.54949 | 28.09838 | From TF-636 and dirt roads | Abandoned Quarry | La Pina, Las Eras/Moradas |
El Pino | -16.46825 | 28.20032 | TF-28 road after passing the bridge over Barranco del Helecho to North-east direction | Road outcrop | Top of Coroco, La Pina, Cactus, Las Eras |
Roadside Car Park | -16.42711 | 28.2019 | Directly next to TF-622, and in front of Las Eras bus stop | Car Park | Pink stripe, Coroco, La Pina, Las Eras |
Las Carretas | -16.4619 | 28.20911 | Madre del Agua road to a dirt track | Abandoned quarry | Pink stripe, Coroco, La Pina (clearest outcrop), Las Eras |