Photoscot - Campsie and Fintry Hills

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Killearn and the Campsie Fells 17271 83 Campsie and Fintry Hills Killearn and the Campsie Fells, with the Corrie of Balglass. 05 April 2012
The Campsie Fells with Dumgoyne and Dumfoyn 17049 83 Campsie and Fintry Hills The Campsie Fells with Dumgoyne and Dumfoyn, taken from Kelvindale, Glasgow by David Palmar. These two volcanic plugs or necks mark the western end of the Campsie Fells. The Carboniferous outpouring of lava from these volcanoes and others gave rise to the Campsies, Kilpatricks and Renfrew heights, which are collectively known as the Clyde Plateau Lavas. To the right can be seen some of the lava flows. The weather is a typically anticyclonic winter scene, with cold dry air, blue skies and snow. 01 January 2021
Dumgoyne and Dumfoyn 17046 83 Campsie and Fintry Hills Dumgoyne and Dumfoyn, taken from Kelvindale, Glasgow by David Palmar. These two volcanic plugs or necks mark the western end of the Campsie Fells. The Carboniferous outpouring of lava from these volcanoes and others gave rise to the Campsies, Kilpatricks and Renfrew Heights, which are collectively known as the Clyde Plateau Lavas. The weather is a typically anticyclonic winter scene, with cold dry air, blue skies and snow. 08 January 2021
The volcanic plug of Dumgoyne 17045 83 Campsie and Fintry Hills Dumgoyne, taken from Kelvindale, Glasgow by David Palmar. This volcanic plug or neck marks the western end of the Campsie Fells. The Carboniferous outpouring of lava from these volcanoes and others gave rise to the Campsies, Kilpatricks and Renfrew Heights, which are collectively known as the Clyde Plateau Lavas. The weather is a typically anticyclonic winter scene, with cold dry air, blue skies and snow. 08 January 2021
The Campsie Fells from Lennoxtown 14784 83 Campsie and Fintry Hills The Campsie Fells from Lennoxtown, showing the Carboniferous lava flows and a scree slope formed after the last glaciation by frost shattering, and gravity. 01 January 2019
The Campsie Fells from Lennoxtown 14783 83 Campsie and Fintry Hills The Campsie Fells from Lennoxtown, showing the gullied surface of the south slope, where postglacial river erosion has cut into the glacial till and other deposits on the hillside. 01 January 2019
Jackdaws, Lennoxtown 14782 83 Campsie and Fintry Hills Jackdaws (Corvus monedula), Lennoxtown 01 January 2019
Meikle Bin in the snow 14622 83 Campsie and Fintry Hills The Meikle Bin, the second highest point in the Campsie Fells, and the Clachie Burn in the snow from the Crow Road from Lennoxtown to Fintry 15 February 2016
Stronend and the Fintry Hills in the snow 14621 83 Campsie and Fintry Hills Stronend and the Fintry Hills in the snow from the Kippen to Fintry road 15 February 2016
Stronend and the Fintry Hills in the snow 14620 83 Campsie and Fintry Hills Stronend and the Fintry Hills in the snow from the Kippen to Fintry road 15 February 2016

Killearn and the Campsie Fells

17271

Campsie and Fintry Hills

Killearn and the Campsie Fells, with the Corrie of Balglass.

05 April 2012

The Campsie Fells with Dumgoyne and Dumfoyn

17049

Campsie and Fintry Hills

The Campsie Fells with Dumgoyne and Dumfoyn, taken from Kelvindale, Glasgow by David Palmar.
These two volcanic plugs or necks mark the western end of the Campsie Fells.
The Carboniferous outpouring of lava from these volcanoes and others gave rise to the Campsies, Kilpatricks and Renfrew heights, which are collectively known as the Clyde Plateau Lavas. To the right can be seen some of the lava flows.
The weather is a typically anticyclonic winter scene, with cold dry air, blue skies and snow.

01 January 2021

Dumgoyne and Dumfoyn

17046

Campsie and Fintry Hills

Dumgoyne and Dumfoyn, taken from Kelvindale, Glasgow by David Palmar.
These two volcanic plugs or necks mark the western end of the Campsie Fells.
The Carboniferous outpouring of lava from these volcanoes and others gave rise to the Campsies, Kilpatricks and Renfrew Heights, which are collectively known as the Clyde Plateau Lavas.
The weather is a typically anticyclonic winter scene, with cold dry air, blue skies and snow.

08 January 2021

The volcanic plug of Dumgoyne

17045

Campsie and Fintry Hills

Dumgoyne, taken from Kelvindale, Glasgow by David Palmar.
This volcanic plug or neck marks the western end of the Campsie Fells.
The Carboniferous outpouring of lava from these volcanoes and others gave rise to the Campsies, Kilpatricks and Renfrew Heights, which are collectively known as the Clyde Plateau Lavas.
The weather is a typically anticyclonic winter scene, with cold dry air, blue skies and snow.

08 January 2021

The Campsie Fells from Lennoxtown

14784

Campsie and Fintry Hills

The Campsie Fells from Lennoxtown, showing the Carboniferous lava flows and a scree slope formed after the last glaciation by frost shattering, and gravity.

01 January 2019

The Campsie Fells from Lennoxtown

14783

Campsie and Fintry Hills

The Campsie Fells from Lennoxtown, showing the gullied surface of the south slope, where postglacial river erosion has cut into the glacial till and other deposits on the hillside.

01 January 2019