“Based on Mr Stokoe’s advice that AGL1 is the standard used by HMRC officers assessing claims for Aggregates Levy relief or exemption for slate I adopted the BGS report [Merriman] classification for investigation of the Aggregates Levy claim made by the Appellant.”
“2. I make this statement in support of the defence made by the Respondent, HMRC, in their rejection of the claim made by the Appellant, Lovie Ltd for repayment of Aggregates Levy paid in respect of aggregates produced at Cottonhill Quarry, Macduff, Aberdeenshire, Scotland.”
“2.1 Information relating to the Aggregates Levy legislation is provided by ‘Aggregates Levy. HMRC Reference: Notice AGL1’ dated 2017. 2.2 Geological terms are used in accordance with national and international standards (e.g. BS 5930, BS EN ISO 14688) other than as defined in BGS Report CR/03/281N (Merriman, RJ, Highley, D E, and Cameron, D G. 2003): Definition and characteristics of very-fine-grained sedimentary rocks: clay, mudstone, shale and slate.”
“29. Accordingly, and in the absence of any expert evidence, much in this case turns upon my assessment of the documentary evidence in the light of the parties’ respective analysis of it. As I have already noted, to the extent that the witnesses expressed their opinions on the documents they discussed I have discounted their evidence.”
“The rocks exposed in Cottonhill Quarry are typically low-grade regionally metamorphosed, fine grained rocks with a well developed cleavage, or where coarser grained an ability to split into layers. Based upon these characteristics, it is concluded that the rock being worked at Cottonhill Quarry belonging to the Macduff Slate Formation can be classified geologically as: SLATE.”
“3.2 The quarry has been in operation since the mid-1970’s and presently extends over an area of about 7 ha including the soil bunds around the periphery. It is situated on a low hill with surface level 80-85 m above Ordnance Datum (aOD) below which the quarry is worked on three levels: in the south the access ramp from the B9031 leads to an area at 68-70 m presently used for the offices, weighbridge and vehicle parking; a ramp in the west of the quarry from this level leads to the main working area at 58-59 m aOD from which extraction is progressing into an intermediate level at 65-68 m in the south east of the quarry. 3.3 Blasting is used to loosen the rock, mainly along natural discontinuities, so that it can be extracted by mechanical excavator. Processing is carried out on site using mobile crushing and screening plant to produce a range of aggregate products (e.g. Appendix 3). 3.4 Desk study (Appendix 2) reveals that Cottonhill quarry lies within the outcrop of a group of rocks of early Palaeozoic (probably Cambrian) age now classified by the BGS as the Macduff Formation. In other published works by the BGS and other authors the rocks are termed the Macduff Slate Formation or referred to simply as the Macduff slates.”
“The most significant features to determine whether to classify a rock as slate are (i) grain size, (ii) the presence of cleavage and (iii) chemical composition.”
“Problems have arisen with the precise definition of the term shale, slate and clay (see Appendix 1). The purpose of this paper is to define these more carefully, in terms of their characteristics and geological original, in a form that will assist HM Customs and Excise officers during site visits. However, the original choice of these terms for the purpose of the Act is believed to have been based on their use as economic mineral commodities rather than geological entities. With this in mind, the closely related rock types, siltstone and mudstone have been included in the paper.”
“Siltstone, clay, shale and mudstone are very-fine-grained sedimentary rocks. Slate is the low-grade metamorphic equivalent of these rocks. The main constituents are clay minerals and quartz, and they have grain sizes of less than 0.032 mm (<32 µm) (Appendix 4). In this report the BGS size division 32 µm between very-fine sand and silt has been used (Hallsworth & Knox, 1999). The division based on the Wentworth scale and BS 5930, that is generally used by the industry and scientifically, is taken at 63 µm (Wentworth, 1922). However, 32 µm is a useful division for observation of hand specimens since it is the finest particle size that can be detected as granular material by using a hand lens and is, therefore, practical for use in field observation. Individual grains smaller than 32 µm cannot be resolved with the naked eye or with the aid of a hand lens. The existence of different classification limits does mean that, in certain circumstances, depending on the grain size of the sediment, there may be doubt as to whether a material is actually predominantly a mudstone/shale or a siltstone. This can only be resolved by sampling and grain size analysis. Should any conflict arise it is recommended that the division at 63 µm be used as this is widely recognised.”
“HMRC Notice AGL1 in its present form (updated09 February 2017 ) states that: ‘BGS definitions of industrial minerals apply for the purposes of the Aggregates Levy’ but gives no specific definition of slate.”
“metamorphic rocks are generally classified according to fabric and mineralogy rather than grain size. Most metamorphic rocks are distinguished by foliation which may impart fissility.”
“201. The term slate has been used traditionally as a rock name for a compact, fine-grained, low-grade metamorphic rock with a slaty cleavage, that is, a strong fissility along planes that allow the rock to be parted into thin plates, indistinguishable from each other in terms of lithological characteristics. However, the name also has industrial connotations for a rock which is, or has been used for roofing, billiard tables, drawing boards, damp proof courses et cetera on account of its strong fissility. In this context, the facility may be of either tectonic or bedding depositional origin. The protolith of a “slate” is almost invariably fine-grained but can include mudstones, volcaniclastic rocks or even pyroclastic rocks. It may therefore be in igneous or sedimentary rock. On the basis of the range of lithologies that have been encompassed within the name slate, together with the practical connotations in the name, it is not a preferred route name. However, it is accepted that the name is entrenched in the literature and that it is useful as a general field name for fine-grained fissile rocks of undefined protolith, many of which can be hard to classify modally because of the fine grain size. Few qualifiers other than colour, for example grey-green slate, will be appropriate for the root name slate since the use of the name implies that little is known about the rock other than grain size and texture. If a protolith or modal root name can be used, it is preferable to indicate the presence of a slaty cleavage by textural qualifier slaty, for example slaty meta-mudstone, slaty slate semi-pelite, slaty metatuffite.”
“Few qualifiers other than colour, for example grey-green slate, will be appropriate for the root name slate since the use of the name implies that little is known about the rock other than grain size and texture.”
“As with judicial or other opinions, what carries weight is the reasoning, not the conclusion.”